METHUEN'S TEXT-BOOKS OF SCIENCE OUTLINES OF PHYSICAL CHEMISTRY OUTLINES OF PHYSICAL CHEMISTRY BY I GEORGE SENTER D.Sc. (LOND.), PH.D. (LEIPZIG), F.I.C. PRINCIPAL OF BIRKBECK COLLEGE. LONDON EXAMINER IN CHEMISTRY, UNIVERSITY OF LONDON EXTERNAL EXAMINER IN CHEMISTRY, UNIVERSITY OF BIRMINGHAM FORMERLY READER IN CHEMISTRY IN THE UNIVERSITY OF LONDON LECTURER ON CHEMISTRY AT ST. MARY'S HOSPITAL MEDICAL SCHOOL AND EXAMINER IN CHEMISTRY TO THE ROYAL COLLEGE OF PHYSICIANS OF LONDON AND THE ROYAL COLLEGE OF SURGEONS OF ENGLAND S2VENTH EDITION METHUEN & CO. LTD. 36 ESSEX STREET W.C. LONDON S4 First Piiblished Second Edition Third Edition Fourth Edition Fifth Edition Sixth Edition Seventh Edition January 28 th rgog February igir September 1912 January I 9 I 4 November 1915 April 1918 A::/: vU : *H J A',-* r**- ** PREFACE TO FIRST EDITION THE present book is intended as an elementary in- troduction to Physical Chemistry. It is assumed that the student taking up the study of this subject has already an elementary knowledge of chemistry and phy- sics, and comparatively little space is devoted to those parts of the subject with which the student is presumed to be familiar from his earlier work. Physical chemistry is now such an extensive subject that it is impossible even to touch on all its important applications within the limits of a small text-book. I have therefore preferred to deal in considerable detail with those branches of the subject which usually present most difficulty to beginners, such as the modern theory of solutions, the principles of chemical equilibrium, elec- trical conductivity and electromotive force, and have devoted relatively less space to the relationships between physical properties and chemical composition. The prin- ciples employed in the investigation of physical proper- ties from the point of view of chemical composition are illustrated by a few typical examples, so that the student should have little difficulty in understanding the special works on these subjects. Electrochemistry is dealt with A 1 vi OUTLINES OF PHYSICAL CHEMISTRY rather more fully than has hitherto been usual in ele- mentary works on Physical Chemistry, and the book is therefore well suited for electrical engineers. From my experience as a student and as a teacher, I am convinced that one of the best methods of familiarising the student with the principles of a subject is by means of numerical examples. For this reason I have, as far as possible, given numerical illustrations of those laws and formulae which are likely to present difficulty to the be- ginner. This is particularly important with regard to cer- tain formulae more particularly those in the chapter on Electromotive Force which cannot easily be proved by simple methods, but which even the elementary student must make use of. The really important thing in this connection is not that the student should be able to prove the formula, but that he should thoroughly understand its meaning and applications. I have throughout the book used only the most ele- mentary mathematics. In order to make use of some of the formulae, particularly those in the chapters on Velo- city of Reaction and Electromotive Force, an elementary knowledge of logarithms is required, but sufficient for the purpose can be gained by the student, if necessary, from a few hours' study of the chapter on " Logarithms " in any elementary text-book on Algebra. The experiments described in the sections headed " Practical Illustrations " at the conclusion of the chap- ters can in most cases be performed with very simple apparatus, and as many as possible should be done by the student. The majority of them are also well adapted for lecture experiments. The more elaborate experi- PREFACE vli ments which arc usually performed during a course of practical Physical Chemistry are also mentioned for the sake of completeness ; for full details a book on Practical Physical Chemistry should be consulted. In drawing up my lectures, which have developed into the present book, I have been indebted most largely to the text-books of my former teachers, Ostwald and Nernst, more particularly to Ostwald's Allgemeine Chemie (2nd Edition, Leipzig, Engelmann) and to Nernst's Theo- retical Chemistry (4th Edition, London, Macmillan). 1 The following works, among others, have also been consulted : Van't Hoff, Lectures on Physical Chemistry ; Arrhenius, Theories of Chemistry ; Le Blanc, Electrochemistry; Dan- neel, Elektrochemie (Sammlung Goschen) ; Roozeboom, Phasenlehre ; Findlay, The Phase Rule ; Mellor, Chemi- cal Statics and Dynamics ; Abegg, Die elektrolytische Dissociationstheorie. In these books the student will find fuller treatment of the different branches of the subject. References to other sources of information on particular points are given throughout the book. The importance of a study of original papers can scarcely be overrated, and I have given references to a number of easily accessible papers, both in English and German, some of which should be read even by the beginner. In the summarising chapter on " Theories of Solution" references are given which will enable the more advanced student to put himself abreast of the pre- sent state of knowledge in this most interesting subject. In conclusion, I wish to express my most sincere thanks to Assistant-Professor A. W. Porter, of University x The fifth German edition of Nernst's text-book has now appeared. viii OUTLINES OF PHYSICAL CHEMISTRY College, London, for reading and criticising the sections on osmotic pressure and allied phenomena, and for valu- able advice and assistance on many occasions; also to Dr. H. Sand, of University College, Nottingham, and Dr. A. Slator, of Burton, for criticising the chapters on Electromotive Force and on Velocity of Reaction respec- tively. Lastly, I wish to acknowledge my indebtedness to my assistant, Mr. T. J. Ward, in the preparation of the diagrams and for reading the proofs. G. S. November, 1908 PREFACE TO SECOND EDITION AS less than two years have elapsed since the appear- ance of the First Edition, only a few slight altera- tions have been rendered necessary by the progress of the subject in the interval. The opportunity has, how- ever, been taken to revise the text thoroughly ; in one or two places the wording has been slightly altered for the sake of greater clearness, and some misprints have been corrected. A few additions of some importance have also been made. In conformity with the elementary character of the book, the mathematical proofs of the connection be- tween osmotic pressure and the other properties of solu- tions which can be made use of for molecular weight determinations were omitted from the first edition. The book has, however, been more largely used by advanced students than was anticipated, and at the request of several teachers the proofs in question have now been inserted as an appendix to chapter V. The section dealing with the relationship between physical properties and chemical constitution has been rendered more com- plete by the insertion of brief accounts of absorption spectra and of viscosity. x OUTLINES OF PHYSICAL CHEMISTRY I am again indebted to Professor Porter for much kind advice and assistance, and take this opportunity of expressing to him my grateful thanks. I wish also to acknowledge my indebtedness to a number of friends and correspondents, more particularly to Dr. A. Lapworth, F.R.S., Dr. J. C. Philip, Dr. A. E. Dunstan, Dr. W. Maitland and Mr. W. G. Pirie, M.A.. for valuable sug- gestions. G. S. December, 1910. PREFACE TO FIFTH EDITION THE fact that a fifth large edition is called for within seven years of the first appearance of this book shows that the object with which it was written to assist in spreading a knowledge of the principles and methods of Physical Chemistry is being satisfactorily fulfilled. The opportunities afforded by the calls for successive editions have been taken advantage of to keep the book up to date and further to increase its usefulness by in- troducing certain new sections and amplifying others. Thus for the Third Edition a new chapter on Colloidal Solutions was written and a selection of questions and numerical problems was added. In the Fourth Edition the latter important section was amplified, and the last chapter, on Electromotive Force, was considerably ex- tended. For the Present Edition additions have been made to the chapters on Thermochemistry and on Heterogeneous Equilibrium, and a number of minor alterations have been made. In the Preface to the First Edition the great educa- tional value of numerical problems and examples was emphasized, and further experience has served to con- firm and strengthen the opinion then stated. In addition to working out the problems in the book, the student would do well to make use of one or other of the excel- lent books on Physico-chemical Calculations which have recently appeared. G. S. LUMSDEN, ABERDEENSHIRE, September, 1915. TABLE OF CONTENTS (The numbers refer to pages) CHAPTER I PAGE FUNDAMENTAL PRINCIPLES OF CHEMISTRY. THE ATOMIC THEORY i Elements and compounds, i Laws of chemical combination, 3 Atoms and molecules, 5 Fact. Generalisation or natural law. Hypothesis. Theory, 6 Determination of atomic weights. General, 8 Volumetric method. Gay-Lussac's law of volumes. Avogadro's hypothesis, 9 Dulong and Petit's law, n Isomorphism, 13 Determination of atomic weights by chemical methods, 14 Relation between atomic weights and chemical equivalents. Valency, 15 The values of the atomic weights, 16 The periodic system, 20. CHAPTER II GASES ||| . ' . 25 The gas laws, 25 Deviations from the gas laws, 28 Kinetic theory of gases. General, 29 Kinetic equation for gases, 30 Deduction of gas laws from the equation pv = %mnc z , 31 Van der Waals' equation, 33 Avogadro's hypothesis and the molecular weight of gases. General, 36 Density and molecular weight of gases and vapours, 36 Results of vapour density determinations. Abnormal molecular weights, 40 Association and dissociation in gases, 41 Ac- curate determination of molecular and atomic weights from gas densities, 42 Specific heat of gases. General, 43 TABLE OF CONTENTS x iii Specific heat at constant pressure, Cj,, and constant volume, C v , 44 Specific heat of gases and the kinetic theory, 46 Experimental illustrations, 47. CHAPTER III LIQUIDS 49 General, 49 Transition from gaseous to liquid state. Critical phenomena, 49 Behaviour of gases on compression, 51 Application of Van der Waals' equation to critical pheno- mena, 53 Law of corresponding states, 56 Liquefaction of gases, 58 Relation between physical properties and chemi- cal composition of liquids. General, 59 Atomic and mole- cular volumes, 60 Additive, constitutive, and colligative properties, 62 Refractivity, 63 Rotation of plane of polarization of light, 66 Absorption of light, 69 Viscosity, 73 Practical illustrations, 77 CHAPTER IV SOLUTIONS 80 General 80 Solution of gases in gases, 81 Solubility of gases in liquids, 82 Solubility of liquids in liquids, 84 Distilla- tion of homogeneous mixtures, 87 Distillation of non- miscible or partially miscible liquids ; steam distillation, go Solution of solids in liquids, 91 Effect of change of tem- perature on the solubility of solids in liquids, 92 Relation between solubility and chemical constitution, 94 Solid solutions, 94 Practical illustrations, 95. CHAPTER V DILUTE SOLUTIONS . . . . . .97 General, 97 Osmotic pressure. Semi-permeable membranes, 97 Measurement of osmotic pressure, 99 Van't Hoff's theory of solution, 101 Recent direct measurements of osmotic pressure, 104 Other methods of determining osmo- tic pressure, 105 Mechanism of osmotic pressure, 106 Osmotic pressure and diffusion, 108 Molecular weight of dissolved substances. General, IOQ Molecular weights xiv OUTLINES OF PHYSICAL CHEMISTRY PACE from osmotic pressure measurements, no Lowering of vapour pressure, in Elevation of boiling-point, 114 Ex- perimental determination of molecular weights by the boiling-point method, 116 Depression of the freezing-point, 119 Experimental determination of molecular weights by the freezing-point method, 120 Results of molecular weight determinations in solution. General, 121 Abnormal mole- cular weights, 123 Molecular weight of liquids, 125 The results of measurements, 127 Nature of surface tension, 129 Practical illustrations, 129. Mathematical deduction of formulae, 131. CHAPTER VI THERMOCHEMISTRY I39 General, 137 Hess's law, 139 Representation of thermo- chemical measurements. Heat of formation. Heat of solution, 141 Heat of combustion, 145 Thermochemical methods, 145 Results of thermochemical measurements, 147 Relation of chemical affinity to heat of reaction, 148 Practical illustrations, 153. CHAPTER VII EQUILIBRIUM IN HOMOGENEOUS SYSTEMS. LAW OF MASS ACTION . . . . 154 General, 154 Law of mass action, 155 Strict proof of the law of mass action, 160 Decomposition of hydriodic acid, 161 Dissociation of phosphorus pentachloride, 163 Equili- brium in solutions of non-electrolytes, 164 Influence of temperature and pressure on chemical equilibrium. General, 166 Le Chatelier's theorem, 169 Relation between chemi- cal equilibrium and temperature. Nernst's views, 169 Practical illustrations, 170. CHAPTER VIII HETEROGENEOUS EQUILIBRIUM. THE PHASE RULE -V, . * . . . . , . 172 General, 172 Application of law of mass action to hetero- geneous equilibrium, 172 Dissociation of salt hydrates, 174 TABLE OF CONTENTS xv PAGE Dissociation of ammonium hydrosulphide, 176 Analogy between solubility and dissociation, 177 Distribution of a solute between two immiscible liquids, 177 The phase rule. Equilibrium between water, ice and steam, 179 Equilibrium between four phases of the same substance. Sulphur, 183 Systems of two components. Salt and water, 186 Freezing mixtures, 189 Systems of two components. General, 190 Hydrates of ferric chloride, 194 Transition points, 197 Practical illustrations, 197. CHAPTER IX VELOCITY OF REACTION. CATALYSIS* . . 200 General, 200 Unimolecular reaction, 202 Other unimolecular reactions, 205 Bimolecular reactions, 207 Trimolecular reactions, 209 Reactions of higher order. Molecular- kinetic considerations, 211 Reactions in stages, 212 Determination of the order of a reaction, 213 Complicated reaction velocities, 215 Catalysis. General ,217 Charac- teristics of catalytic actions, 217 Examples of catalytic action. Technical importance of catalysis, 219 Biological importance of catalysis. Enzyme reactions, 221 Mechan- ism of catalysis, 222 Nature of the medium, 224 Influence of temperature on the rate of chemical reaction, 225 Formulae connecting reaction velocity and temperature, 228 Practical illustrations, 229. CHAPTER X ELECTRICAL CONDUCTIVITY .... 234 General, 234 Electrolysis of solutions. Faraday's laws, 236-=- Mechanism of electrical conductivity, 238 Freedom of the ions before electrolysis, 240 Dependence of conductivity on the number and nature of the ions, 242 Migration velocity of the ions, 243 Practical determination of the relative migration velocities of the ions, 246 Specific, molecular and equivalent conductivity, 249 Kohlrausch's law. Ionic velocities, 251 Absolute velocity of the ions, Internal xvi OUTLINES OF PHYSICAL CHEMISTRY PAGE friction, 253 Experimental determination of conductivity of electrolytes, 254 Experimental determination of molecular conductivity, 257 Results of conductivity measurements, 258 Electrolytic dissociation, 260 Degree of ionisation from conductivity and osmotic pressure measurements, 261 Effect of temperature on conductivity, 263 Basicity of acids from conductivity measurements, 264 Grotthus' hypo- thesis of electrical conductivity, 264 Practical illustrations, 264. CHAPTER XI EQUILIBRIUM IN ELECTROLYTES. STRENGTH OF ACIDS AND BASES. HYDROLYSIS . 266 The dilution law, 266 Strength of acids, 269 Strength of bases, 274 Mixture of two electrolytes with a common ion, 276 Isohydric solutions, 277 Mixture of electrolytes with no common ion, 278 Dissociation of strong electrolytes, 279 Electrolytic dissociation of water. Heat of neutrali- sation, 283 Hydrolysis, 285 Hydrolysis of the salt of a strong base and a weak acid, 287 Hydrolysis of the salt of a weak base and a strong acid, 290 Hydrolysis of the salt of a weak base and a weak acid, 292 Determination of the dissociation constant for water, 293 Theory of indica- tors, 296 The solubility product, 298 Applications to analytical chemistry, 300 Experimental determination of the solubility of difficultly soluble salts, 301 Complex ions, 303 Influence of substitution on degree of ionisation, 304 Reactivity of the ions, 306 Amphoteric electrolytes, 307 Practical illustrations, 308. CHAPTER XII COLLOIDAL SOLUTIONS. ADSORPTION . :; 313 Colloidal solutions. General, 313 Preparation of colloidal solu- tions, 315 Osmotic pressure and molecular weight of colloids, 316 Optical properties of colloidal solutions, 317 Brownian movement, 318 Electrical properties of col- loids, 319 Precipitation of colloids by electrolytes, 320 TABLE OF CONTENTS xvii Suspensions, suspensoids and emulsoids, 322 Filtration of colloidal solutions, 323 Adsorption, general, 324 Adsorp- tion of gases. Adsorption formulae, 328 The cause of adsorption, 329 Further illustrations of adsorption, 330. CHAPTER XIII THEORIES OF SOLUTION - 333 General, 333 Evidence in favour of the electrolytic dissociation theory, 335 lonisation in solvents other than water, 337 The old hydrate theory of solution, 339 Mechanism of electrolytic dissociation. Function of the solvent, 342 Hydration in solution, 345. CHAPTER XIV ELECTROMOTIVE FORCE . . . . .348 The Daniel cell, 348 Relation between chemical and electrical energy, 351 Measurement of electromotive force, 354 Standard of electromotive force. The cadmium element, 356 Solution pressure, 358 Calculation of electromotive force at a junction metal/salt solution, 360 Differences of potential in a voltaic cell, 362 Influence of change of con- centration of salt solution on the E.M.F. of a cell, 365 Concentration cells, 367 Cells with different concentrations of the electrode materials (substances producing ions), 371 Electrodes of the first and second kind. The calomel elec- trode, 373 Single potential differences. The capillary electrometer, 378 Gas cells, 383 Potential series of the elements, 387 Cells with different gases, 391 Oxidation- reduction cells, 393 Electromotive force and chemical equilibrium, 396 Electrolysis and polarization, 398 Sep- aration of ions (particularly metals) by electrolysis, 400 The electrolysis of water, overvoltage at electrodes, 401 Electrolysis and polarization (continued) 404 Accumulators, 405. The electron theory, 407 Practical illustrations, 410. b DEFINITIONS AND UNITS 1 In this section the centimetre-gram-second (C.G.S.) system of units is used throughout, length being measured in centimetres (cms.), mass in grams, and time in seconds. Density is mass per unit volume : unit, gram per c.c. (cubic centi- metre). Specific Volume (i/density) is volume per unit mass : unit, c.c. per gram. Velocity is rate of change of position : unit, cm. per sec. or cm. /sec. Acceleration is rate of change of velocity : unit, cm. per sec. per sec. or cm./sec. 2 . Momentum is mass x velocity : unit, gram-cm, per sec. Force is mass x acceleration (rate of change of momentum). Unit, the dyne, is that force which is required to produce an acceleration of i cm. per sec. per sec. in a mass of i gram. As a gram-weight, falling freely, obtains an acceleration of 980-6 cm. per sec. (owing to the attraction of the earth) the force represented by the gram-weight = g8o'6 dynes at a latitude of 45 and at sea-level. Energy may be defined as that property of a body which diminishes when work is done by the body ; and its diminution is measured by the amount of work done. Work Done is force x distance (the work done by a force is measured by the product of the force and the distance through which the point of application moves in the direction of the force). The unit of work 1 The more important constants made use of in physical chemistry are collected here for convenience of reference, xviii DEFINITIONS AND UNITS xix (which is also the unit of energy) is the dyne-centimetre or erg. The gram-centimetre unit is sometimes used; i gram-centimetre = 980-6 ergs; also the joule ( = io 7 ergs) is frequently used, especially in electrical work (see below). Power is rate of doing work, unit, erg per second. There are six chief forms of energy: (i) mechanical energy, (2) volume energy, (3) electrical energy, (4) heat, (5) chemical energy, (6) radiant energy. These forms of energy are mutually convertible, and according to the law of conservation of energy, there is a definite and invariable relationship between the quantity of one kind of energy which disappears and that which results. The unit of energy, the erg, has already been defined. It is some- times convenient to express certain forms of energy in special units, heat* for example, in calories ; in the following paragraphs the equivalents in ergs of these special units are given. Volume Energy is often measured in litre-atmospheres. When a volume, v lt of a gas expands to the volume v% against a constant pressure p, say that of the atmosphere, the external work done by the gas (gained) is p (v z - vj. The (average) pressure of the atmosphere on unit area (i sq. cm.) supports a column of mercury 76 cm. high and i sq. cm. in cross-section. Hence the pressure on i sq. cm. = 76 x 13*596 = 1033-3 grams weight (as the density of mercury is 13*596), or 1033-3 x 980-6 = 1,013,200 dynes. As the work done is the product of the constant pres- sure and the increase of volume, i litre-atmosphere (the work done when the increase in the volume of a certain quantity of a gas is i litre or 1000 c.c.) = 1,013,200 x 1000 c= 1,013,200,000 ergs. Electrical Energy is the product of electromotive force and quantity of electricity, and is usually measured in volt-coulombs or joules. The practical unit of quantity of electricity is the coulomb ; it is that quantity of electricity which under certain conditions liberates o'ooniS grams of silver from a solution of silver nitrate. If a coulomb passes through a conductor in i second, the strength of current is i ampere ; the latter is therefore the practical unit of strength of current. The practical unit of resistance is the ohm, which is the resistance at o offered by a column of mercury 106*3 cm * l n g an< ^ weighing 14-4521 grams. The practical unit of electromotive force is the volt; when a current of i ampere passes in i second through a conductor of resistance i ohm, the electromotive force is i volt. xx OUTLINES OF PHYSICAL CHEMISTRY The definitions of the C.G.S. units of electromotive force, current strength and resistance are to be found in text-books of physics, and cannot be given here. It can be shown that i ohm = io 9 C.G.S. units and i ampere = i/io C.G.S. unit; hence, by Ohm's law, i volt = io 8 C.G.S. units. Further, i volt-coulomb or i joule = io 8 x io- 1 = io 7 C.G.S. units or io 7 ergs. Heat Energy is measured in calories. The mean calorie is i/ioo of the amount of heat required to raise i gram of water from o to 100 and does not differ much from the amount of heat required to raise i gram of water from 15 to 16. i calorie = 42,650 gram-centimetres = 41,830,000 ergs (the mechanical equivalent of heat) = 4*183 joules. One joule = 0-2391 calories. There is no special unit for chemical energy ; it is usually measured in volt-coulombs or calories. The value of R, in the general gas equation (p. 27) for a mol of gas = 34,760 gram-centimetres = 83,150,000 ergs = 8-315 joules = 1*985 calories = 0*08205 litre-atmospheres. USE OF SIGNS IN ELECTRO-CHEMISTRY. There has always been much confusion in Electro-chemistry as to the proper use of positive and negative signs, and even now no general agreement has been reached on the subject. Recently, however, a simple convention has been suggested by the German Electro-chemical Society (Bunsen-Gesellschaft) which promises to find general acceptance. The potential difference has the positive sign if the metal is charged positively with respect to the solution, and negative if the metal is negatively charged, when metal and solution are combined with a comparison electrode to form a cell (cf. p. 358). In the present book, while this con- vention is adopted for the potential series of the elements, etc., the potential differences are often given in absolute value and the E.M.F. of combinations illustrated by the graphic method described on pp. 365, 377, 386 and elsewhere. As a result of considerable experience, it has been found that the graphic method is much more useful in avoiding errors of sign than any convention with regard to the use of signs. OUTLINES OF PHYSICAL CHEMISTRY CHAPTER I FUNDAMENTAL PRINCIPLES OF CHEMISTRY. THE ATOMIC THEORY Elements and Compounds Definite chemical substances are divided into the two classes of elements and chemical com- pounds. Boyle, and later Lavoisier, denned an element as a substance which had not so far been split up into anything simpler. The substances formed by chemical combination of two or more elements were termed chemical compounds This definition proved to be a very suitable one, and retained its value even when many of the substances classed as ele- ments by Lavoisier proved to be complex. In course of time it came to be recognised that the substances which resisted further decomposition possessed certain other properties in com- mon, for example, the so-called atomic heat of solid elements proved to be approximately 6*4 (p. 12), and it was found possible to assign even newly-discovered elements with more or less certainty to their appropriate positions in the periodic table of the elements p. 21). There are, therefore, conclusive reasons, apart from the fact that they have so far resisted decomposi- tion, for regarding elements as of a different order from chemical compounds, and these reasons remain equally valid when full allowance is made for the remarkable discoveries of the last few years in this branch of knowledge. CHEMISTRY Until lately no case of the transformation'of one element into another was known, but recent work on radium, by Ramsay and Soddy and others, has shown that this element is continuously undergoing a series of transformations, one of the final products of which is the inactive gas helium. It might at first sight be supposed that the old view of the impossibility of transforming the elements could be maintained, radium being looked upon as a chemical compound of helium with another element, but further consideration shows that this suggestion is not tenable, as radium fits into the periodic table, and, so far as is known, possesses all those other properties which have so far been con- sidered characteristic of elements as distinguished from chemical compounds. Evidence is gradually accumulating which indicates that the slow disintegration, with final production of other elements, is not confined to radium alone, but is shown more particularly by certain elements of high atomic weight such as uranium and thorium. It is true that the change is spontaneous, as so far there is no known means of initiating it or even of influencing its rate, but further progress in this direction is doubtless only a matter of time. As the phenomenon in question is probably a general one, it seems desirable to retain the term " element " to indicate a substance which has a definite position in the periodic table, and has the other properties usually regarded as characteristic of elements. From what has been said, it will be evident that it is difficult to define an element in a few words, but in practice there will probably not be much difficulty in drawing the distinction between elements and compounds. Ostwald l (i 907) defines an element as a substance which only increases in weight as the result of a chemical change, and which is stable under any attainable conditions of temperature and pressure, but in this definition the question of radio-active substances is left out of account. 1 Prinzipien dw Qhentie, Leipzig, 1907, p, 266,. FUNDAMENTAL PRINCIPLES OF CHEMISTRY 3 Laws of Chemical Combination Towards the end of the eighteenth century, Lavoisier established experimentally the law of the conservation of mass, which may be expressed as follows : When a chemical change occurs, the total iveight (or mass) of the reacting substances is equal to the total weight (or mass) of the products. As the weight is proportional to the mass or quantity of matter, the above law may also be stated in the form that the total quantity of matter in" the uni- verse is not altered in consequence of chemical (or any other) changes. It is, of course, impossible to prove the law with absolute certainty, but the fact that in accurate atomic weight determinations no results in contradiction with it have been obtained shows that it is valid at least within the limits of the unavoidable experimental error. The enunciation of the law of the conservation of mass by Lavoisier, and the extended use of the balance, facilitated the investigation of the proportions in which elements combine, and soon afterwards the first law of chemical combination was estab- lished by the careful experimental investigations of Richter and Proust. This law is usually expressed as follows : A definite compound always contains the same elements in the same proportions. The truth of this law was called in question by the famous French chemist Berthollet. Having observed that chemical processes are greatly influenced by the relative amounts of the reacting substances (p. 155), he contended that when, for example, a chemical compound is formed by the combination of two elements, the proportion of one of the elements in the compound will be the greater the more of that element there is available. This suggestion led to the famous controversy between Berthollet and Proust (1799-1807), which ended in the firm establishment of the law of constant proportions. All subsequent work has shown that the law in question is valid within the limits of experimental error. In certain cases, elements unite in more than one proportion 4 OUTLINES OF PHYSICAL CHEMISTRY to form definite chemical compounds. Thus Dalton found by analysis that two compounds of carbon and hydrogen methane and ethylene contain the elements in the ratios 6 : 2 and 6 : i by weight respectively ; in other words, for the same amount of carbon, the amounts of hydrogen are in the ratio 2:1. Similar simple relations were observed for other compounds, and on this experimental basis Dalton (1808) formulated the Law of Multiple Proportions, as follows : When two elements unite in more than one proportion, for a fixed amount of one element there is a simple ratio between the amounts of the other element. Dalton's experimental results were not of a high order of accuracy, but the validity of the law was proved by the subsequent investigations of Berzelius, Marignac and others. Finally, there is a third comprehensive law of combination, which includes the other two as special cases. It has been found possible to ascribe to each element a definite relative weight, with which it enters into chemical combination. The Law of Combining Proportions, which expresses this conception, is as follows : Elements combine in the ratio of their combining weight 's, or in simple multiples of this ratio. The combining weights are found by analysis of definite com- pounds containing the elements in question. When the com- bining weight of hydrogen is taken as unity, the approxi- mate values for chlorine, oxygen and sulphur are 35-5, 8 and 1 6 respectively. These numbers also represent the ratios in which the elements displace each other in chemical com- pounds. Water, for example, contains 8 parts by weight of oxygen to i of hydrogen, and when the former element is dis- placed by sulphur (forming hydrogen sulphide) the new com- pound is found to contain 16 parts by weight of the latter element. 16 parts of sulphur are therefore equivalent to 8 parts of oxygen, and the combining weights are therefore often termed chemical equivalents. The chemical equivalent of an element is FUNDAMENTAL PRINCIPLES OF CHEMISTRY 5 that quantity of it which combines with, or displaces, one part (strictly i'oo8 parts) by weight of hydrogen (cf. p. 18). It must be clearly understood that the above generalisations or laws are purely experimental ; they express in a simple form the results of the investigations of many chemists on the com- bining powers of the elements, and are quite independent of any hypothesis as to the constitution of matter. As they have been established by experiment, we are certain of their validity only within the limits of the unavoidable experimental error, and cannot say whether they are absolutely true. It is possible that when the methods of analysis are greatly improved, it will be possible to detect small variations in the composition of definite compounds, but up to the present the most careful investigations, in the course of atomic weight determinations, have failed to show any deviation from the results to be expected according to the laws. Atoms and Molecules The question now arises as to whether a theory can be suggested which allows of a convenient and consistent representation of the laws enunciated above. The atomic theory, first brought forward in its modern form by Dalton (1808), answers these requirements. Following out an idea of the old Greek philosophers, Dalton suggested that matter is not infinitely divisible by any means at our disposal, but is made up of extremely small particles termed atoms ; the atoms of any one element are identical in all respects and differ, at least in weight, from those of other elements. By the association of atoms of different kinds, chemical compounds are formed. The laws of chemical combination find a simple explanation on the atomic theory. Since a chemical compound is formed by the association of atoms, each of which has a definite weight, it must be of invariable composition. Further when atoms combine in more than one proportion, for a fixed amount of atoms of one kind the amount of the other must in- crease in steps, depending on the relative atomic weight which is the law of multiple proportions. It is here assumed that 6 OUTLINES OF PHYSICAL CHEMISTRY the ultimate particles of a compound are formed by the associa- tion of comparatively few atoms, and this holds in general for inorganic compounds. Finally, the law of combining weights is also seen to be a logical consequence of the atomic theory, the empirically found combining weights, or chemical equiva- lents, bearing a simple relation to the (relative) weights of the atoms (p. 15). When Dalton brought forward the atomic theory, the number of facts which it had to account for was comparatively small. As knowledge has progressed, the atomic theory has proved capable of extension to represent the new facts, and its applica- tion has led to many important discoveries. At the present day, the great majority of chemists consider that the atomic theory has by no means outgrown its usefulness. Fact. Generalisation or Natural Law. Hypothesis. Theory 1 Chemistry, like most other sciences, is based on facts, established by experiment. A few such facts have already been mentioned, for example, that certain chemical compounds, which have been investigated with the greatest care, always contain the same elements in the same proportions. A mere collection of facts, however, does not constitute a science. When a certain number of facts have been established, the chemist proceeds to reason from analogy as to the behaviour of systems under conditions which have not yet been investigated. For example, Proust showed by careful analyses that there are two well-defined oxides of tin, and that the composition of each is invariable. From the results of these and a few other investigations, he concluded from analogy that the composition of all pure chemical compounds is invariable, although of course very few of them had then been investigated from that point of view. To proceed in this way is to generalise^ and the short statement of the conclusion arrived at is termed a generalisation 1 H. Poincare", La Science et I'Hypothese, Paris, Flammarion ; Ostwald, Vorlesungen uber Naturphilosophie, Leipzig, 1902; Alexander Smith, General Inorganic Chemistry, London, 1906. FUNDAMENTAL PRINCIPLES OF CHEMISTRY 7 or law. It will be evident that a law is not in the nature of an absolute certainty ; it comprises the facts experimentally estab- lished, but also enables us (and herein lies its value) to foretell a great many things which have not been, but which if necessary could be, investigated experimentally. The greater the number of cases in which a law has been found to hold, the greater is the confidence in its validity, until finally a law may attain practically the same standing as a statement of fact. We may confidently expect that however greatly our views regarding natural pheno* mena may change, such generalisations as the law of constant proportions will remain eternally true. Natural laws can be discovered in two ways : (i) by corre- lating a number of experimental facts, as just indicated ; (2) by a speculative method, on the basis of certain hypotheses as to the nature of the phenomena in question. The meaning to be at- tached to the term " hypothesis " is best illustrated by an example. In the previous section we have seen that the laws of chemical combination are accounted for satisfactorily on the view that matter is made up of extremely small, discrete particles, the atoms. Such a mechanical representation, which is more or less inaccessible to experimental proof, is termed a hypothesis A hypothesis may then be defined as a mental picture of an unknown, or largely unknown, state of affairs, in terms of some- thing which is better known. Thus, the state of affairs in gases, which is and Avill remain unknown to us, is represented, according to the kinetic theory, in terms of an enormous number of rapidly moving perfectly elastic particles, and on this basis it is possible, with the help of certain assumptions, to deduce certain of the laws which are actually followed by gases (p. 25). There does not appear to be any fundamental distinction in the use of the terms hypothesis and theory. A theory may be defined as a hypothesis, many of the deductions from which have been confirmed by experiment, and which admits of the con- venient representation of a large number of experimental facts. There is some difference of opinion as to the value of 8 OUTLINES OF PHYSICAL CHEMISTRY hypotheses and theories for the advancement of science. 1 The majority of scientists, however, appear to consider that the advantages of hypotheses, regarded in the proper light and not as representing the actual state of affairs, are much greater than the disadvantages. Boltzmann, 2 indeed, maintains that " new discoveries are made almost exclusively by means of special mechanical conceptions ". DETERMINATION OF ATOMIC WEIGHTS General After the laws of chemical combination had been established, the next problem with which chemists had to deal was the determination of the relative atomic weights of the elements. This might apparently be done by fixing on one element, say hydrogen, as the standard ; a compound containing hydrogen and another element may then be analysed, and the amount of the other element combined with one part of hydrogen will be its atomic weight. It is clear, however, that this will be the case only when the binary compound contains one atom of each element, and it was just this difficulty of deciding the relative number of atoms of the two elements present that rendered the decision between a number and one of its multi- ples or sub-multiples so difficult. It has already been pointed out that the amount of an ele- ment which combines with, or displaces, part by weight of hydrogen (strictly speaking, 8 parts by weight of oxygen) is termed the combining weight or chemical equivalent of an ele- ment. The first step in determining the atomic weight of an element is to find the chemical equivalent as accurately as pos- sible by analysis and then to find the relation between the atomic weight and chemical equivalent by one of the methods described below. The atomic weight may be equal to, or a simple multiple of, the chemical equivalent. 1 In one or two recent books, Ostwald has treated certain branches of chemistry on a system free from hypotheses. 2 Gas Theorie, Leipzig, 1896, p. 4. FUNDAMENTAL PRINCIPLES OF CHEMISTRY 9 Dalton, working on the assumption that when two elements unite in only one proportion one atom of each is present, drew up the first table of atomic weights. Water was found by analysis to contain i part of hydrogen to 8 parts of oxygen by weight ; the atomic weight of oxygen was therefore taken as 8. In the same way, since ammonia contained i part of hydrogen to 4-6 parts of nitrogen, the atomic weight of the latter element was taken as 4*6. Great advances in this subject were then made by the Swedish chemist Berzelius. For fixing the pro- portional numbers, he depended to some extent, like Dalton, on the assumption of simplicity of composition, but was able to check the numbers thus obtained by the application of Gay- Lussac's law of volumes and Dulong and Petit's law. Later still, the discovery of isomorphism by Mitscherlich afforded yet another means of checking the atomic weights. Besides these physical methods, chemical methods may also be used for fixing the atomic weights of the elements. Each of these methods ivill now be shortly referred to. (a) Volumetric Method. Gay-Lussac's Law of Volumes. Avogadro's Hypothesis Gay-Lussac, on the basis of an extensive series of experiments on the combining volumes of gases, established the law of gaseous volumes, which may be expressed as follows : Gases combine in simple ratios by volume, and the volume of the gaseous product bears a simple ratio to the volumes of the re- acting gases, when measured under the same conditions. A few years before, the same chemist had discovered that all gases behave similarly with regard to changes of pressure and temperature, and this fact, taken in conjunction with the law of volumes and the atomic theory, seemed to point to some simple relation between the number of particles in equal volumes of different gases. Berzelius suggested that equal volumes of different gases, under corresponding conditions of temperature and pressure, contain the same number of atoms. It was soon found, however, that this assumption was untenable, and the io OUTLINES OF PHYSICAL CHEMISTRY view held at the present day was first enunciated by the Italian physicist Avogadro. He drew a distinction between atoms, the smallest particles which can take part in chemical changes, and molecules, the smallest particles which can exist in a free con- dition, and expressed his hypothesis as follows : Equal volumes of all gases, under the same conditions of temperature and pressure, contain the same number of molecules. In expressing the results of determinations of the densities of different gases, hydrogen, as the lightest gas, is taken as standard, and the number expressing the ratio of the weights of equal volumes of another gas (or vapour) and hydrogen, measured under the same conditions, is the density of the gas (or vapour density in the case of a vapour). From Avogadro's hypothesis it follows at once that the ratio of the vapour densities of another gas and hydrogen, being a comparison of the relative weights of an equal number of molecules, is also the ratio of the molecular weights. It is usual to refer both atomic and mole- cular weights to the atom of hydrogen as unity, 1 and therefore the molecular weight, being referred to a standard half that to which the vapour density is referred, is double the vapour density. When the molecular weight is known, it is a comparatively simple matter to establish the atomic weight. As an example, we may employ the volumetric method to fix the atomic weight of beryllium, a matter of great historical interest. It was found by analysis that beryllium chloride contains 4*55 parts of beryllium to 3 5 '5 parts of chlorine by weight; in other words, the chemi- cal equivalent of beryllium is 4*55. If beryllium be regarded as a bivalent metal (p. 16), the formula for the chloride will be BeCl 2 , and its atomic weight 2. x 4-55 = 9-1. If, however, it is trivalent, the formula for the chloride must be BeCl 3 , and, to obtain the ratio for Be : Cl found experimentally, its atomic weight must be 4'55 x 3 ** I 3'^5- The vapour density of the chloride was de- termined by Nilson and Petterson, and from the result the mole- cular weight calculated as 8o'i. The molecule of beryllium 1 Strictly speaking, to the atom of oxygen as 16 (p. 18). FUNDAMENTAL PRINCIPLES OF CHEMISTRY n chloride cannot therefore contain more than 35-5 x 2 = 71 parts of chlorine, the formula for the chloride is BeCl 2 , and the atomic weight of beryllium 9*1. The determination of atomic weights by the volumetric method thus reduces to finding the smallest quantity of an element present in a molecule, referred to the atom of hydrogen as unity. If the molecular weights of a large number of vola- tile compounds containing a particular element are determined, it is practically certain that at least some of the compounds will contain only one atom of the element in question, and the pro- portion in which the element is present in these compounds is its atomic weight. In the above example, for instance, it has been assumed that only one atom of beryllium is present in the molecule of beryllium chloride of weight 8o'i, and the justification for this assumption is that no compound is known the molecule of which contains less than 9-1 parts of beryllium. It is clear that the numbers thus obtained are maximum values, and the possibility is not excluded that the true values may be fractions of those thus arrived at. The values generally accepted are, however, confirmed by so many independent methods that every confidence can be placed in their trustworthiness. (b) Dulong and Petit's Law In 1818, the French chemists Dulong and Petit enunciated the important kw that for solid elements the product of the specific heat and atomic weight is constant, amounting to about 6-4. This law is a very striking one when the great differences in the magnitude of the atomic weights are taken into account. Thus, the specific heat of lead the ratio of the quantity of heat required to raise i gram of the metal i in temperature to that required to raise the temperature of the same weight of water i is 0-031, and its atomic weight 207, the product being 6*4; whilst for lithium, with a specific heat of 0*9 and an atomic weight of 7, the product is 6-3. Since quantities of the different elements in the proportion of their atomic weights require the same amount 12 OUTLINES OF PHYSICAL CHEMISTRY of heat to raise the temperature by a definite number of degrees, the law may also be expressed as follows : The atoms of all ele- ments have the same capacity for heat. It is clear that this law can be used to determine the atomic weight of an element when the specific heat is known, the quotient of the constant by the specific heat giving the re- quired value. Dulong and Petit's law was largely used by Berzelius in fixing the values of the atomic weights. Like many other empirical laws, that of Dulong and Petit is only approximately true, the " constant " varying from about 6-0 to 6-7. This degree of concordance is, of course, quite sufficient for fixing the values of the atomic weights, as it is only necessary for this purpose to choose between a number and a simple multiple or submultiple. Moreover, the specific heat varies with the allotropic form of the element and with the temperature, and there is much uncertainty as regards the proper conditions for comparison. Regnault, who made a series of very careful determinations of specific heats, showed that most elements of small atomic weight, more particularly carbon, silicon and boron, have exceptionally small atomic heats. Later, how- ever, it was found that the specific heats of these elements increase rapidly with rise of temperature, and at high tempera- tures their behaviour is in approximate accordance with Dulong and Petit's law. This is clear from the accompanying table, showing the behaviour of carbon (diamond) and boron. CARBON (DIAMOND). BORON. Temp. Sp. Heat. Atomic Heat. Temp. Sp. Heat. Atomic Heat. 10 206 600 1000 0-II28 0-2733 0-4408 0-4589 i'33 3-25 5-28 5-5i 27 126 177 233 0-2382 0-3069 0-3378 0-3663 2'6l 3'4<> 370 4-02 The few elements which show this abnormal behaviour are of FUNDAMENTAL PRINCIPLES OF CHEMISTRY 13 low atomic weight, but the converse does not hold, as the atomic heat of lithium is normal. Some years after the introduction of Dulong and Petit's law, a similar law for compounds was enunciated by Neumann. He showed that, for compounds of similar chemical character, the product of specific heat and molecular weight is constant in other words, the molecular heats of similarly constituted com- pounds in the solid state are equal. In 1864, Kopp extended Neumann's law by showing that the molecular heat of solid compounds is an additive property, being made up of the sum of the atomic heats of the component atoms. It follows that in certain cases atoms have the same capacity for heat before and after entering into chemical combination. For ex- ample, the specific heat of calcium chloride is 0-174, the mole- cular heat is therefore 0-174 x in = 19-3, and the atomic heat of each atom 6-4. This law may be used to estimate the atomic heats of sub stances which cannot be readily investigated in the solid form, The atomic heat of solid oxygen in combination is about 4-0 and of solid hydrogen 2*3. (c) Isomorphism Mitscherlich observed that the corre- sponding salts of arsenic acid, H 3 AsO 4 , and phosphoric acid, H 3 PO 4 , crystallize with the same number of molecules of water, are identical, or nearly so, in crystalline form, and can be obtained from mixed solutions in crystals containing both salts, so-called mixed crystals. On the basis of these and similar observations, Mitscherlich established the Law of Isomorphism, according to which compounds of the same crystalline form are of analogous constitution. Thus, when one element replaces another in a compound without altering the crystalline form, it is assumed that one element has displaced the other atom for atom. The replacing quantities of the different elements are therefore in the ratio of their atomic weights, and if the atomic weight of one of them is known, that of the other can be calculated. This principle was largely used by Berzelius for fixing atomic i 4 OUTLINES OF PHYSICAL CHEMISTRY weights before the establishment of Dulong and Petit's law, and afforded a welcome corroboration of those obtained by the use of the law of volumes. The converse to the law of isomorphism does not hold, as elements may displace one another atom for atom with complete alteration of crystalline form. The principle of isomorphism is, however, somewhat in- definite, inasmuch as even the most closely related compounds are not completely identical in crystalline form, and it is difficult to decide where the line between similarity and want of similarity is to be drawn. Thus the corresponding angles for the naturally-occurring crystals of the carbonates of cal- cium, strontium and barium are: Aragonite, 116 10'; Stron- tianite, 117 19'; Witherite, 118 30'. Tutton, 1 from a careful comparative study of the sulphates and selenates of potassium, rubidium and caesium, has shown that each salt has its own specific interfacial angle, but the differences produced by dis* placing one metal of the alkali series by another does not exceed i of arc, and is usually much less. The three most important characteristics for the establishment of isomorphism are : (1) The capacity of forming mixed crystals. The miscibility must be complete, or within fairly wide limits of concentration. (2) Similarity of crystalline form, which must include at least approximate agreement in the values of the geometrical con- stants. (3) The capacity of crystals of one substance to increase in size in a saturated solution of the other. (d) Determination of Atomic Weights by Chemical Methods It is evident from the considerations advanced in the section on the determination of atomic weights by volu- metric methods (p. 10) that if the composition of a binary compound containing one or more atoms of an element such as hydrogen or chlorine for each atom of an element of unknown atomic weight has been determined by analysis, and if further the relative number of atoms of hydrogen or chlorine present is 1 Science Progress, 1906, i, p. 91. FUNDAMENTAL PRINCIPLES OF CHEMISTRY 15 known, the atomic weight of the other element can at once be calculated. In the case of beryllium chloride, it has been shown that the number of chlorine atoms present can be deter- mined by a physical method (p. 10), but such determinations can sometimes be made by purely chemical methods. As an illustration, we will consider the determination of the atomic weight of oxygen. Analysis shows that water contains approxi- mately i part of hydrogen to 8 parts of oxygen by weight. If the molecule of water contains one atom each of hydrogen and oxygen, its formula must be HO and the atomic weight of oxygen will be 8 ; if, on the other hand, two atoms of hydrogen are present, the formula must be H 2 O and the atomic weight of oxygen must be 1 6 in order to obtain the ratio between the weights of the elements found experimentally. It has been found that by the action of metallic sodium half the hydrogen in water can be displaced, and as by definition atoms are indi- visible, this indicates that the molecule of water contains two (01 a multiple of two) atoms of hydrogen. The (probable) formula for water is therefore H 2 O and the atomic weight of oxygen 16. It will be evident that, as in the case of the volumetric method, the value thus obtained for the atomic weight is a maximum and further experiments are necessary to fix the value definitely. Relation between Atomic Weights and Chemioal Equivalents. Yalency The exact proportions in which the elements enter into chemical combination are determined by analysis, and the numbers thus obtained, referred to a definite standard, represent, according to the atomic theory, the atomic weights, or simple multiples or sub-multiples of the atomic weights, of the respective elements. The choice between several possible numbers is based on the methods discussed in the foregoing paragraphs, more particularly on Avogadro's hypo- thesis, and the fact that these independent methods give the same values affords strong evidence that the numbers thus ob- tained are the true ones a view which obtains still further 1 6 OUTLINES OF PHYSICAL CHEMISTRY support from the periodic classification of the elements due to Mendeleeff (1869). The ordinary chemical formulae with which the student is familiar are based on the atomic weights thus obtained. For example, the formulae of a number of compounds containing only hydrogen and one other element are as follows : HC1, H 2 O, NH 3 , CH 4 . It is evident from these formulae that the power of different elements to combine with hydrogen is very different ; whilst one atom of chlorine combines with only one atom of hydrogen, one atom of carbon can become associated with no less than four atoms of hydrogen. The combining capacity of an element for hydrogen or other univalent element is termed the valency of an element, chlorine being a univalent and carbon a quadrivalent element. A little consideration of the above formulae will make clear the relationship between the atomic weight and the chemical equivalent of an element. It is clear that an amount of one element equivalent to its atomic weight may combine with (or displace) i, 2, 3 or more parts of hydrogen by weight, depending on its valency. Since the chemical equivalent of an element is that amount of it which can combine with or displace one part by weight of hydrogen it follows that Atomic weight ~, , , s_ = Chemical equivalent. Valency As has been indicated in the foregoing paragraphs, the atomic weight and the chemical equivalent are often deter- mined more or less independently and the quotient of the two values is the valency. In other cases, however (for example, the volumetric method and the chemical method), the chemical equivalent and the valency are determined, and the product of the two is the atomic weight. The Values of the Atomic Weights After the establish- ment of the law of multiple proportions and the formulation of the atomic theory by Dalton, it became a matter of the utmost importance for chemists to determine the atomic weights of FUNDAMENTAL PRINCIPLES OF CHEMISTRY 17 the elements with the greatest possible accuracy. This task was undertaken by Berzelius, who, in the course of about six years (1810-1816), fixed the combining weights of most of the known elements. Since then, the determination of atomic weights has proceeded regularly, but on two occasions a special impulse was given to these investigations. The first occasion was a suggestion by Prout that the atomic weights are exact multiples of that of hydrogen. The idea under- lying this assertion was that hydrogen is the primary element, the other elements being formed from it by condensation. The results of Berzelius were incompatible with Prout's hypothesis, but as the atomic weights of certain elements un- doubtedly approximated to whole numbers, Stas made a number of atomic weight determinations with a degree of accuracy which has only been improved upon in quite recent times. The results obtained by Stas completely disposed of Prout's hypothesis in its original form. The second event which stimulated atomic weight investiga- tions was the development of the periodic classification of the elements. In certain cases, the order of the elements, arranged according to their atomic weights, did not correspond with their chemical behaviour, and Mendeleeff asserted that in these cases the commonly accepted atomic weights were inaccurate. The investigations undertaken to test these suggestions afforded striking confirmation of Mendeleeff's views in some cases, but not in others. As regards recent progress in this branch of investigation special mention should be made of the determina- tion of the combining ratios of hydrogen and oxygen by Morley l and of the comprehensive and masterly investigations of T. W. Richards and his co-workers. 2 As the combining weights are relative, it is necessary to fix on a standard to which they may be referred. Dalton took the atomic weight of hydrogen, the lightest element, as unit, but 1 Smithsonian Contributions to Knowledge, 1895. 2 See, for example, J. Amer. Chem. Soc., 1907, 29, 808-826. 2 1 8 OUTLINES OF PHYSICAL CHEMISTRY Berzelius, from practical considerations, proposed oxygen as standard, putting its atomic weight = 100. The justification for this procedure is that very few elements form compounds with hydrogen suitable for analysis ; the majority of determina- tions have been made with compounds containing oxygen, and until comparatively recently the ratio of the atomic weights of hydrogen and oxygen was not accurately known. Although the hydrogen standard again came into use after the time of Berzelius, mainly because hydrogen was taken as a standard for other properties, yet in more recent times the oxygen standard has again come most largely into use, the atomic weight of that element being taken as 16*00. The unit to which atomic weights are referred is therefore ^ of the atomic weight of oxygen, and is rather less than the atomic weight of hydrogen. 1 Besides the advantage already mentioned, the atomic weights of more of the elements approximate to whole numbers when the oxygen standard is used, which is a distinct advantage, since round numbers are generally used in calculations. Chemical equivalents, like atomic weights, should be referred to the oxygen standard, and the chemical equivalent of an element is a number representing that quantity of it which combines with, or displaces, 8 parts by weight of oxygen. The arguments in favour of the oxygen standard seem con- clusive, and as it is very confusing to have two standards in general use, it is very satisfactory that the International Com- mittee on Atomic Weights now use the oxygen standard only. 1 According to the recent determinations of Morley, Rayleigh and others the atomic weight of oxygen is about 15*88 when hydrogen is taken as unit. It follows that on the oxygen standard, O = 16-00, the atomic weighf. of hydrogen is about i'oo8. FUNDAMENTAL PRINCIPLES OF CHEMISTRY 19 INTERNATIONAL ATOMIC WEIGHTS (1912) Elements. Sym- bols. At. Wt. = i6. Elements. Sym- bols. At. Wt. O = 16. Aluminium Al 2 7 -I Neodymium . Nd I 44'3 Antimony . Sb I20'2 Neon Ne 20'2 Argon A 39-88 Nickel Ni 58-68 Arsenic As 74-96 Niton Barium Ba I3737 (Radium Emana- Bismuth Bi 208-0 tion) Nt 222-4 Boron . B ii-o Nitrogen . N 14-01 Bromine . Br 79-92 Osmium Os 190-9 Cadmium . . Cd 112-40 Oxygen 16*00 Caesium . Cs 132-81 Palladium . Pd 106-7 Calcium Ca 40-07 Phosphorus P 31-04 Carbon C I2'OO Platinum . Pt 195-2 Cerium Ce 140-25 Potassium . K 39-10 Chlorine . Cl 35-46 Praseodymium . Pr 140-6 Chromium . Cr 52-O Radium Rd 226-4 Cobalt Co 58-97 Rhodium . Rh 1 02 -9 Columbium Cb 93-5 Rubidium . Rb 85-45 Copper Cu 63-57 Ruthenium Ru 101-7 Dysprosium Dy 162-5 Samarium . Sa 150-4 Erbium Er 167-7 Scandium . Sc 44-1 Fluorine . F 19-0 Selenium . Se 79-2 Gadolinium Gd I 57'3 Silicon Si 28-3 Gallium Ga 69-9 Silver . Ag 107-88 Germanium Ge 72-5 Sodium Na 23-00 Glucinum . Strontium . Sr 87-63 (beryllium) . Gl 9-1 Sulphur S 32-07 Gold ... Au 197-2 Tantalum . Ta 181-5 Helium He 3*99 Tellurium . 9 . Te 127-5 Hydrogen . . H 1-008 Terbium Tb 159-2 Indium In 114-8 Thallium . Tl 204-0 Iodine . I 126-92 Thorium . Th 232-4 Iridium . Ir 193-1 Thulium . Tm 168-5 Iron . Fe 55-84 Tin . Sn 119-0 Krypton Kr 82-9 Titanium . Ti 48-1 Lanthanum La 139-0 Tungsten . W 184-0 Lead . Pb 207-10 Uranium . U 238-5 Lithium Li 6-94 Vanadium . V 51-0 Lutecium . Lu 174-0 Xenon Xe 130-2 Magnesium Mg 24-32 Ytterbium Manganese Mercury Mn H g 54-93 200-6 (Neoytterbium). Yttrium Yb Yt 172*0 89-0 Molybdenum Mo 96-0 Zinc . Zn 65-37 Zirconium . . Zr 90-6 Only significant figures are given in the table. Where no figure follows the decimal point, the value of the first decimal is uncertain. 20 OUTLINES OF PHYSICAL CHEMISTRY The Periodic System It was early observed that there are some remarkable relationships between the magnitude of the atomic weights of the elements and their chemical behaviour. The most important observation in this connection is that the differences in the atomic weights of successive members of the same group of elements are approximately 16 or a multiple of that number. Thus for the halogen group, F = 19, Cl = 35*5, Br = 80, I = 127, the differences between each element and its immediate predecessor are 16-5, 44-5 and 47 respectively, the latter two numbers being approximately 3x16. Further, for the members of the alkali group, Li = 7, Na = 23, K = 39, Rb = 85*5, Cs = 132*9, the differences are 16, 16, 46*5 and 47*2 respectively. In 1864, a considerable advance was made by the English chemist Newlands, which is summarised in the law of octaves. He pointed out that when the elements, beginning with lithium, are arranged in the order of ascending atomic weights, there is a gradual variation in properties till the eighth element is reached ; this element (sodium) shows a strong resemblance to the first element, lithium, the ninth element, magnesium, is similar in chemical behaviour to beryllium, and so on. The first fourteen elements may therefore be arranged as follows : Li=*7 Be = 9 B = n C=i2 N = i4 O=i6 F=i9 Na=2 3 Mg=2 4 Al=2 7 Si = 28 P = 3 i 8 = 32 = 35-5 and the elements which show similar chemical behaviour are thus brought into the same vertical row. On these lines, but without any knowledge of the views of Newlands, a complete system for classifying the elements, termed the periodic system was later developed by Mendeleeff. The system is based on the observation that when the elements are arranged in the order of ascending atomic weights, elements with similar chemical properties recur at regular intervals. O Ii w 3 I ro Jl u CQ B >. so fc fc s ro II CO N 8 II ii r O vo j^ ^T " w i ! ii 4 & w w 22 OUTLINES OF PHYSICAL CHEMISTRY The accompanying table (p. 2 i), in which the atomic weights are only approximate, is practically the same as that proposed originally by Mendeleeff. Starting with helium = 4 (which was unknown in Newlands' time) we have the arrangement shown in the first line of the table, in which the properties vary regularly from the first member to fluorine. The next element, neon = 20, is an inactive gas, and is therefore placed below helium, sodium falls into its proper place below lithium, and so on. The first and second periods possess 8 elements each. A third period is started with potassium, but in this case it is necessary to pass over 18 elements before another metal (rubidium), bearing a close resemblance to potassium, is reached. Such a period of 18 elements is termed a long periodic contrast to the two short periods of 8 elements each. The whole table is made up of two short and five long periods, but four of the long periods are . incomplete and the last one contains only three elements. The positions of the elements in these periods are fixed by their chemical relationships with those above them (in the vertical rows), and it is assumed that the blanks indicate the positions of elements which have not yet been discovered. The arrangement of the three intermediate elements in each of the first three long periods presented a certain difficulty, and Mendeleeff put them in a group by themselves, the so-called eighth group (group vm. in the table). A study of the elements arranged as above reveals many striking regularities. Thus the valency with regard to hydrogen increases regularly up to the middle of a short period and then falls to unity, whilst the valency for oxygen increases regularly from the beginning to the end of a period. Helium and the elements in the same vertical row do not enter into chemical combination, and may therefore be regarded as having zero valency. The valency relations in the long periods are not quite so regular, being complicated by the fact that most of the elements have several valencies. Many of the physical properties of the elements, such as the FUNDAMENTAL PRINCIPLES OF CHEMISTRY 23 melting-point, the atomic volume and the density, also vary regularly within each period. For example, the melting-points in the first series gradually rise from helium to carbon and fall again to fluorine, and similarly the elements of highest melting- point (iron, cobalt, nickel, etc.) occur in the middle of the long periods. Besides this variation of physical properties in the horizontal series, there is a similar, but much less marked, variation in the vertical series ; in the case of the alkali metals, for example, there is a gradual fall in the melting-point from lithium to caesium. Not only the physical properties, but also the chemical properties of the elements vary regularly within the periods. Thus the elements on the extreme left hand of the table are inactive gases, those in the second group decompose water and are strongly electropositive, at the middle of the period they appear to be electrically indifferent (carbon, silicon) and towards the right hand strongly electronegative. The statements in the last three paragraphs are summarised in the periodic law, due to Mendeleeff, which may be expressed as follows : The properties of the elements^ as well as the proper- ties of their compounds, are periodic functions of the atomic weights. The arrangement of the elements according to the periodic system is not in all respects satisfactory. Copper, silver and gold do not fit very well into their positions beside the alkali metals, and it has been suggested that they belong more properly to the eighth group, coming after nickel, palladium and platinum respectively. Further, the atomic weight of argon is greater than that of potassium, but the former element must undoubtedly precede the latter in the periodic table. The question which has raised most discussion in this connection, however, is the relative position of tellurium and iodine. Although from its chemical relationships the latter element must follow tellurium, yet experiment shows that the atomic weight of tellurium is greater than that of iodine. It is at first 24 OUTLINES OF PHYSICAL CHEMISTRY natural to suppose that there must have been some mistake in determining the atomic weights, but the recent work of Laden - burg, Puccini, Kothner, Brereton Baker 1 and others leave practically no room for doubt that the facts are as stated. It is unquestionable that the periodic system is of great value, but the above considerations indicate that it is only a first approxi- mation to a satisfactory system. The periodic system is of use mainly in three ways : (a) As a system of classification which indicates in a fairly satisfactory way the chemical and physical relationships of the elements. () For predicting the existence and properties of elements hitherto undiscovered. (c) For enabling us to fix the correct values of the atomic weights of elements which do not form volatile compounds. When the periodic system was first brought forward, there were more blanks in the table than there are at the present day, and MendeleefT not only suggested that the positions of these blanks corresponded with hitherto undiscovered elements, but even foretold the properties of the missing members of the series from the known properties of the elements near them in the periodic table. It is an interesting historical fact that within a few years three of the blanks had been filled by ele- ments gallium (1875), scandium (1879), germanium (1886) having in all respects the properties foretold by Mendeleeff. The use of the periodic system, for fixing atomic weights will be readily understood from the foregoing. When the equivalent of the element has been determined, it is usually possible to decide which multiple of it is to be taken, as there will in general be only one position in the table into which the element can be satisfactorily fitted. 1 Trans. Chetn. Soc., 1907, 91, 1849. CHAPTER II GASES The Gas Laws The gaseous form of matter is charac- terised by its tendency to fill completely and to a uniform density any available space. In general, gases are less dense than other forms of matter, and their internal friction is much less. In consequence of this, the laws expressing the behaviour of gases under varying conditions are much simpler than those holding for liquids and solids. The most striking fact about these laws is that they are to a great extent inde- pendent of the nature of the gas : the volume of all gases is affected by changes of temperature and pressure to much the same extent. The well-known laws which represent more or less accurately the behaviour of all gases under varying conditions may be enunciated as follows : - 1. At constant temperature, the volume, v, of a given mass of any gas is inversely proportional to the pressure, p ; otherwise expressed, pv = constant (Boyle, 1662). 2. At constant pressure, the volume, v, of a given mass of any gas is proportional to its absolute temperature, T (273 + temp. Centigrade] (Gay-Lussac, 1802). 3. At constant volume, the pressure of a given mass of any gas is proportional to its absolute temperature. These laws are not independent ; when any two of them are known, the third can readily be deduced. The three laws just given may be summarised in a single 25 26 OUTLINES OF PHYSICAL CHEMISTRY equation, which represents the behaviour of a gas when any two of the determining factors are varied. Let / , v and T repre- sent the original pressure, volume and temperature of a definite quantity of a gas, and p lt v l and 1\ the final values. Suppose that at first the pressure is altered from / to its final value/! at constant temperature, then, by Boyle's law, the gas will have a new volume, V, given by the equation / # = p-^T. Then, keeping the pressure constant at p lt alter the temperature from T to the final value T lf the final volume, v lt will, by Gay-Lussac's law, be given by the equation V/T = s^/Tj. Substituting in the last equation the value of V obtained from the former equation (V = /oV/i) we obtain P Q V Q p^v, ^ = S*H = constant. L o M This may be written in the form pv rT where r is a constant ; in other words, the product of the pressure and volume of a gas is proportional to the absolute temperature. At a definite temperature and pressure, the volume of the gas', and consequently the value of r, will be proportional to the quantity of gas taken. Further, according to Avogadro's hypothesis, the molecular weight in grams of all gases occupies the same volume under the same conditions. It follows that for these quantities the constant r will have the same value for all gases, quite independent of the conditions under which the gases are measured. This special value of the constant may conveniently be represented by R, and we then obtain the equation PV = RT, where V is the volume occupied by the molecular weight of a gas in grams, at the absolute temperature T and under the pressure P an equation which is of fundamental importance for the behaviour of gases and also for dilute solutions. The molecular weight of a gas in grams, which, according to the atomic theory, represents the weight of the same number of molecules in each case, is conveniently termed a mol (Ostwald). GASES 27 The numerical value of R, in C.G.S. units, may readily be calculated from the accurate observations of the densities of gases made by Regnault, Rayleigh and others. There is, how- ever, a little uncertainty in the calculation owing to the fact that the volumes occupied by a mol of different gases under equiva- lent conditions are not quite the same, although very nearly so. Thus 2 -oi 6 grams of hydrogen, 32-00 grams of oxygen and 28*02 grams of nitrogen occupy 22*43, 22 '39 ar >d 22*40 litres respectively at o and 76 cms. Taking 22*40 litres as a mean value, and substituting the values for T (273) and P (76 x 13*59 = 1033*3 grams per sq. cm.), we obtain PV low* x 22,400 ergs As the pressure is measured in gram/cm. 2 , the volume is of the dimensions cm. 8 , and T is merely a number, the above value for R is of the form gram x cms. or gram-centimetres. The calorie, the ordinary heat unit, is equal to 42,640 gram-centi- metres = 41,830,000 ergs, so that the value of R is almost ex- actly double (accurately 1*99 times) that of a calorie. We may therefore write the gas equation in the simplified form PV = i*99T, but the approximate form PV = 2T is sufficiently accu- rate for many purposes. In this form the gas equation is repre- sented in thermal units. The product P V in the gas equation is of the nature of energy, as is clear from the fact that when a volume, v t of a gas is gener- ated under constant external pressure (say that of the atmosphere) the work done is proportional to the volume and to the pressure overcome, and therefore to their product. The work done by or upon a gas when it changes its volume under a constant ex- ternal pressure can readily be obtained in thermal units by using the second form of the gas equation given above. Thus if a mol of a gas is generated at o under the pressure of the atmos- phere, the amount of heat absorbed in performing the external work of expansion, PV, is 2! = 2 x 273 = 546 cal. Since PV is constant, the pressure under which a definite a8 OUTLINES OF PHYSICAL CHEMISTRY mass of a gas is generated at a definite temperature has no influence on the external work of expansion. Thus, to take the above illustration, if a mol of a gas is generated under a pressure of atmosphere, the volume will be 22-4 x 10 = 224 litres, and the work done will again be 546 cal. at o. Deviations from the Gas Laws Careful experiment shows that although the gas laws, which are summarised in the general formula PV = RT, give a general idea of the behaviour of gases, yet they do not represent accurately the behaviour of any single gas, the deviations depending both on the conditions of observation and on the nature of the gas. It may be said, in general, that the laws are the more nearly obeyed the higher the temperature and the smaller the pressure, and, as regards the nature of the gas, the further it is removed from the temperature of liquefaction. A gas which would folloM the gas laws accurately is called a perfect or ideal gas, and ordinary gases approach more or less nearly to this ideal behaviour. The accompanying figure (Fig. i) gives a graphic representa- tion of the behaviour of the three typical gases, hydrogen, nitrogen and carbon dioxide, according to Amagat. The pro- duct PV, in arbitrary units, is represented on the vertical axis and the pressure P, in atmospheres, along the horizontal axis. If PV were constant (Boyle's law), the curves would be straight lines parallel to the horizontal axis. Actually, PV increases continuously with the pressure in the case of hydrogen, and for nitrogen and carbon dioxide it first decreases, reaches a mini- mum, and beyond that point increases with increase of pres- sure. All gases except hydrogen show a minimum in the curve, which indicates that the compressibility is at first greater than corresponds with Boyle's law, reaches a point (which differs for different gases) at which for a short interval Boyle's law is followed, and beyond that point is less compressible than the law indicates. Hydrogen, on the other hand, is always less GASES 29 compressible than the law requires at ordinary temperatures, but at very low temperatures it would also probably show a minimum in the curve. That the deviations from the simple law become less the higher the temperature, is very well illus- trated by the curves for carbon dioxide at 35*1 and 100. Mercury) 2O 40 6O 80 IOO 120 140 160 1 80 20O 22O 240 260 28O 3 which, since the volume, v, of the cube is /*, can be put in the more convenient form, p = ^mnc^jv or pv = ^mn = \rnnc* From the above equation, which has been derived on certain more or less plausible assumptions regarding the constitution of gases, some of the laws which have been obtained experimentally may readily be deduced. Since on the assumptions made in deducing the general 32 OUTLINES OF PHYSICAL. CHEMISTRY formula the right-hand side of the equation is made up of factors which are constant at constant temperature, the product of pressure and volume must also be constant, which is Boyle's law. Moreover, the above equation may be written in the form pv = . \rnnc 1 . As shown in mechanics, the expression \m indicating that at the latter temperature it is completely split up into iodine atoms. Bromine is also partially decomposed at 1500, and chlorine commences to split up about the same temperature. It had previously been shown by Deville and Troost that the molecular weight of sulphur also diminishes with increasing temperature, and above 800 gives results which indicate that only diatomic molecules are present. Nernst 1 has quite recently succeeded in extending this method up to 2000 by using a vessel of iridium coated outside and inside with a paste of magnesia and magnesium chloride, and heated in an electric furnace. At this temperature, the molecular weight of mercury is 201, indicating that the atoms of this element have undergone no further simplification, whilst sulphur, between 1800 and 2000, has a density of about 24, indicating that the diatomic molecules are split up, to the ex- tent of about 33 per cent., into single atoms. Association and Dissociation in Gases We have al- ready seen that such substances as sulphur and arsenic have abnormally high molecular weights at low temperatures ; such substances are said to be associated. This peculiarity is not confined to elements, as the molecular weight of acetic acid, which, as determined by chemical methods, is 60, exceeds 100 when determined by the vapour density method at comparatively low temperatures. The conclusion that acetic acid in the form of vapour at comparatively low temperatures consists largely of double molecules (CH 3 COOH) 2 , is in satisfactory agreement with other considerations. 1 Compare Wartenberg, loc. cit. 42 OUTLINES OF PHYSICAL CHEMISTRY An apparent deviation from Avogadro's hypothesis of a different nature is met with, for example, in the case of gaseous ammonium chloride. On chemical grounds, the molecular formula, NH 4 C1, is given to this substance, corresponding with a molecular weight of 53-5, whereas the observed value, obtained from its vapour density, is only half as great. This behaviour could be accounted for on the assumption that, at the tem- perature of the experiment, the molecule is to a great extent split up, or dissociated, into NH 3 and HC1 molecules, and the experimental justification for this assumption has been obtained by Pebal (1862), who effected a partial separation of the decomposition products by taking advantage of their different rates of diffusion. It may be added that in the complete absence of moisture, ammonium chloride can be vaporized without dissociation, and then has the normal molecular weight deduced by means of Avogadro's hypothesis. 1 Accurate Determination of Molecular and Atomic Weights from Gas Densities We have seen that Avogadro's hypothesis does not hold strictly for actual gases, and that the reason for this is probably to be found in the mutual attractions and finite volumes of the gas particles. We may, therefore, assume that it would be strictly true for an ideal gas, and, on the basis of van der Waals' equation, apply a correction to actual gases to find their true molecular weights, that is, the relative masses which would occupy equal volumes at great rarefaction, when the gas laws would be strictly followed (p. 28). The method followed is therefore to determine the volume of a definite mass of a gas under two or more pressures (the compressibility of the gas), and find by extrapolation the relative densities of different gases as the pressure approaches zero. This method has been used more particularly by Daniel Berthelot and by Lor d Rayleigh. From the results, the follow- *H. Brereton Baker, Trans. Chem. Society, 1894, 65, 6n ; 1898,73, 422. Compare Johnston, Zeitsch. physikal Chem., 1908, 61, 457. GASES 43 ing molecular weights (vapour density x 2) were calculated by Berthelot (oxygen = 32 being taken as the standard) : H 2 N 2 CO O 2 CO 2 N 2 O HC1 2*0145 28*013 28*007 32*000 44*000 44*000 36-486 From these observations, the following atomic weights have been obtained, the values derived by chemical methods being placed below for comparison : O H C N Cl Gas density 16*000 1-0075 12-000 14-005 35*479 Chemical 16*000 1*008 12-00 14*01 35*45 The agreement, except in the case of chlorine, is excellent. As a matter of fact, the chemical value for chlorine is probably too low ; the recent investigations of Richards and Wells l appear to show that the true value is 35*473, almost identical with that obtained by the density method. The above striking results lend strong support to the assump- tion that in the limit Avogadro's hypothesis is strictly valid for all gases. SPECIFIC HEAT OF GASES General The specific heat of any substance may be defined as the ratio of the amounts of heat required to raise i gram of the substance in question and i gram of water through a given range of temperature. The amount of heat required to raise i gram of water i in temperature is termed a calorie, and hence the specific heat may also be defined as the quantity of heat in calories required to raise i gram of the substance i in tem- perature. This statement has only a definite meaning, however, when the conditions under which the heating is carried out are stated, and this is particularly true of gases. If a gas is suddenly compressed it becomes warmer, although no heat has been supplied to it, and, conversely, if a gas is allowed to expand against pressure it becomes cooled, although no heat has been abstracted from it. According to the above definition, i y. A mer. Chem. Soc., 1905, 27, 459. 44 OUTLINES OF PHYSICAL CHEMISTRY amount of heat supplied Specific heat = -. *-*- nse in temperature so that if a gas is warmed by compression its specific heat is zero. Moreover, if, while a gas is expanding against pressure, sufficient heat is supplied to keep its temperature constant, the heat supplied has a certain finite value whilst the change of tempera- ture is zero, so that the specific heat, according to definition, is infinite. It is clear that the specific heat of a gas may have any value whatever, unless the conditions under which it is measured are stated. Specific Heat at Constant Pressure, G p , and Constant Volume, C, There are two important cases in which the term " specific heat of a gas " is clearly defined : (a) the specific heat at constant volume, C,, (b) the specific heat at constant pressure, C p . In the former case, the volume is kept constant whilst the gas is being heated, and no external work is done. In the latter case, the volume is allowed to increase whilst heat is being supplied, work is therefore done against the pressure of the atmosphere, which tends to cool the gas. Sufficient heat must therefore be supplied not only to raise the temperature, but to make up for the cooling due to the external work performed. It is clear that the specific heat at constant pressure is greater than that at constant volume, and the difference is the heat equi- valent of the amount of work done against the external pressure. The difference between the two specific heats may readily be obtained in thermal units by using the general gas equation. For this purpose, it is convenient to deal with a mol of a gas. It has already been shown (p. 27) that when a gas expands at constant pressure, the work done is measured by the product of the pressure and the change of volume. If at first the absolute temperature is T lf we have the equation PV l = RTj where V 1 is the molecular volume. If the temperature is raised to T 2 , and the new molecular volume is V 2 , the work done during the expansion is P(V 2 -V 1 ) = R(T 2 -T 1 ). GASES 45 In the present case, T 2 - Tj is i, therefore P(V 2 - V t ) = R. Further, the difference in the molecular heats of a gas at constant pressure and constant volume is the external work done when a mol of gas is raised i in temperature, and there- fore M (C P C v ) (where M is the molecular weight of the gas) is also = P (V 2 - Vj). Hence M (C p - C,) - R. In thermal units, R is approximately 2 calories, so that the difference of the specific heats of a mol of any gas in other words, the difference of the molecular heats of any gas at constant pressure and at constant volume is 2 calories. The specific heat of a gas at constant pressure can readily be determined by passing a known quantity of it, heated to a definite temperature, through a metallic worm in a calorimeter, at such a rate that there is a constant difference of temperature between the entering and issuing gas. It is more difficult to determine directly the specific heat at constant volume, and this has only been accomplished satisfactorily in comparatively recent times. 1 The molecular heats MC, and MC P (molecular weight x specific heat) of a few of the commoner gases are given in the accompanying table, the values of C being obtained from those of C p by subtracting 2 calories : Specific Gas. Heat, MCj,, MC tf CJC V C P Argon . _ 4-98 2-98 1-66 Helium . 66 Mercury 2-965 66 Hydrogen 3-409 6-880 4-880 412 Oxygen 0-2175 6-960 4-960 40 Hydrogen chloride Chlorine 0-1876 0-1241 6-84 8-820 4-84 6-820 409 29 Nitrous oxide 0-2262 9'99 7-99 247 Ether . 0-4797 35-5I 33'5i 060 1 Joly, Proc. Roy. Soc., 1889 47, 218. Compare Preston, Theory of Heat, p. 239. 46 OUTLINES OF PHYSICAL CHEMISTRY For diatomic molecules, the average value of the molecular heat at constant volume is about 4-8 calories in the neighbour- hood of 100; but chlorine and bromine are exceptions. For triatomic molecules the average value of MC t is 6-5 cal. and the value increases with the complexity of the compound, as is illustrated in the table. Specific Heat of Gases and the Kinetic Theory- Much light is thrown on the question of the specific heat of gases by the kinetic theory. According to this theory the energy-content of a gas is made up of three parts: (i) the energy of rectilineal (progressive motion of the molecules), the so-called kinetic energy (p. 32) ; (2) the energy of intramolecular motion ; (3) the potential energy due to the mutual action of the atoms ; 1 and when heat is supplied to a gas at constant volume all three factors of the energy may be affected. For monatomic gases, however, such as mercury vapour, the factors (2) and (3) are presumably absent, and the heat supplied must simply be employed in increasing the kinetic energy of the molecules. We have already learnt (p. 32) that the kinetic energy of i mol of any gas = f PV = 3T if expressed in thermal units. When a gas is raised at constant volume from the absolute temperature Tj to T 2 we have for the kinetic energies at the two temperatures the equations f PjV = 3^ and f P 2 V = 3T 2 , where Pj and P 2 are the pressures at T 1 and T 2 respectively. Subtracting the first equation from the second, we obtain f (Pj-PjJV = 3(T 2 -T!) and for a rise of temperature of i f (P 2 - Pj)V = 3 (calories). Therefore the molecular kinetic energy of a monatomic gas is increased by 3 calories for a rise of i in temperature, or, in other words, the molecular heat MC, of a monatomic gas at constant volume is 3 calories. As the specific heat at constant pressure is 3 + 2 = 5 calories, the ratio, MC P /MC V , for a monatomic gas must be r66, if the assumptions we have made on the basis of the kinetic theory are justified. As has already been mentioned, C e is somewhat difficult to 1 Boltzmann, he. cit., ?, 54.. GASES 47 determine directly, and to test the above deduction from the kinetic theory it is simpler to determine the ratio C P /C, in- directly, which can be done in various ways, for example, by measuring the velocity of sound in a gas. Kundt and Warburg (1876) therefore determined the velocity of sound in mercury vapour and obtained for the above ratio the value r66, in exact accord with the theoretical value, undoubtedly one of the most striking triumphs of the kinetic theory. Conversely, a gas for which the ratio C P /C, is r66 must be monatomic, and by this method Ramsay showed that the rare gases argon and helium are monatomic. For gases containing two or more atoms in the molecule, the heat supplied is employed not only in accelerating the rectilinear motion of the particles, but also in performing internal work in the molecule. As the former effect alone requires 3 calories, the total molecular heat of a polyatomic gas will be 3 + calories, where a is a positive quantity, constant for any one gas. The value of MCp will be 5 + a calories, and the ratio of the specific heats will be MC P 5 + a less than 1-67 but greater than i. A comparison of the numbers given in the table shows that this deduction is in complete accord with the experimental facts. It may be expected that the more complex the molecule the greater will be the amount of heat expended in performing internal work and therefore the greater will be the specific heat. In accordance with this, MC, for i mol of ether vapour is 33*5 calories, and for turpentine (C 10 H 16 ) 66'8 calories. The specific heat of monatomic gases is independent of temperature, that of polyatomic gases usually increases slowly with temperature. Experimental Illustrations Experiments with gases are usually somewhat difficult to perform, and require special ap- paratus. Experimental illustrations of the simple gas laws are 48 OUTLINES OF PHYSICAL CHEMISTRY described in all text-books on physics, and need not be con- sidered here. The determination of the density l and hence the molecular weight of such a gas as carbon dioxide by Regnault's method may be performed as follows : One of the bulbs is first exhausted as completely as possible by means of a pump, the stop-cock closed, and the bulb weighed. It is then filled with water by opening the stop-cock while the end of the tube dips under the surface of water and again weighed. The volume of the bulb is obtained by dividing the weight of the water by its density at the temperature of the experiment. The water is removed from the bulb by means of a filter-pump, the interior of the bulb is dried (by washing out with alcohol and ether and warming), pkced nearly to the stop-cock in a bath at constant temperature, the end is then connected to a T piece bv means of rubber tubing ; one of the free ends of the T piece is connected, through a stop-cock or rubber tube and clip, to a pump, the other, also through a stop-cock or rubber tube and clip, to an apparatus generating carbon dioxide. The bulb is evacuated by means of the pump, the stop-cock connecting it with the latter is then closed, that connecting it with the carbon dioxide apparatus opened, the bulb filled with carbon dioxide, disconnected and weighed. As the apparatus fills it with carbon dioxide at rather more than atmospheric pressure, the stop-cock is opened for a moment to adjust it to atmospheric pressure before weighing. The weight of a known volume of the gas at known temperature and pressure having thus been determined, its density and molecular weight can readily be calculated. The determination of vapour densities by Victor Meyer's method is fully described on page 38, and may readily be performed by the student with ether or chloroform, steam being used as jacketing vapour. i For full details as to the manipulation of gases, consult Travers 1 Experimental Study of Gases (Macmillan, 1901). CHAPTER III LIQUIDS General Liquids, like gases, have no definite form, but, unlike the latter, they have a definite volume, which is only altered to a comparatively small extent by changes of tempera- ture and pressure. In contrast to the simple gas laws, the formulae connecting temperature, pressure and volume of liquids are very compli- cated and empirical in character, and depend also on the nature of the liquid. This is, of course, connected with the fact that liquids represent a much more condensed form of matter than gases. i c.c. of liquid water at 100, when converted into vapour at the same temperature, occupies a volume of over 1600 c.c. It seems plausible to suggest that the main reason why the formulae representing the behaviour of liquids are so much more complicated than the gas laws is that the mutual attraction of the particles, which is almost negligible in the case of gases (p. 34), is of predominant importance for liquids. As is well known, gases can be liquefied by increasing the pressure and lowering the temperature ; and, conversely, by raising the temperature and diminishing the pressure a liquid can be changed to a gas. It is shown in the next section that there is no difference in kind, but only a difference in degree, between liquids and gases. Transition from Gaseous to Liquid State. Critioal Phenomena If gaseous carbon dioxide, below 31, is con- fined in a tube and the pressure on it gradually increased, a point will be reached at which liquid makes its appearance in 4 40 OUTLINES OF PHYSICAL CHEMISTRY the tube, and the whole of the gas can be liquefied without appreciable increase of pressure. If, however, carbon dioxide above 31 is continuously compressed, no separation into two layers (liquid and gas) occurs, no matter how high the pressure applied. Similarly, if carbon dioxide is contained in a sealed tube, under such conditions that both liquid and gas are present, and the temperature is gradually raised, it will be noticed that when the temperature reaches 31 the boundary between liquid and vapour disappears, and the contents of the tube become homogeneous. Other liquids show the same remarkable phenomena, but at tem- peratures which are characteristic for each sub- stance. This temperature is known as the critical temperature; above its critical temperature no pressure, however great, will serve to liquefy a gas, below its critical temperature any gas can be liquefied by pressure. That pressure which is just sufficient to liquefy a gas at the critical tem- perature is termed the critical pressure, and the specific volume under these conditions is called the critical volume. The critical phenomena may be observed, and rough measurements of the constants obtained, with an apparatus (Fig. 3) used by Cagniard de la Tour, who discovered these phenomena in 1822. The upper part of the branch A contains a suitable volume of the liquid to be examined, the branch B, the upper pait of which is gradu- ated, contains a little air to act as a manometer, the remainder of the apparatus (the shaded part in the figure) is filled with mercury. The tube at first contains both vapour and liquid, but on gradually raising the temperature, a point is ultimately reached at which the boundary between liquid and vapour becomes faint, and finally disappears ; the tube is momentarily filled with peculiar flicker- FIG. 3. LIQUIDS ing striae, and then the contents become quite homogeneous. On allowing to cool, a mist suddenly appears in the tube at a certain temperature, and separation into liquid and vapour again occurs. The temperature at which the boundary dis- appears on heating or reappears on cooling approximates to the critical temperature, and the critical pressure can be cal- culated from the volume of air in B. Accurate measurements of the constants may be made by methods described by Young l and others. As the temperature rises, the density of the liquid in the sealed tube naturally decreases, whilst that of the vapour increases, and it has been shown that at the critical temperature the densities of liquid and vapour are equal. The critical temperatures and pressures of a few substances are given in the accompanying table : Critical Temperature, C. Critical Pressure (Atmospheres). Helium - 267-268 2-3 Hydrogen Nitrogen .* -2 3 8 -149 *5 27 Oxygen . - 119 58 Carbon dioxide 3i 72 Ethyl ether 195 35 Ethyl alcohol . 243 63 Behaviour of Gases on Compression We have already learnt that if gaseous carbon dioxide is compressed at a tem- perature below 31 it can be liquefied, but if the compression is carried out above 31 no separation into two layers occurs. These relations are best shown diagrammatically, as in Fig. 4, in which the ordinates represent the pressures and the abscissae the corresponding volumes at constant temperature. If the gas in question obeys Boyle's law, the curves obtained by plotting the pressures against the corresponding volumes at constant temperature (the so-called isothermals) are hyperbolas, corresponding with the equation/^ constant, and this condi- tion is approximately fulfilled by air, as shown in the upper right- 1 Phil. Mag., 1892, [v.], 33* J 53. 52 OUTLINES OF PHYSICAL CHEMISTRY hand corner of the diagram. An examination of the isothermals for carbon dioxide shows that the same is nearly true of this gas at 48-1, but at 35-5, and still more at 32-5, the isothermals deviate from those of an ideal gas. At the latter temperature it is very interesting to observe that the compressibility at 75 Y t Air. Carbon FIG. 4. atmospheres is very great for a short part of the curve, and beyond that point extremely small ; in the latter respect the highly compressed gas resembles a liquid. At the critical point, 31 -i, the curve is for a short distance practically hori- zontal, thus representing a great decrease of volume for a small change of pressure in other words, a high compressibility. Finally, at 21*1 and 13*1, separation of liquid takes place, the LIQUIDS 53 curves run horizontal whilst the gas is changing to liquid at constant pressure, and then the curves run almost vertical, indicating a small decrease of volume with increase of pres- sure (f.e. t a small compressibility), characteristic of liquids. It is evident from the foregoing that at any point within the dotted line ABC both vapour and liquid are present ; at any point outside only one form of matter, either vapour or liquid. The above considerations serve to show that there is no fundamental distinction between gases and liquids: a highly- compressed gas above its critical point cannot be definitely classified either as liquid or gas. It is evident from the figure that as regards compressibility, highly compressed carbon dioxide behaves more like a liquid than a gas. // is, in fact, possible to pass from the typically liquid to the gaseous form, and vice versa, without a separation into two layers. Thus liquid carbon dioxide below 31, under the conditions represented by the point x l in Fig. 5, may be compressed above its critical pressure along x- l y l and then warmed above its critical temperature whilst the pressure is kept constant at y^ During this process no separation into two layers will be noticed, and by now re- ducing the pressure the fluid can be obtained in as dilute a form as desired (what is ordinarily termed a gas), say the con- dition represented by x, whilst remaining quite homogeneous. Similarly a gas can be completely converted to a liquid without discontinuity, along xyy^x Y Application of van der Waals' Equation to Critical PhenomenaWe have already learnt that no actual gas follows the gas laws quite strictly, and, further, that the behaviour of actual gases can be represented with fair ac- curacy, even up to high pressures, by van der Waals' equation, + ^ J (V - b) = RT. If this equation is arranged in descending powers of V it becomes 54 OUTLINES OF PHYSICAL CHEMISTRY This is a cubic equation, V being treated as the variable and P and T, as well as a, b, and R, as constants. Ac- cording to the conditions the equation has either three real roots or one real and two imaginary roots. Otherwise expressed, the magnitudes of a and b may be such that at one temperature and pressure, the volume V has three real values, whilst at another temperature and pressure it may have only one real value. We will now compare these theo- retical deductions with the actual case of car- bon dioxide. It is clear from Fig. 4 that at 13*1 and 48 atmo- spheres, carbon dioxide has two volumes, as a gas (represented by the point D) and as a liquid (the point E), but the third volume demanded by the equation is not shown. At 48- 1, on the other hand, there is only one volume for each pressure, corres- ~~~ ponding with one real Volume > root of the equation under these conditions. FIG. 5. Some light is thrown on the question of the missing third real volume when the isothermal curves for carbon dioxide are plotted by substituting the values of a and b> found experi- mentally (p. 34) in equation (i). The wavy curve ABCDE shown in Fig. 5 was obtained in this way ; on comparison with the experimental curve for carbon dioxide (Fig. 4), it will be LIQUIDS 55 seen that whereas the points D and E in the latter isothermal for 13 are joined by a straight line DE, in the former the corresponding points E and A are joined by the dotted line ABCDE, which represents a change from the gaseous to the liquid form without discontinuity. The point C, at which the line of constant pressure cuts the isothermal, represents the third of the volumes required by the above cubic equation, but it probably cannot be realised in practice, as the part DCB of the curve on which it occurs represents decrease of volume with diminishing pressure, quite contrary to our usual experi- ence. On the other hand, the sections AB and ED have a real meaning. When a vapour is compressed till saturated, it does not necessarily liquefy; in the complete absence of liquid it may be compressed considerably beyond the point at which liquefaction occurs in the presence of traces of liquid; in other words, a part of the curve ED may be experimen- tally realised. Similarly, water may be heated in a carefully cleaned vessel several degrees above its boiling point, that is, it does not necessarily pass into vapour when the superincum- bent pressure is less than its vapour pressure, and a part of the curve AB may thus be experimentally realised. Similar phenomena will be met with later ; it often happens that when a system is under such conditions that the separation of another phase (form of matter) is possible, the change does not occur in the absence of the new phase. Van der Waals' equation can also be employed to obtain important relations between the critical constants and the other characteristic constants representing the behaviour of gases. It has already been pointed out that the densities and consequently the volumes of liquid and gas become equal at the critical temperature, and as this must also be true for the intermediate third volume, it follows that the three roots of the equation , T , /, RT\ _ TO a^ r ab . ^ v \ + T) v + P v " T = (l) become equal under these conditions. If, in this general 56 OUTLINES OF PHYSICAL CHEMISTRY equation, we call the three roots V lf V 2 and V 3 , then the equation ( v - v i)( v ~ V 2)( V - V 3 ) = must hold > which, when the roots are equal, becomes (V - V*) 3 - V - 3 V*V 2 + 3 V* 2 V - V* 3 = o (2), where V^ is the critical volume. Equating the coefficients of the identical equations (i) and (2), we have sV* (i) ; - 3 vi (ii) ; g - v (iii). From the last three equations, the values of the critical con- stants can readily be obtained in terms of R, a and b. We have Critical volume V* = 3^ (from ii and iii), Critical pressure P* = -=* (from ii), Critical temperature T^ = (from i). We thus reach the interesting result that the critical constants may be calculated from the deviations from the gas laws, when the latter are expressed in terms of the constants a and b of Van der Waals' equation. As an illustration of the satisfactory agreement between the observed and calculated values, we will take the data for ethylene, for which a = 0*00786, b = 0*0024, R = 0-0037. Vj, = 0*0072 (observed value 0*006), P t = -=r = ^o't; (observed value si atmospheres) 27 x (0*0024)2 8 x 0*00786 , . T fc = * = 262 Abs. (observed value 282 ). 27 x 0*0024 x 0*0037 Law of Corresponding States Van der Waals has further pointed out that if the pressure, volume and temperature of a substance are expressed as multiples of the critical values, that is, if we put P = aP*, V = /3V A , T = yT*, and then substitute in the equation (P + a/V 2 )(V - b) = RT, P, V* and T* being LIQUIDS 57 replaced by their values in terms of a, b and R, the equation simplifies to This equation does not contain the constants characteristic of any particular substance, and ought therefore to hold for all substances in the gaseous and liquid state. Experiment shows, however, that it is only to be regarded as a first ap- proximation, the deviation in many cases being much greater than the experimental error. For our present purpose, these considerations are chiefly of importance as affording information regarding the proper con- ditions for comparison of the physical properties of liquids. If we wish, for example, to compare the molecular, volumes of ether and alcohol, it would probably not be satisfactory to compare them at the ordinary temperature of a room, as this would be near the boiling-point of ether, 35, but much below that of alcohol, 78. According to van der Waals, the proper temperatures for comparison, the so-called " corresponding tem- peratures," are those which are equal fractions of the respective critical temperatures. Thus, if we choose 20, or 293 Abs., as the temperature of experiment for ether, the critical tem- perature of which is 195, or 468 Abs., the proper temperature, /, for comparison with alcohol (critical temperature, 243 C.) will be given by 27320 = 273 / , whence /= 5 i. The same considerations apply to the pressures. The theoretical basis for this method of comparison is that, as mentioned above, the choosing of pressures, volumes or tem- peratures which for different substances bear the same proportion to their respective critical constants leads, when substituted in van der Waals' equation, to an equation which is the same for all substances, and the practical justification for choosing these as corresponding conditions is that more regularities are actually 58 OUTLINES OF PHYSICAL CHEMISTRY observed by this method than when "the comparison is made under other circumstances. Liquefaction of Gases As already indicated, all gases can be liquefied by cooling them below their respective critical temperatures and applying pressure. The methods employed for this purpose by Cailletet, Pictet, Wroblewski and others are fully described in text-books of physics. In recent years the older methods have been almost completely displaced, in the case of the less condensible gases, such as air and hydro- gen, by a method introduced almost simultaneously by Linde and by Hampson. The principle of the method is that when a gas is allowed to pass from a high to a low pressure through a porous plug without performing external work it becomes cooled (Joule-Thomson effect). The cooling effect is due to the performance of internal work in overcoming the mutual attrac- tion of the particles, and is therefore only observed for " im- perfect " gases (p. 34). The effect is the greater the lower the temperature at which the expansion takes place, and the greater the difference of pressure on the two sides of the plug. The cooling effects thus obtained are summed up in a very ingenious way by the principle of " contrary currents," the same quantity of gas being made to circulate through the apparatus several times, and after passing through the plug being caused to flow over and cool the tube through which a further quantity of gas is passing on its way to the plug (or small orifice). The apparatus employed is represented diagrammatically in Fig. 6. By means of the pump A, the gas is compressed in B to (say) 100 atmospheres, the heat given out in this process being absorbed by surrounding B with a vessel through which a continuous current of cold water is passed. The cooled, com- pressed gas then passes down the central tube G, towards the plug E, being further cooled on the way by the gas passing up the wide tube D, which has just expanded through the plug. After passing through E and thus falling to its original pressure, the gas passes upwards over the central tube G and again LIQUIDS % 59 reaches A by the tube C and the left-hand valve at the bottom of A. The direction of the circulating stream of gas is indicated by the arrows. In course of time, the temperature becomes so low that part of the gas is liquefied and collects in the vessel F. More air is drawn into the appar- atus as required, and the process is continuous. By means of an apparatus con- structed on this principle Dewar, and, somewhat later, Travers, succeeded in obtaining liquid hydrogen in quantity. All known gases have now been liquefied. The liquefaction of helium was effected quite recently by Kam- merlingh Onnes. RELATION BETWEEN PHYSI- CAL PROPERTIES AND CHEMICAL CONSTITUTION General The foregoing para- graphs of this chapter represent an introduction to the relation- ship between the physical pro- perties of liquids and their chemi- cal composition, inasmuch as in- formation has been gained as to the conditions under which measurements should be made with different liquids in order to obtain comparable results (theory Lit FlG - of corresponding states). Although in this chapter we are mainly concerned with the physical properties of pure liquids, it is convenient to include also some observations with solu- 6o OUTLINES OF PHYSICAL CHEMISTRY tions. We will deal shortly with the following physical pro- perties: (i) Atomic and molecular volumes; (2) refractivity ; (3) rotation of plane of polarization of light ; (4) absorption of light; (5) viscosity. Atomic and Molecular Volumes In the case of gases, we have seen that simple relations are obtained when the volumes occupied by different substances in the ratio of their molecular weights are compared ; at the same temperature and pressure, the volumes are equal. The justification for taking the molecular weights (in grams, for instance) as comparable quantities is that, according to the molecular theory, equal numbers of molecules of different substances are thus compared. Similarly, in dealing with liquids, it is usual to determine the molecular volume of the liquid, i.e., the volume occupied by the molecular weight of the liquid in grams, which is, of course, ob- tained by dividing the molecular weight in grams by the density of the liquid at the temperature of experiment. As the specific volume, v, of a liquid is inversely as the density, the molecular volume may also be defined as molecular weight in grams x sp. volume. Similarly, the atomic volume = (atomic weight in grams) 4- density, or, (atomic weight in grams) x sp. volume. Kopp was the first chemist to carry out an extended series of observations on this subject, and he found that the most regular results were obtained when molecular volumes were determined, not at the same temperature, but at the boiling-points of the respective liquids under atmospheric pressure. It is interesting to observe that this purely empirical method of procedure was found much later to be theoretically justifiable, as the boiling- points of most liquids are approximately two-thirds of their respective critical temperatures (both measured on the absolute scale). The boiling-points are therefore corresponding tempera- tures, (p. 57). Kopp found that as a first approximation the molecular volume could be regarded as the sum of numbers representing LIQUIDS 6 1 the volumes of the component atoms. The atomic volumes of the commoner elements occurring in organic compounds are as follows : C H Cl Br I S 0(0 -H) 0(0 = ) ii 5*5 22'8 27*8 37*5 22*6 7*8 12*2 In some cases the atomic volume depends on the way in which the element is bound, thus oxygen joined to hydrogen (hydroxyl oxygen) has the atomic volume 7*8, whilst for oxygen doubly linked to carbon (carbonyl oxygen) the volume is 12*2. As an illustration the calculated and observed volumes of acetic acid may be compared as follows : 2C = 22 4 H - 22 (Carbonyl) O = 12-2 (Hydroxyl) Q = 7-8 64*0 As the molecular weight of acetic acid is 60 and its density at the boiling-point is 0-942 the observed molecular volume M/d = 637. It should be mentioned that the atomic volumes given above are not obtained directly, but by comparison of chemical compounds with definite differences of composition (e.g., the difference in the molecular volumes of the compounds C 4 H 10 and C 4 H 8 gives the volume of two atoms of hydrogen), and are therefore not necessarily the same as those for the free elements. In some cases, however, the two values coincide, thus the atomic volumes of the free halogens, chlorine and bromine, at their boil- ing-points are 23*5 and 27' i respectively, whilst their values in combination are 22-8 and 27*8, so that the halogens have ap- proximately the same volume in the free and combined condi- tion. The same is approximately true for certain other elements for which comparison is possible. The extended investigations of Thorpe, Lossen and Schiff 62 OUTLINES OF PHYSICAL CHEMISTRY afford a general -confirmation of Kopp's conclusions; the cal- culated and observed values generally agree within about 4 per cent. Although, strictly speaking, the consideration of the mole- cular volume of a substance in solution does not belong to this section, it is convenient to refer to it here. The molecular solu- tion volume ', M#, of a substance may readily be calculated from the formula Mv = j =-, where M is the molecular weight a a of the solute in grams, n the weight of the solvent containing M grams of solute, d the density of the solution, and d' that of the solvent. This formula is derived on the assumption, which is certainly not justifiable, that the density of the solvent itself is not affected by dissolving a substance in it, and therefore Mz/is only the " apparent " solution volume. The molecular volume is sometimes nearly the same in the free state and in solution 1 (e.g.) bromine in carbon tetrachloride), but is often much less (e.g., many salts in water). Additive, Constitutive and Colligative Properties The molecular volume is a good example of what is termed an additive property, since it can be represented as the sum of volumes pertaining to the component atoms. It is not, how- ever, strictly additive, since it is influenced somewhat by the arrangement of the atoms in the molecule, and therefore the atoms to some extent influence each other. Properties which depend largely on the constitution of the molecule, in other words, on the arrangement of the atoms in the molecule, are termed constitutive ; a typical constitutive property is the rota- tion of the plane of polarization of light (p. 66). The only strictly additive property is weight. Other properties, such as the refractivity, the molecular volume, heat of combustion, etc*, are more or less additive, but are to some extent complicated by constitutive influences, probably due largely to the mutual influence of the atoms. There is a third class of properties, which always retain the 1 Lumsden, Trans. Chem. Soc., 1907, 91, 24 ; Dawson, ibid., 1910, 97, 1041. LIQUIDS 63 same value independent of the number and nature of the atoms in a molecule or of their arrangement, and depend only on the number of molecules. A good illustration of these properties has already been met with in connection with gases. When these are taken in quantities which, according to the atomic theory, are proportional to their molecular weights, they all exert the same pressure when occupying equal volumes at the same tempera- ture. Such properties have been termed colligative by Ostwald. Many illustrations of these three classes of properties will be met with in the course of our work. Refractivity The velocity with which light is propagated through different substances is very ' different. The relative velocities in two media can be deduced when the change in direction of a ray of light in passing from one medium to another is known. When the ray passes from one medium to the other, the incident ray, the refracted ray (in the second medium) and the normal to the boundary between the two media (a line drawn perpen. FIG. 7. dicular to the boundary where the incident ray meets it) are in one plane. If / is the angle of incidence (the angle between the incident ray and the normal) (Fig. 7) and r is the angle of refraction (the angle between the normal and the refracted ray) and i\ and v 2 the respective velo- cities of light in the two media, it can be shown that the ratio of the sine of the angle of incidence to the sine of the angle of refraction is constant, and is equal to the ratio of the velocity of light in the two media. The ratio in question is termed the index of refraction, and is usually represented by the symbol n. We have therefore the relation n = sin r '2 64 OUTLINES OF PHYSICAL CHEMISTRY If the first medium is a vacuum, n is always greater than i in other words, light attains its greatest velocity in a vacuum, and is retarded on passing through matter. The refractive index is, however, often referred to air as unity, and to convert the values thus found to a vacuum they must be multiplied by 1-00029, giving what is termed the "absolute refractive index". An instrument employed for the determination of refractive indices is termed a re fracto meter. Among the more convenient forms of refractometer, those due to Abbe* and to Pulfrich may be specially mentioned. Ordinary white light cannot be employed for refractivity measurements, as the component rays are refracted or retarded to a different extent on passing through matter, the rays thus scattered or dispersed giving rise to a spectrum. This difficulty is "avoided by using light of the same wave-length (so-called monochromatic light), and for this purpose .sodium light, the wave-length of which is represented by the letter D, is con- venient. Measurements of the refractive index referred to sodium light are represented by the symbol D . The refractive index of a given substance, like any other property, depends on the conditions of temperature, pressure, etc., under which the measurements are made. It has been found convenient to express the results of measurements not simply in terms of D , but in terms of the function - where d is the density of the liquid or gas (Gladstone and Dale, 1858). This purely empirical function, known as the refraction constant, 1 is, for any given substance, practically inde- pendent of the temperature. In 1880, Lorenz and Lorentz arrived simultaneously, from theoretical considerations, at the n 2 - i i somewhat more complicated expression, 2 . j, and showed that, for the same substance, it remained fairly constant, not only for widely differing temperatures, but even for the change from liquid to gaseous form. Thus Eykman found that the 1 The expression here called the " refraction constant " is sometimes called the " specific refractivity". LIQUIDS 65 value of this function for isosafrol, C 10 H 10 O 2 , amounted to 0-2925 and 0-3962 at 17-6 and 141 respectively, and Lorenz obtained for water at 10 and water vapour at 100 the values 0*2068 and 0*2061 respectively. For comparative purposes, it is usual to employ the atomic refraction (atomic weight x refraction constant) and the mole- cular refraction (molecular weight x refraction constant) ; the latter, if we employ the second form of the refraction constant, is given by -5 * -7, where M is the molecular weight. In this case also it has been found, from measurements on many organic liquids, that the molecular refraction may be represented to a first approximation as the sum of the refrac- tions of the component atoms, so that the refractive power is largely an additive property. Just as in the case of molecular volumes, however, there are certain deviations from this additive behaviour (constitutive influences) which may be connected with the arrangement of the atoms in the molecule. Briihl, 1 who has been particularly prominent in investigating this question, points out that the molecular refraction of compounds containing double and triple bonds is greater than the calculated value, and he takes account of this constitutive influence by ascribing definite refractivities to these bonds. The most recent values for a few of the elements are as follows : Oxygen Double Triple C H (in CO group) (in ethers) (in OH group) Cl I bond bond 2-418 i-ioo 2-2ii 1-643 1-525 5-967 13-90 1733 2-398 Later investigations show that neighbouring double or triple bonds exert a mutual influence, so that the matter becomes somewhat complicated. Conversely, it is sometimes possible, from measurements of the refractive index (or other physical property), to draw con- clusions as to the constitution of chemical compounds, but as 1 For a short summary of Bruhl's work, by himself, see Proc. Royal Institution, 1906, 18, 122. 2 The numbers are referred to the D line (sodium light) and are calcu- lated according to the Lorentz formula. 5 66 OUTLINES OF PHYSICAL CHEMISTRY our knowledge of the relations between physical properties and chemical constitution is very imperfect, this method should only be employed with great caution. It is evident that no conclu- sions as to chemical constitution can be drawn from additive properties, but only from constitutive properties. Rotation of Plane of Polarization of Light The pro- perties of liquids so far dealt with have been mainly additive, the magnitude of properties such as volume, effect on the speed of light, etc., being much the same in the free state and in combination. We have now to deal with the property pos- sessed by a few liquids (and dissolved substances) of rotating the plane of polarized light a property which depends entirely upon the arrangement of the atoms in the molecule. Isomeric substances have in general nearly equal molecular refractivity and molecular volume, but it often happens that of two isomeric substances, such as the two lactic acids, one rotates the plane of polarized light and the other does not. Plane polarized light (light in which the vibrations are all in one plane) is obtained by passing monochromatic light through a polarizing prism (Nicol prism or tourmaline plate) which cuts off all the rays except those vibrating in one plane. A prism of this type is mounted at some distance from another similar prism in such a way that light which has been polarized in the first prism may be examined after it has passed through the second prism, which is termed the analyser. If now the analyser is rotated until it is perpendicular to the polarizer, all ; the light which passes through the former will be cut off by the analyser, and on looking through the eyepiece the field will appear dark. If now, while the prisms are in this relative posi- tion, a tube filled with turpentine is placed between them, the field again appears clear, but becomes dark on rotating the analyser through a certain angle. This observation is readily accounted for on the view that the plane of polarization is twisted through a certain angle whilst the light is traversing the turpentine, and the analyser must therefore be rotated in ordej LIQUIDS 67 to bring it into the former relative position with regard to the polarized ray. The angle through which the analyser has been turned is read off on a graduated scale. The instrument used for measuring the rotation of liquids, which consists essentially of the two prisms and graduated scale, as described above, is termed a polarimeter. The observed angle of rotation depends on the nature of the liquid, on the wave-length of the light employed in the measurements, and on the temperature, and is proportional to the length of liquid traversed. For purposes of comparison, the results are usually expressed in terms of the specific rotation [a] for a fixed temperature / and a particular wave-length of light (for example, sodium light) by means of the formula where a is the observed angle, / is the length of the column of liquid in decimetres, and d is the density of the liquid at the temperature /. The molecular rotation m[a] is obtained by multiplying the specific rotation by the molecular weight of the liquid. The specific rotation of substances in solution is represented by the analogous formula r ,* iooa [0] D = W where g is the number of grams of solute in 100 grams of the solution, d is the density of the solution at the temperature /, and a and / have the same significance as before. The liquids and dissolved substances which possess this re- markable property are almost exclusively compounds containing carbon. Further, only compounds containing an asymmetric carbon atom, that is, a carbon atom joined to four different groups, have the power of rotating polarized light ( van't Hoff and Le Bel, 1874). For example, the graphic formula of ordinary lactic acid, which is optically active, may be written as follows : 68 OUTLINES OF PHYSICAL CHEMISTRY CH 8 : OH H-i COOH showing that no two of the groups attached to the central carbon atom are identical. A further 'remarkable fact is that when one form of a substance, such as lactic acid, can rotate the plane of polarized light to the right, a second modifica- tion can always be obtained which, although identical with the first in all other physical properties, rotates polarized light to the left to the same extent as the first modification rotates it to the right. The first is termed the dextro or d modi- fication, the second the laevo or / modification. Van't Hoff and Le Bel account for this on the hypothesis that the four different groups are not in the same plane as the carbon atom, but are arranged in the form of a tetrahedron with the carbon atom in the centre. It can be shown, most readily by means of a model, 1 that when all 4 four groups are different there are two arrangements which cannot be made to coincide by rotating one of the models. These two arrangements behave to each other as object and mirror image, or a right- and left-hand glove, which cannot be brought into the same relative position, and, according to the theory, correspond with the dextro and laevo modifications respectively. If any two of the groups become identical, however, the two arrangements can always be brought ;:o coincidence, and there is no possibility of optical isomerism. In calculating the specific rotation of a dissolved substance, it is implicitly assumed that it is not affected by an indifferent solvent. As a matter of fact, however, the molecular rotation of a dissolved substance often differs considerably from its value 1 Models for this purpose can be bought for a few pence, or can be made by the student with a piece of cork and four pins provided with differently coloured balls at the ends. LIQUIDS 69 in the pure state. This is well shown by the following results obtained by Patterson 1 for /-menthyl-^-tartrate in the pure state, and in 1-2 per cent, solution. Molecular Rotation of /-menthyW-tartrate. Solvent. Molecular Rotation at 20. None - 284 Ethyl alcohol -306-2 Benzene - 296-1 Nitrobenzene - 245-3 So far, no definite connection has been found between any other property of the solvent and its effect on the rotation of a solute. Almost the only regularity which has yet been dis- covered in this branch of the subject is that the rotatory power of the salt of an optically active acid (or base) in dilute solution is independent of the nature of the base (or acid) with which it is combined. This important result is further referred to at a later stage. , All transparent substances, when placed in a magnetic field, rotate the plane of polarized light, and the late Sir William Perkin, who devoted many years to the systematic investigation of this subject, showed that this magnetic rotation is, like refrac- tivity, largely an additive property. Absorption of Light 2 When a ray of white light passes through matter a greater or less amount of absorption invari- ably occurs, and the spectrum of the issuing ray shows dark bands corresponding with the rays which have been absorbed. This spectrum is termed an absorption spectrum. Absorption may be general or selective. In the former case there is a general weakening throughout whole regions of the spectrum ; in the latter case, there are independent relatively narrow bands in different regions of the spectrum. ^ee Trans. Chem. Soc., 1905, 87, 128. 2 Smiles, Chemical Constitution and some Physical Properties (Long- mans, 1910), pp. 324-423. 70 OUTLINES OF PHYSICAL CHEMISTRY The absorption spectrum is one of the most characteristic properties of a given substance or class of substances under definite conditions. Thus, for instance, the absorption spectra of permanganates in dilute solution are characterised by the presence of five dark bands in the green. In the case of liquids or solutions, absorption is most conveniently measured in the transmitted light, as already indicated. In the case of solids, however, observations may be made with reflected light, as part at least of the reflection takes place from layers a little below the surface, and the short distance traversed is usually sufficient to produce some absorption. The method which is most largely employed in the case of liquids is to use as a source of illumination the electric arc or spark passing between metallic (preferably iron) poles, the spectrum of the light being photographed after the latter has passed through the liquid. Substances which have high ab- sorbing power are usually examined in solution, and the solvent chosen should not itself show absorption in the part of the spectrum studied. Ethyl alcohol is most largely used as solvent. A very important question in such measurements is the effect of dilution on the persistence and intensity of a band it very often happens that a band appears only within certain limits of dilution. For this reason, it is usual to carry out measurements with varying thicknesses of the absorbing layer and with varying concentrations. The solutions are made more and more dilute till absorption is no longer observed. For purposes of comparison, the solutions to be examined are usually made up to contain simple fractions of a mol per litre. The method usually employed in representing the results graphically requires some explanation. It is illustrated in Fig. 8, which shows the absorption in the ultra-violet region of a solution of the amino derivative of dimethyldihydroresorcin in ethyl alcohol. The diagram shows the presence of one band. The principle of the method is that the oscillation frequencies of the limits of the absorption band are plotted LIQUIDS 71 against the logarithms of the relative thicknesses referred to the thinnest layer of the most dilute solution examined. It is more convenient to use Oscillation Frequencies. FIG. 8. 2000 1,500 1000 . c 500 -| X 250 g 200 o the logarithms of the relative thicknesses than the thicknesses them- selves as ordinates. The latter are shown on the right-hand side of the figure, and it is evident that if equal increments of thickness were used, the curve would become inconveniently long. The space above the curve shows the wave lengths of the light, absorbed at different dilutions, and the curve itself represents the limits of the absorption. The lowest part of the curve, usually termed the " head," is that point at which the strongest ab- sorption takes place ; in the diagram it occurs at an oscillation frequency of 3600 units. The so- called " persistence " of the band is the difference of the logarithms of the thicknesses at which the band makes its appearance and dis- appears respectively, and is indicated on the diagram by its depth (in the present case extending from i to 23 units). 34 32 I 30 I '28 I 26 24 *22 > ; a liquid of small viscosity, such as ether, is said to have a high degree of fluidity. The magnitude of the viscosity depends greatly on the nature of the liquid. Thus the viscosity of warm ether is very small, whereas that of treacle and of pitch is so great that they approximate to the behaviour of solids, the internal friction of which is extremely high. The internal friction of gases is very small (p. 25). The coefficient of viscosity, rj, is usually defined as the force required to move a layer of unit area in unit time through a distance of unit length past an adjacent layer unit distance away. For water at 15, rj = o - oi34 in absolute units; for glycerine at the same temperature, rj = 2-34. The coefficient of viscosity of a liquid can be calculated from the rate of outflow from a cylindrical tube by means of the equation where v is the volume of liquid discharged in the time /, p the pressure under which the outflow takes place, r the radius and / the length of the tube. In practice, however, the rate of flow of the liquid is compared with that of a standard liquid, usually water, under the same experimental conditions, and its absolute viscosity, 17, calculated by means of the formula "nho = */** where r}^ is the absolute viscosity of water at the temperature of the experiment, and t and / w are the times required for the discharge of equal volumes of the liquid and water respectively. The viscosity of liquids diminishes rapidly as the temperature LIQUIDS 75 O rises, but so far no simple relationship of general applicability connecting change of viscosity and temperature has been dis- covered. Measurement of Yiscosity The determination of vis- cosity by the comparative method may be conveniently carried out with the apparatus described by Ostwald and illustrated in Fig. 9. It consists essenti- ally of a capillary tube, db, connected at its upper part with a bulb /, and at its lower end with a wider tube, bent into U- shape and provided with a bulb at 25. Acetone 0-00397 0-00316 Methyl alcohol 0*00846 0-00580 Acetic anhydride O'OI3O O'oo86o Water 0-0178 0-00891 Ethyl alcohol O-OI79 o-o 108 Benzonitrile 0*0194 0-0125 Nitrobenzene 0-0307 0-0182 In recent years the viscosity of mixtures of liquids has been the subject of a good deal of investigation. If for simplicity we confine our attention to mixtures of two components only, three classes may be distinguished : (1) The viscosity of the mixture lies between those of the pure components. Example, ethyl alcohol and carbon disul- phide. (2) The viscosity of the mixture in certain proportions is greater than that of either component. Example, pyridine and water. (3) The viscosity of the mixture in certain proportions is less than that of either constituent. Example, benzene and acetic acid. A few numbers illustrating the behaviour of the mixtures LIQUIDS 77 cited as examples of classes (2) and (3) are given in the accompanying table. Pyridine and Water.l Benzene and Acetic Acid.* Per cent. Pyridine. T? at 25. Per cent. Benzene. , at 25. 0'00 0-00890 o-oo 0-01174 IQ'28 0-01336 34'93 0*00734 39-84 0-01833 48-29 0-00666 59'7 0*02187 77-26 0-00597 66-6 5 O-O2225 8973 0-00591 80-15 0-01894 97-25 0-00594 lOO'OO 0-00885 IOO-00 0-00598 The results are very similar to those for the vapour pressures of binary mixtures, described later (p. 87). No general agreement has so far been reached as to the explanation of these remarkable differences in the behaviour of binary mixtures (compare p. 322). Measurements of the viscosity of salt solutions (solutions which conduct the electric current) have also led to interesting results, but they cannot be usefully considered at the present stage. Practical Illustrations, (a) Critical Phenomena The critical phenomena can be observed in an apparatus, con- structed like that of Cagniard la Tour, but more simply as fol- lows : A tube 3-4 mm. internal diameter and 3-4 cm. long is constructed out of a piece of glass tubing, the walls of which are 0*7-0-8 mm. thick, by closing one end in the blow-pipe and drawing out the other at a distance 3-4 cm. from the closed end into a fairly long (5-6 cm.) thick-walled capillary tube. The capillary is then bent, at a point about i cm. from the commence- ment of the wide part of the tube, at right angles to the latter and then partly filled with ether as follows. The tube is warmed and the capillary end dipped into ether, which is drawn into the tube 1 Hartley, Thomas and Appleby, Trans. Chem. Soc., 1908, 94, 538. 2 Dunstan, ibid., 1905, 87, 16. 78 OUTLINES OF PHYSICAL CHEMISTRY as the latter cools. The ether in the tube is then boiled gently to expel all the air, the end of the capillary dipping all the time in ether, and on again allowing to cool, ether is drawn in so as practically to fill the tube. The excess of ether is then boiled off till the tube is about three-quarters full, the end of the capillary being in ether throughout, and then allowed to cool till the liquid just begins to rise up the capillary tube, showing that the pressure inside is somewhat less than atmospheric ; the capillary is then rapidly sealed off near the bend on the side remote from the tube. In order to observe the capillary phenomena in the tube thus prepared, the latter is suspended by a wire and heated by means of a Bunsen burner held in one hand, the face being protected, in the event of an explosion, by a large plate of glass held in the other hand. In this way, the complete dis- appearance of the liquid above a certain temperature, and its reappearance on cooling, may be observed without the least danger. When practicable, the tube may be heated in an iron or copper vessel provided with mica windows, and the critical temperature may be read off on a thermometer placed side by side with the tube in the air bath. () Determination of Molecular Volume The determination of the molecular volume of a liquid reduces to a determination of its density at a definite temperature compared with that of water as unity, and any of the well-known methods for deter- mining the density of liquids may be employed for this purpose. A direct method for determining the density, and hence the mole- cular volume, of a liquid at its boiling-point has been described by Ramsay. A tube is drawn out to a long neck and the latter bent in the form of a hook. The vessel is then filled with liquid, heated in the vapour of the same liquid till equilibrium is reached and then weighed. If the volume of the vessel and its coefficient of expansion are known, the molecular volume of the liquid can at once be calculated. LIQUIDS 79 Measurements of the refractive index of liquids (water alcohol, benzene) and of the rotation of the plane of polarization of light by liquids or solutions (cane sugar in water) should be made by the student ; the methods are fully described in text- books of physics. The experiments on rotation of the plane of polarization may conveniently be made in connection with the hydrolysis of cane sugar in the presence of acids (p. 230). CHAPTER IV SOLUTIONS General Up to the present, we have dealt only with the properties of pure substances which may exist in the gaseous, liquid or solid state, or simultaneously in two or all of these states. We now proceed to deal with the properties of mixtures of two or more pure substances. When these mixtures are homogeneous, they are termed solutions. 1 There are various classes of solutions, depending on the state of the components, The more important are : (i) Solutions of gases in gases ; (ii) Solutions of (a) gases, (b) liquids, (c) solids in liquids ; (iii) Solutions of solids in solids, so-called solid solutions ; and each of these classes will be briefly considered. A distinction is often drawn between solvent and dissolved substance, but, as will appear particularly from the sections dealing with the mutual solubility of liquids, there is no sharp distinction between the two terms. The component which is present in greater proportion is usually termed the solvent. The dissolved substance is sometimes called the solute. When one of the compounds is present in very small pro- portion, the system is termed a dilute solution, and as the laws a The term solution is also applied to mixtures which appear homo- geneous to the naked eye but heterogeneous when examined with a micro- scope or ultramicroscope, e.g., colloidal solution of arsenic sulphide. The usual definition of a solution is "a homogeneous mixture which cannot be separated into its components by mechanical means," but the last part of this definition is open to objection. 80 SOLUTIONS 81 representing the behaviour of dilute solutions are comparatively simple, they will be dealt with separately in the next chapter. Solution of Gases in Gases This class of solution differs from the others in that the components may be present in any proportion, since gases are completely miscible. If no chemical change takes place on mixing two gases, they behave quite in- dependently and the properties of the mixture are therefore the sum of the properties of the constituents. In particular, the total pressure of a mixture of gases is the sum of the pressures which would be exerted by each of the components if it alone occupied the total volume a law which was discovered by Dalton, and is known as Dalton s law of partial pressures. Dalton's kw is of the same order of validity as Avogadro's hy- pothesis ; it is nearly true under ordinary conditions, and would in v all probability become strictly true at great dilution. Dalton's law can of course be tested by comparing the sum of the pressures exerted separately by two gases with that after admixture, but it is of interest to inquire into the possibility of measuring the partial pressure of one of the components in the mixture itself. It was pointed out by van't Hoff that this is always possible if a membrane can be obtained which allows only one of the gases to pass through. This suggestion was experimentally realised by Ram- say * in the case of a mixture of nitrogen and hydrogen as follows: P (Fig. 10.) is a palladium vessel containing nitrogen, the pressure of which can be determined from the difference of level between A and B in the manometer, which contains mercury. P is enclosed in another vessel, which can be filled H FIG. 10. Phil. Mag., 1894, [v.], 38, 206. 82 OUTLINES OF PHYSICAL CHEMISTRY with hydrogen at any desired pressure. The vessel P is heated and a stream of hydrogen at known pressure passed through the outer vessel. As palladium at high temperatures is permeable for hydrogen, but not for nitrogen, the former gas enters P till its pressure outside and inside are equal. The total pressure in P, as measured on the manometer, is greater than the pressure in the outer vessel, and it is an experimental fact that the excess pressure inside is approximately equal to the partial pressure of the nitrogen. If, on the other hand, we start with a mixture of hydrogen and nitrogen, and wish to find the partial pressure of the latter, all that is necessary is to put the mixture inside a palladium bulb, keep the latter at a constant high temperature and pass a current of hydrogen at known pressure through the outer vessel till equi- librium is attained, as shown on the manometer. The difference between the external and internal pressure is then the partial pressure of the nitrogen. This very instructive experiment will be referred to later in connection with the modern theory of solutions (p. 101). Solubility of Gases in Liquids In contrast to the com- plete miscibility of gases, liquids are only capable of dissolving gases to a limited extent. When a liquid will not take up any more of a gas at constant temperature it is said to be saturated with the gas, and the resulting solution is termed a saturated solution. The amount of a gas taken up by a definite volume of liquid depends on (a) the pressure of the gas, (b) the tem- perature, (c) the nature of the gas, (d) the nature of the liquid. The greater the pressure of a gas, the greater is the quantity of it taken up by the solvent. For gases which are not very soluble, and do not enter into chemical combination with the solvent, the relation between pressure and solubility is expressed by Henry's law as follows : The quantity of gas taken up by a given volume of solvent is proportional to the pressure of the gas. Another way of stating Henry's law is that the volume of a gas taken up by a given volume of solvent is independent of the SOLUTIONS 83 pressure. This is clearly equivalent to the first statement, be- cause when the pressure is doubled the quantity of gas absorbed is doubled, but since its volume, by Boyle's law, is halved, the original and final volumes dissolved are equal. The question may be regarded from a slightly different point of view, which is instructive in connection with later work. When a definite volume of liquid is saturated with a gas at a certain pressure, there is an equilibrium between the dissolved gas and that over the liquid, and Henry's law may be expressed in the alternative form : The concentration of the dissolved gas is proportional to that in the free space above the liquid. We may consider that the gas distributes itself between the solvent and the free space in a ratio which is independent of the pressure. The solubility of gases in liquids diminishes fairly rapidly with rise of temperature. For purposes of comparison, the solvent power of a liquid for a gas is best expressed in terms of the " coefficient of solubility," which is the volume of the gas taken up by unit volume of the liquid at a definite temperature. 1 The so-called "absorption coefficient " of Bunsen, in which solubility measurements are still often expressed, is the volume of a gas, reduced to o and 76 cm. pressure, which is taken up by unit volume of a liquid at a definite temperature under a gas pressure equal to 76 cm. of mercury. With regard to the influence of the nature of the gas on the solubility, it may be said in general that gases which have distinct basic or acidic properties, for example, ammonia and hydrogen chloride, are very soluble, whilst neutral gases, such as hydrogen, oxygen and nitrogen, are comparatively insoluble. Further, gases which are easily liquefied, for example, sulphur dioxide and hydrogen sulphide, are fairly soluble. As regards the relation between solvent power and the nature of the liquid, very little is known. In general, the order of the solubility of gases in different liquids is the same, and the solvent power of a liquid therefore appears to be to some extent a specific property. 1 Alternatively : the ratio of the concentration in liquid and in gas space. OUTLINES OF PHYSICAL CHEMISTRY The above remarks are illustrated by the following table, in which the coefficients of solubility of some typical gases in water and in alcohol are given : Gas. Water. Alcohol. Ammonia 1050 _ Hydrogen sulphide Carbon dioxide 80 1-8 18 4'3 Oxygen . 0-04 0-28 Hydrogen O'O2 0-07 It may be mentioned that the solubility of gases in water is greatly diminished by the addition of salts, and to a much smaller extent by non-electrolytes. The interpretation of these results has given rise to considerable difference of opinion. 1 Solubility of Liquids in Liquids As regards the mutual solubility of liquids, three cases may be distinguished : (i) The liquids mix in all proportions, e.g., alcohol and water ; (2) the liquids are practically immiscible, e.g., benzene and water ; (3) the liquids are partially miscible, e.g., ether and water. (i) and (2) Complete miscibility and non-miscibility Very little is known as to the factors which determine the miscibility or non-miscibility of liquids. The separation of the compon- ents by fractional distillation is discussed in succeeding sections. (3) Partial miscibility If ether, in gradually increasing amounts, is added to water in a separating-funnel, and the mix- ture well shaken after each addition, it will be noticed that at first a homogeneous solution is formed, but when sufficient ether has been added, a separation into two layers takes place on standing. The upper layer is a saturated solution of water in ether, the lower layer a saturated solution of ether in water. As long as the relative quantities of ether and water are such that a separation into two layers takes place on standing, the Compare Philip, Trans. Chem. Sec., 1907, 91, 711; Usher, ibid., 1910, 97, 66. SOLUTIONS 85 composition of these layers is independent of the relative amounts of the components present^ since the composition is determined by the solubility of ether in water and of water in ether at the temperature of experiment. Further, the saturated vapours sent out by the two layers have the same pressure and the same com- position this follows from the fact that they are in equilibrium with the two layers which are in equilibrium with each other. In the majority of cases, the solubility of two partially miscible liquids increases with the temperature, and it may therefore be anticipated that liquids which in certain propor- tions form two layers at the ordinary temperature may be com- pletely miscible at higher temperatures. Several such cases are known, for example, phenol and water, which has been investigated by Alexieeff. At room temperature a saturated solution of phenol in water contains about 8 per cent, of the former component. When more phenol is added two layers are formed and the temperature has to be raised in order to secure complete miscibility. For further additions of phenol up to 36 per cent, the temperature at which complete miscibility occurs rises progressively to 68 '4. In this way the solubility- temperature curve of phenol in water is obtained. Similarly, a saturated solution of water in phenol at 20 contains 28 per cent, of the former component and on further additions of water the temperature of complete miscibility rises progres- sively to 68-4, at which point the two solubility-temperature curves meet. These results are represented graphically in Fig. 1 1, the composition of the mixture being measured on the horizontal axis and temperatures along the vertical axis. The point D represents o per cent, phenol (100 per cent, water), E represents 100 per cent, phenol. At all points outside the curve ABC there is complete miscibility, at points inside the curve two layers exist. The maximum represents the tem- perature, 68*4, above which phenol and water are miscible in all proportions. If, therefore, we start with a homogeneous solution of phenol in water of the composition represented 86 OUTLINES OF PHYSICAL CHEMISTRY by the point x, and gradually add phenol at constant tem- perature, the composition of the. .solution will alter along the dotted line xx until the curve AB is reached at z. This point represents a saturated solution of phenol in water, and on further addition of phenol a separation into two layers takes place, the compositions of which are represented by the points s and z' respectively. As more phenol is added, the composition of the layers remains unaltered, but the relative amount of the second layer increases until at the point z' only this layer is present, and its composition then alters along zx'. 60" A o/ Phenol Miscibility of Phenol and Water. FlG. II. 100 / Phenol o% 100% NICOTINE NICOTINE Miscibility of Nicotine and Water. FlG. 12. If, however, phenol is added to the same solution at the tem- perature corresponding with the point y the composition alters along yy but no separation into two layers takes place. It is evident that there is a striking analogy between the miscibility of two liquids and the critical phenomena represented in Fig. 5. In both cases there is only one phase outside the curves AOE and ABC respectively, and two phases at points inside the curves. Further, above a certain temperature only one phase can exist in each case, and the temperature of com- plete miscibility for binary mixtures may therefore be termed the critical solution temperature. Moreover, just as we can SOLUTIONS 87 pass without discontinuity from a gas to a liquid (p. 53), we can pass from a solution containing excess of water to one contain- ing excess of phenol without discontinuity. Starting with a mixture represented by the point x, the temperature is raised above the critical solution temperature along xy, phenol is then added till the point y' is reached and the homogeneous mixture then cooled along yx. In some cases, however, the solubility of one liquid in another diminishes with rise of temperature, thus if a saturated solution of ether in water, prepared at the ordinary temperature, is gently warmed, it becomes turbid, indicating partial separation of the ether. An interesting example of this behaviour is seen in nicotine and water, which are miscible in all proportions at the ordinary temperature, but separate into two layers when the temperature reaches 60. If a temperature can be reached beyond which the mutual solubility again begins to increase with rise of temperature, the components may again become miscible in all proportions. This has been experimentally realised so far only for nicotine and water, which again be- come completely miscible when the temperature exceeds 210. The remarkable solubility relations of these two liquids are therefore represented by a closed curve (Fig. 12), which will be readily understood by comparison with Fig. n. Distillation of Homogeneous Mixtures A very impor- tant matter with reference to binary homogeneous mixtures is the possibility of separating them more or less completely into their components by distillation. Much light is thrown on this question by the investigation of the vapour-pressure of the mix- ture as a function of its composition at constant temperature. Experimental investigation shows that the curve representing the relation between vapour pressure and composition at constant temperature usually belongs to one of the three main types a, b and c represented in Fig. 13, in which the abscissae represent the composition of the mixture and the ordinates the corres- ponding vapour pressures. 88 OUTLINES OF PHYSICAL CHEMISTRY (a) The vapour-pressure curve of the mixture may have a minimum, as represented by the point U in the curve RUS ; example, hydrochloric acid and water. (In the diagram the ordinate PR represents the vapour-pressure of B, and QS that of the other pure substance A.) () The vapour-pressure curve may show a maximum, repre- sented by the point T on the curve RTS ; example, propyl alcohol and water. P(o/ A) Composition FIG. 13. Q (TOO o/ A) (f) The vapour-pressure of the binary mixture may lie between those of the pure components A and B, as repre- sented by the curve RWS ; example, methyl alcohol and water. In considering these three typical cases with regard to their bearing on the separation of two liquids by fractional distilla- tion, the important question is the relation between the com- position of the boiling liquid and that of the escaping vapour. For a pure liquid, the composition of the escaping vapour is necessarily the came as that of the liquid, but this is not in general the case for a mixture of liquids, and therefore the SOLUTIONS 89 composition of the mixture may alter continuously during dis- tillation. Case (a). Since a liquid boils when its vapour pressure is equal to the external pressure, it is clear that if a mixture the vapour-pressure curve of which has a minimum (as in the curve RUS) be boiled, the composition of the liquid will alter in such a way that it tends to approximate to that represented by the point U, since all other mixtures have a higher vapour pressure, and will consequently pass off first. When finally only the mixture U remains, it will distil at constant tempera- ture like a homogeneous liquid, since the composition of the vapour is then the same as that of the liquid. The best- known example of such a constant-boiling liquid is a mixture of hydrochloric acid and water, which boils at no . If a mixture containing the components in any other proportion be heated, either hydrochloric acid or water will pass off, and the com- position of the liquid will move along the curve to the point of minimum vapour pressure, beyond which it distils as a whole, without further change of composition. Case (b). When, on the other hand, there is a maximum in the vapour-pressure curve, the mixture which has the highest vapour tension will pass over first, and the composition of the residue in the retort will tend towards the component which was present in excess in the initial mixture. In the case of propyl alcohol and water, for example, the mixture which has the highest vapour tension contains from 70 to 80 per cent, alcohol (the maximum being very flat) ; a mixture of this com- position would boil at constant temperature, whilst for one con- taining more water, some of the latter would finally remain in the retort. Case (c). In this case the composition of the vapour, and therefore the composition of the liquid remaining, alter continu- ously on distillation. The vapour, and therefore the distillate, will contain the more volatile liquid, A, in greater proportion, and the residue excess of the less volatile liquid, a partial separation OUTLINES OF PHYSICAL CHEMISTRY being thus effected. If the distillate rich in A is again distilled a mixture still richer in A is at first given off, and the process may be repeated again and again. The more or less complete separation of liquids by this method is termed fractional dis- tillation. It was long thought that constant-boiling mixtures were definite chemical compounds of the two components for example, HC1, 8H 2 O in the case of hydrochloric acid and water, but this view was shown by Roscoe to be untenable. He found that the composition of the mixtures does not correspond with simple molecular proportions of the com- ponents, and, further, that the composition alters con- tinuously with alteration of the pressure under which the distillation is conducted, which is not likely to be the case if definite chemical compounds are present. Distillation of Ncn-Miscible or Partially Miscible Liquids. Steam Distillation If two immiscible liquids are distilled from the same vessel, since one does not affect the vapour pressure of the other, they will pass over in the ratio of the vapour pressures till one of them is used up. The tem- perature at which the mixture boils is that at which the sum of the vapour pressures is equal p(o/ B) Composition FlO. 14. Q zoo / B) to the superincumbent pressure. The curve re- presenting the relation between vapour pressure and composition of the mixture is therefore a straight line (UU', Fig. 14) parallel to the axis of composition, PU representing the sum of the vapour pressures SOLUTIONS 91 RP and QT, of the two components at the temperature in question. These considerations are very important in connection with steam- distillation. This process is usually employed for the separation of substances with a high boiling-point, such as aniline, and will be familiar to the student. The relative volumes of steam and the vapour of the liquid which pass over are in the ratio of the vapour pressures, p^ and / 2 , at the tem- perature of the experiment, and the relative weights which pass over are therefore in the ratio p^ : / 2 a value which almost exactly corresponds with that obtained for gases. As the same value for r is obtained for a mol of other organic compounds, such as urea and glucose, we will represent it by R, to indicate that it is a factor of general im- portance. We have thus obtained two results of the greatest importance : (i) the equation PV = RT is valid for dilute solu- DILUTE SOLUTIONS 103 tions ; (2) the numerical value of R is the same for dissolved substances as for gases. The latter statement implies, as is clear from the general equation, that the osmotic pressure of a definite quantity of cane sugar or other substance in solution is equal to the gas pressure which it would exert if it occupied the same volume in the gaseous form. We may therefore say with van't Hoff that " the osmotic pressure exerted by any substance in solution is the same as it would exert if present as gas in the same volume as that occupied by the solution, provided that the solution is so dilute that the volume occupied by the solute is negligible in comparison with that occupied by the solvent", This statement holds for all temperatures, as is at once clear from the fact that the solution obeys the gas laws. Certain important exceptions to the above rule, more particularly in the case of solutions which conduct the electric current, will be discussed in a later chapter. Some important consequences of the validity of the general equation, PV = RT, for dissolved substances will be dealt with in detail later. In particular, the molecular weight of a dis- solved substance is the quantity in grams which, when dissolved in 2 2 '4 litres at o, exerts an osmotic pressure of i atmosphere, a definition almost exactly analogous to that for gases (p. 36). The same fact may be expressed somewhat differently as fol- lows : Quantities of different substances in the ratio of their molecular weights, when dissolved in equal volumes of the same solvent, exert the same osmotic pressure. So far, we have considered only the experimental basis of the theory of solution. It has, however, been shown theoretically by van't Hoff, by thermodynamical reasoning, that the osmotic pressure and gas pressure must have the same absolute value, if the solution is sufficiently dilute, and this conclusion has been confirmed by Lord Rayleigh and by Larmor, among others. The latter writer puts the matter as follows : " The change of available energy on further dilution, with which alone we are concerned in the transformations of dilute solu- ^YSICAL CHEMISTRY tions [(/". p. 150], depends only on the further separation of the particles ... and so is a function only of the number of dissolved molecules per unit volume and of the temperature, and is, per molecule, entirely independent of their constitution and that of the medium," 1 the assumption being made that the particles are so far apart that their mutual influence is negligible. " The change of available energy " is thus brought into exact correlation with that which occurs in the expansion of a gas. Recent direct Measurements of Osmotic Pressure It is a remarkable fact that, although Pfeffer's osmotic pres- sure measurements were made as early as 1877, the degree of accuracy attained by him has not been improved upon until quite recently. Accurate measurements are, however, very desirable, because although the relation between osmotic pres- sure and concentration can be calculated from the gas laws in dilute solution, there is still much uncertainty as to how far the gas laws are applicable, or what is the exact relationship between osmotic pressure and concentration, in concentrated solutions. In particular, it is, or was until quite recently, uncertain whether V in the general equation, PV = RT, should represent the volume of the solvent or that of the solution. This uncertainty has been to some extent removed by the very careful measurements carried out by Morse and Frazer 2 since 1903 by Pfeffer's method with slight modifications. Their results show that, if V in the general equation be taken as the volume of the solvent, aqueous solutions of cane sugar approximately follow the gas laws up to a concentration of 342 grams of the solute in 1000 grams of water. A few of their results, illustrating the above statement, are given in the accompanying table; the numbers under "gaseous" are calculated on the assumption that the sub- stance as gas occupies the same volume as the solvent in the solution. 1 Larmor, Encyc. Britannica, loth ed., vol. xxviii., p. 170. *Amer. Chem. J., 1905,34, i; 1906, 36, i, 39; 1007, 37, 324, 425, 558; 38, 175; 1908, 39, 667; 40, i, 194; 1909, 4*1 * 2571 *9"i 4S 554. etc. DILUTE SOLUTIONS 105 Concentration of Solution. Pressure at constant temp. Ratio of A (20) (atmospheres). osn lotic pres- re to gas ressure. Mols per 1000 grams of water. Mols per litreU! solution. Gaseous. Osmotic. p O'lO 0-09794 2'39 2-522 055 0*20 OT9I92 4-78 5^23 051 0-40 0-36886 9-56 9-96 038 o - 6o 0-532S2 J 4'34 15-20 060 0-80 0-68428 19-12 20"6o 077 I '00 0-82534 23-90 26-12 093 The table shows that only when concentrations are referred to a definite weight (or volume) of solvent is there proportionality between concentration and osmotic pressure ; if they are re- ferred to a constant volume of solution ( column 2) the osmotic pressure increases faster than the concentration. The numbers in the fifth column show, however, that the osmotic pressure at 20 is on the average about 6 per cent, greater than the gas pressure. Curiously enough, the ratio is about the same at all temperatures from o to 25. Other Methods of Determining Osmotic Pressure The difficulties inherent in the direct determination of osmotic pressure can often be avoided by determining it indirectly by comparison with a solution of known osmotic pressure. Solutions which have the same osmotic pressure are said to be iso tonic or isosmotic. One such method, used by de Vries, depends on the use of plant cells as semi-permeable membranes. The protoplasmic layer which surrounds the cell-sap is permeable to water, but impermeable to many substances dissolved in the cell-sap, such as glucose and potassium malate. If such a cell is placed in contact with a solution of higher osmotic pressure than the cell-sap, water is withdrawn from the cell (just as a sugar solution absorbs water through a semi-permeable membrane) and the protoplasm shrinks away from the cell-wall ; a pheno- menon which is termed plasmolysis. If, however, the solution has a smaller osmotic pressure than that of the cell-sap, water enters the cell, the protoplasm expands and lines the cell-wall. The behaviour of the protoplasm, especially if coloured, can be 1 Zeitsch. physikal. Chem., 1888, 2, 415. 106 OUTLINES OF PHYSICAL CHEMISTRY followed under the microscope, and by trial a solution can be found which has comparatively little effect upon the appearance of the cell, and is therefore isotonic with the cell contents. A method depending on the same principle, in which red blood corpuscles are used instead of vegetable cells, has been described by Hamburger, 1 and the cell-walls of bacteria may also be used as semi-permeable membranes. The following table contains some " isotonic coefficients " as given by de Vries and by Hamburger ; the numbers represent the ratio of the osmotic pressures of equimokcular or equimolar solutions of the compounds mentioned. Isotonic Coefficients. Plasmolytic With Red Blood Substance. Method. Corpuscles. Cane sugar . . . 1-81 172 Potassium nitrate . . 3-0 3-0 Sodium chloride . .3*0 3-0 Calcium chloride . 4'33 4*05 It will be observed that, although the results obtained by the two methods agree fairly well, the osmotic pressures for equi- valent solutions are not equal, as would be expected according to Avogadro's hypothesis. The deviation from the expected result is such that potassium nitrate, for example, exerts an osmotic pressure about 17 times greater than that due to an equimolar solution of cane sugar. This observation is of fundamental importance in connection with modern views as to salt solutions. The Mechanism of Osmotic Pressure The foregoing considerations are quite independent of any hypothesis as to the exact nature of osmotic pressure, and so far no general agreement has been reached on this point. Van't Hoff inclines to the view that the pressure is to be accounted for on kinetic grounds, 2 perhaps as being due to the bombardment of the 1 Zeitsch. physikal. Chem., 1890, 6, 319. 2 For a discussion between van't Hoff and Lothar Meyer on this point, see Zeitsch. physikal. Chem. t 1890, 5, 23, 174. DILUTE SOLUTIONS 107 walls of the vessel by solute particles, in the same way as the pressure of a gas is produced according to the kinetic theory, and the fact that the osmotic pressure is proportional to the absolute temperature appears rather to support this suggestion. Other views are that it is connected with attraction between solvent and solute, or perhaps with surface tension effects. It may be pointed out that the equivalence of osmotic pressure and gas pressure in great dilution is no evidence that they arise from the same cause. As regards semi -permeable membranes, their efficiency does not depend, as might at first sight be sup- posed, on anything in the nature of a sieve action, only the smaller molecules being allowed to pass, but rather upon a difference in their solvent power for the two components of the mixture. The action of the palladium in Ramsay's experiment (p. 81) is very probably to be accounted for in this way, and that the same is true for solutions is well illustrated by an in- structive experiment due to Nernst and illustrated in Fig. 17. The wide cylin- drical glass tube A is closed at the bottom with an animal membrane (bladder) which has previously been thoroughly soaked in water; it is then filled with a, mixture of ether and benzene and fitted with a FIG. 17. cork and narrow tube, as shown in the figure. The cell is supported on a piece of wire gauze in a beaker partly filled with moist ether and loosely closed by a cork, B. After a time it will be observed that the liquid has risen to a considerable height in the narrow tube. What occurs in this case is that the ether dissolves in the water with which the membrane is soaked, and in this way is transferred inside the cell, whilst the benzene, being insoluble in water, is unable to pass out. loS OUTLINES OF PHYSICAL CHEMISTRY Similarly, the efficiency of the copper ferrocyanide membrane may depend on its solvent power for water but not for sugar. Osmotic Pressure and Diffusion It has already been pointed out that there is a close connection between osmotic pressure, as defined above, and diffusion; it is the difference in the osmotic pressure of cane sugar in different parts of a system which causes it in time to be uniformly distributed through that system. The diffusion of dissolved substances was very fully investigated by Graham, but the general law of diffusion was first enunciated by Fick. Fick's law is comprised in the equation ds = - DA^<#, ax which states that the amount of solute, ds, which passes through the cross-section of a diffusion cylinder is proportional to the area, A, of the cross-section, to the difference of concentration, dc t at two points at a distance dx from one another, to the time, dt t and to a constant, D, characteristic for the substance, and termed the diffusion-constant. As an illustration of the above formula, it was found that when dc=- 1 gram per c.c., dx=i cm., A = i sq. cm. and dt= one day, that 0-75 grams of sodium chloride passed between the two surfaces. This is excessively slow, in comparison with the high osmotic pressures set up even by dilute solutions, and the explanation is to be found in the great friction due to the smallness of the particles. As the driving force the osmotic pressure and the rate of diffusion are known, the resistance to the movement of the particles can be obtained. It has been calculated that the enormous force of four million tons weight is needed to force i gram mol of cane sugar through water at a velocity of i cm. per sec. The more rapid diffusion in gases may plausibly be ascribed to the much smaller resistance to the movement of the particles. The rate of diffusion is much influenced by temperature and, curiously enough, to about the same extent for all solutes DILUTE SOLUTIONS 109 the average increase is about -fa of the value at 1 8 for every degree C. MOLECULAR WEIGHT OF DISSOLVED SUBSTANCES. General It has already been pointed out (p. 103) that since Avogadro's hypothesis is valid for solutions, the molecular weight of a dissolved substance can readily be calculated when the osmotic pressure exerted by a solution of known concentration at known temperature and pressure is known. An illustration of this is given on the next page. As, however, the direct measure- ment of osmotic pressure is a matter of considerable difficulty, it has been found more convenient for the purpose to measure other properties of solutions, the relationship of which to the osmotic pressure is known. The only three methods which can be dealt with here are : (1) The lowering of vapour pressure ; (2) The elevation of boiling-point ; (3) The lowering of freezing-point, brought about by adding a known weight of solute to a known weight or volume of solvent. It can be shown by thermodynamical reasoning (p. 131) that un- der certain conditions the lowering of vapour pressure, the eleva- tion of the boiling-point and the lowering of the freezing-point due to the addition of a definite quantity of solute to a definite volume of solvent are each proportional to the osmotic pressure of the solution. Further, the equations expressing the exact relation- ships between these three factors and the osmotic pressure have also been established, 1 and all these theoretical deductions have been fully confirmed by experiment. // follows that just as equimolecular quantities of different substances in equal volumes of the same solvent exert the same osmotic pressure, so equimole- cular quantities of different substances in equal volumes of the same solvent raise the boiling-point) lower the freezing-point, and lower the vapour tension to the same extent. These statements find a very simple representation on the molecular theory. Since 1 Appendix, pp. 131-138. no OUTLINES OF PHYSICAL CHEMISTRY equimolecular quantities of different substances contain the same number of molecules, it follows that the magnitude of the osmotic pressure, lowering of vapour pressure, etc., depends only on the number of particles present and is independent of their nature (colligative properties, p. 63). The molecular weight of the solute could, of course, be obtained by determining one of the factors (i), (2), (3) and then calculating the value of the osmotic pressure, but it is much simpler to obtain the molecular weight by comparison with a substance of known molecular weight. It may be mentioned that besides the methods just indicated, there are other analogous methods for determining molecular weights which, from considerations of space, cannot be referred to here. Nernst has pointed out that any process involving the separation of solvent and solute can be used for determining molecular weights, and a little consideration will show that the four methods just mentioned come under this heading. Moreover, the osmotic effect of the solute is to diminish tha readiness with which part of the solvent may be separated from the solution, and the effect of the solute on the boiling- and freezing-points of the solvent must therefore be in the direction already indicated. The mathematical proof of the connection between these four properties depends upon the equivalence of the work done in removing part of the solvent from the solu- tion (Appendix). The four different methods for determining molecular weights in solution and the general nature of the results obtained will now be considered in detail. Molecular Weights from Osmotic Pressure Measure- ments, (a) from absolute values of the osmotic pressure The principle of this method has already been discussed (p. 103). If g grams of substance, dissolved in v c.c. of solvent, gives an osmotic pressure of/ cm. at T abs., the molecular weight, m, will be that quantity which, when present in 22,400 c.c. of solvent, will give an osmotic pressure of 76 cm. Hence, since is proportional to the amount of substance used (p. 26), DILUTE SOLUTIONS in pv 22,400 x 76 g x 22,400 x 76 x (273 + f) or /;/ = - 7 - 273/2? As an example, we will take an experiment of Morse and Frazer (p. 105) in which a solution containing 34-3 grams of sugar in 1000 c.c. (really 1000 grams) of water gave an osmotic pressure of 2*522 atmospheres = 191*6 cm. at 20. Hence m = 34-2 x 22,400 x 76 x 293 = 6 . Q 273 x 191*6 x 1000 as compared with the theoretical value of 342. Alternatively, by formula (2) p. 36 m = g RT -342 x 0-08205 x 293 = 6 pv 2*522 x i (b] By comparison of osmotic pressures Since equimolecular solutions in the same solvent have the same osmotic pressure, it is only necessary to find the strengths of two solutions which are in osmotic equilibrium (isotonic), and if the molecular weight of one solute is known that of the other can be calculated; De Vries found that a 3*42 per cent, solution of cane sugal was isotonic with a 5*96 per cent, solution of raffinose, the molecular weight of which was then unknown. If it be re presented by x, then 3-42 : 5-96 : : 342 : : x, whence # = 596. This result has since been confirmed by chemical methods. Lowering of Yapour Pressure It has long been known that the vapour pressure of a liquid is diminished when a non- volatile substance is dissolved in it, and that the diminution is proportional to the amount of solute added. In 1887 Raoult, on the basis of a large amount of experimental work, established the following important rule : Equimolecular quantities of differ- ent substances, dissolved in equal volumes of the same solvent, lower the vapour pressure to the same extent. On comparing the relative lowering (i.e., the ratio of the observed lowering and the original pressure) in different solvents, the same observer discovered another important rule, which may be expressed as follows : The relative lowering of vapour pressure is equal to the ratio of the number of molecules of solute and the total number of ii2 OUTLINES OF PHYSICAL CHEMISTRY molecules in the solution. Putting p^ and p 2 for the vapour pressures of solvent and solution respectively, the rule may be put in the form A -A = p l N + n in which n and N represent the number of molecules of solute and solvent respectively, In order to illustrate the validity of this rule, some results given by Raoult are quoted in the ac- companying table; the relative lowering is that due to the addition of i mol of solute to 100 mols of the various sol- vents : Solvent. H 2 O PC1 3 CS 2 CC1 4 CH 3 I (C 2 H 5 ) 2 O CH 3 OH Relative lowering croio2 0*0108 0*0105 0*0105 0-0105 0-0096 0*0103 The results agree excellently among themselves, and fairly well with the calculated value, i/ioi = 0*0099. About the same time van't Hoff introduced the conception of osmotic pressure, and showed by a thermodynamical method that the relation between the relative lowering of vapour pres- sure and the osmotic pressure is given by the equation _M. P , r v jRT' where M = molecular weight of solvent, in the form of vapour, s is its density, and the other symbols have their usual significance. The expression M/^RT is therefore constant, since it depends only on the nature of the solvent, and consequently the relative lowering of vapour-pressure is proportional to the osmotic pres- sure P. By using the general equation, PV = RT (where n is the number of mols of solute), P in equation (i) can be elimin- ated, 1 and we finally obtain i P -s -y , where V is the volume of the solvent. If N represents the number of mols of solvent, M its molecular weight and s its * *fT?npc density, the volume V of the solvent = MN/s. Hence P = -j^f ' and when this value is substituted in equation (i) we obtain (pi~Pz)IPi = n l^' DILUTE SOLUTIONS 113 A "A SL A = N- This equation differs from that of Kaoult in that the de- nominator on the right-hand side is N instead of N + n % but they become identical " at infinite dilution " when the volume of the solute is negligible in comparison with that of the solvent. By substituting for n and N gjm and W/M, where g and W are the weights of solute and solvent respectively, m is the (unknown) molecular weight of the solute and M that of the solvent in the form of vapour, we obtain the equation which enables us to calculate the molecular weight of a dissolved substance when the relative lowering produced by a known weight of solute in a known weight of solvent is known. As an illustration, an experiment of Smits may be quoted. He found that at o the lowering of vapour pressure produced by adding 29-0358 grams of sugar to 1000 grams of water is 0-00705 mm., the vapour pressure of water at that temperature being 4*62 mm. Hence 0-0070=1 20-0^8 x 18 --^ = y ^ , and m = 342, 4-02 looom in exact agreement with the theoretical value. As the lowering of vapour pressure is very small and not very easy to determine accurately by a statical method, it has not been very largely used for molecular weight determinations, the closely allied method depending on the elevation of the boiling-point being preferred. It has, however, one great advantage, inasmuch as, unlike the boiling-point and freezing- point methods, it can be used for the same solution at widely different temperatures. For this purpose, a dynamical method suggested by Ostwald and worked out by Walker l has certain advantages. A current of air is drawn in succession through (i) a set of Liebig's bulbs containing the solution of vapour 1 Zeitsch. physikal Chern., 1888, 2, 602. 8 ti4 ' OUTLINES OF PHYSICAL CHEMISTRY pressure / 2 (2) similar bulbs containing the pure solvent vapoui pressure p l (3) a U-tube containing concentrated sulphuric acid. In the first set of bulbs it becomes saturated up to / 2 with the vapour of the solvent, in the second set up to/^ in the U-tube the moisture is completely absorbed. The loss of weight in the second set of bulbs is proportional to p^ -/.,, and the gain in the U-tube to/ x (cf. p. Qi). 1 Elevation of Boiling-point A little consideration shows -that there is a close connection between this method of deter- mining molecular weights and that depending on the lowering of vapour pressure. A liquid boils when its vapour pressure is equal to that of the atmosphere. The presence of a solute lowers the vapour pressure, and to reach the same pressure as before we require to raise the temperature a little; it is evident that, to a first approximation, this elevation must be proportional to the lowering of vapour pressure. It follows that, in this case also, equimolecular quantities of different solutes, in equal volumes of the same solvent, raise the boiling- point to the same extent. The molecular weight of any soluble substance may therefore be found by comparing its effect on the boiling-point of a solvent with that of a substance of known molecular weight. For this purpose, it is convenient to determine the molecular elevation constant, K, for each solvent, that is, the elevation of boiling-point which would be produced by dissolving a mol of any substance in 100 grams or 100 c.c. of the solvent. Actually, of course, the elevation is determined in fairly dilute solution, and the value of the constant calculated on the assumption that the rise of boiling-point is proportional to the concentration. Then the weight in grams of any other compound which, when dissolved in 100 grams or 100 c.c. of the solvent, produces a rise of K degrees in the boiling-point' is the molecular weight. If g grams of substance, of unknown molecular weight, m, dissolved in L grams of solvent raises the boiling-point 8 1 A modification of this method has recently been used by Lord Berkeley and Hartley for the indirect determination of the osmotic pressure of con- centrated solutions of cane sugar (Proc. Roy. Soc. t 1906, 77A, 156. DILUTE SOLUTIONS 115 degrees, whilst m grams in 100 grams of solvent give a rise of K degrees, it follows, since loog/L is the number of grams of substance in 100 grams of solvent, that loop- , ioo,e-K T e : 8 : : m : : K, whence m = =r-f . L Lo In the course of the last few years, the constants for 100 grams and 100 c.c. have been very carefully determined for a large number of solvents, and some of the more important data are given in the accompanying table : Solvent. muiecuiar .c-ievc 100 grams. Ltion v^onsii 100 C.C. Water 5*2 5-4 Alcohol II'5 15-6 Ether 2I'O 30-3 Acetone . . 167 22'2 Benzene . 267 32-8 Chloroform 39' 27-7 Van't Hoff has shown that these constants, some of which had previously been obtained empirically by Raoult, can be calculated from the latent heat of vaporization, H, per gram of solvent, and its boiling-point, T, on the absolute scale, by means of the formula 0-02T 2 -IT- As an example, the calculated value for the molecular elevation constant for water, the latent heat of vaporization of which at its boiling-point is 537 calories, is K = (0-02 x (373) 2 )/S37 = 5' 2 in satisfactory agreement with the experimental value. For all solvents which have been carefully investigated, the experi- mental and calculated values are in good agreement. 1 1 The observed and calculated values for a large number of solvents are given in Landolt and Bornstein's tables. n6 OUTLINES OF PHYSICAL CHEMISTRY Experimental Determination of Molecular Weights by the Boiling-point Method The ease and certainty with which such determinations can now be made is largely due to the work of Beckmann. One of the methods sug- gested by him will first be considered, and then a method due to Landsberger, based on a different principle. (a) Beckmann s Method The apparatus used is represented in Fig. 1 8. The boiling-tube, A, is provided with two side tubes, /j, by means of which the solute (solid or liquid) is introduced, and / 2 , which is connected to a small condenser, by the action of which the amount of solvent is kept fairly constant. The solution is made to boil by the heat from a small screened burner, B, which can be carefully regulated, and the boiling liquid is insulated by means of an air jacket between the outer cylindrical glass tube, G, and the boiling tube. As the temperature of the vapour which escapes from a boiling solution is little, if any, above the boiling-point of the pure solvent, it is necessary to place the thermometer in the boiling liquid so that the bulb is completely immersed. The liquid tends to become superheated, and to eliminate this source of error Beckmann recommends filling up the boiling-tube nearly to the level of the liquid with glass beads or garnets, or, still better, with platinum tetrahedra. The thermometer repre- sented in the figure, which was specially designed by Beck- mann for this work, has a large bulb and an open scale, covering only 5-6, and graduated in T ^. To render the thermometer available for widely different temperatures, there is an arrangement by means of which the amount of mercury in the bulb can be so adjusted that the top of the thread can be brought on the scale at any desired temperature. The sol- vent, of which 10 to 15 grams is usually sufficient, is measured with a pipette, or weighed by difference in the boiling-tube itself ; the solute, if solid, may be conveniently introduced in the form of a compressed pastille or, if liquid, by means of a bent pipette. The boiling-point of the solvent is determined DILUTE SOLUTIONS 117 by causing it to boil fairly vigorously, and the temperature should remain constant within o-oi - 0-015 foi about twenty minutes FIG. 18. while readings are being taken. The temperature is then allowed to fall several degrees by removing the source of heat, the solute n8 OUTLINES OF PHYSICAL CHEMISTRY rapidly introduced, the boiling-point again determined, a fresh quantity of solute introduced, the boiling-point re-determined, and so on. The thermometer should be tapped before each reading. The amount of solute added may conveniently be such that the boiling-point is raised 0-15- 0-2 after each addi- tion. It may be pointed out that more satisfactory results are usually obtained when differences produced by the addition of more solute are used in the calculation than when differences in the boiling-point of solvent and solution are used. As an illustration of the calculation of the results, an. experi- ment with camphor in ethyl alcohol may be quoted. The addition of 0*56 grams of camphor to 16 grams of the solvent raised its boiling-point 0-278. Hence loo^K 100 x 0^56 x 1 1*5 ~TS~ 16 x 0-278 the theoretical value for C 10 H 16 O being 142. With proper precautions, the results obtained by this method are accurate within 3-4 per cent. (b) Landsberger s Method This method depends upon the fact that a solution can be heated to its boiling-point by passing into it a stream of the vapour of the boiling solvent. In this case there is little or no risk of superheating, as the temperature of the vapour is lower than the boiling-point of the solution. The boiling-point of the solvent is first determined by passing in vapour till the temperature ceases to rise, some of the solute is then added, and more vapour passed in until the boiling- point of the solution is reached. As, during the heating, the amount of solvent increases by condensation of vapour, the final amount of solution, upon which of course the observed boiling-point depends, is obtained by weighing after the experi- ment. If no great accuracy is required, the final volume may be read off in the boiling-tube, graduated for the purpose. Radiation may be minimised by jacketing the inner tube with the vapour of the boiling solvent. DILUTE SOLUTIONS 119 Depression of the Freezing-point This is the most accurate and most largely employed method for the deter- mination of molecular weights in solution. The two necessary conditions for its applicability are (i) the pure solvent, free from any of the solute, must separate out when the freezing-point is reached; (2) only a little of the solvent must have separated when the measurement is taken, otherwise the concentration of the solution will be appreciably altered. As in solubility determinations, we are dealing with an equilibrium (p. 84) in this case between ice and solution, and the experimental fact is that the more concentrated the solution the lower is the tem- perature at which equilibrium is reached. It is thus evident that if a large amount of the solvent separates in the solid form, the observed freezing-point is the temperature of equilibrium with a more concentrated solution than that originally prepared. In this case also, the osmotic pressure, and hence the mole- cular weight, could be calculated from the formula connecting osmotic pressure and depression of the freezing-point (p. 138), but the comparison method is always used. Just as for the boiling- point (p. 114) the molecular freezing-point depression , i.e., the depression produced by dissolving i mol of solute in 100 grams or 100 c.c. of the solvent, has been determined for a large number of solvents, and some of the more important data are given in the accompanying table. Molecular Depression. Solvent. 100 grams. 100 c.c. Water . .18-5 18-5 Benzol . . 50 56 Acetic acid -39 41 Phenol . . 74 Naphthalene .69 The molecular depression, K, can be calculated from the latent heat of fusion, H, of the solvent and its freezing point on the absolute scale by means of the expression. 120 OUTLINES OF PHYSICAL CHEMISTRY 0-02T 2 K H analogous to that which holds for the boiling-point elevation. Thus for water we have K = (0-02 x (273) 2 )/8o = i8'6. It may be mentioned, as a matter of historical interest, that the experimental values for K obtained with solutions of cane sugar by Raoult, Jones and others, were at first much greater than 1 8-6, but the careful experiments of Abegg, Loomis, Wildermann, and later of Raoult himself made it clear that the high values previously obtained were due to experimental error, and that, with proper precautions, the value of K deduced on the basis of the theory of solution was fully confirmed by experiment. If g grams of solute, in L grams of solvent, caused a depres- sion, A, of the freezing-point of the solvent, the molecular weight of the solute can be calculated from the formula loqg-K which exactly corresponds with that already given for elevation of boiling-point. Experimental Determination of Molecular Weights by the Freezing-point Method The apparatus which is used almost exclusively for this purpose was also designed by Beckmann, and is shown in Fig. 19. The inner tube, A, which contains the solvent, has a side tube by which the solute may be introduced, and is provided with a Beckmann thermometer, D, and a stirrer, preferably of platinum. The remainder of the apparatus consists of a tube, B, rather wider than A, and fitted into the loose cover of the large beaker, C, which contains water or a freezing-mixture (ice, or ice and salt), the temperature of which is 2-3 below the freezing-point of the solvent. In making an experiment, 15-20 grams of the solvent are weighed or measured into the tube, A, the stirrer and ther- mometer are put in place, and A is then placed in the wider DILUTE SOLUTIONS 121 tube B, which acts as an air mantle. The liquid is then stirred continuously and the thermometer observed. Owing to super- cooling, the temperature falls below the freezing-point of the solvent, but as soon as solid begins to separate, it rises rapidly, owing to the latent heat set free, and the highest temperature observed is taken as the freezing-point of the solvent. The tube is then removed from the bath, the solid allowed to melt, a weighed amount of the solute added, and the determination of the freezing-point repeated. A further por- tion of solute may then be added, and another reading taken. With some sol- vents there is considerable supercooling, and as this would be a source of error owing to separation of much solvent when solidification finally occurs, a small par- ticle of solid solvent is added to start solidification when the temperature has fallen 1-2 below the freezing-point. As an illustration of the calculation of the results, an experiment with napthalene in benzene may be quoted. The addition of 0*142 grams of the compound to 20*25 grams of the solvent lowered the freezing-point 0*2 84. Hence IPO x 0*142 x 51*2 126 AL 0*284 x 20*25 as compared with the theoretical value Fio. 19* 128. Results of Molecular Weight Determinations in Solu- tion. General The most important result of the numerous molecular weight determinations of dissolved substances which 122 OUTLINES OF PHYSICAL CHEMISTRY have been made in recent years is that in general the molecular weight in dilute solution is the same as that deduced from the simple chemical formula of the solute, as based on vapour density deter- minations or on its chemical behaviour. For example, the empirical formula of naphthalene is C 5 H 4 , and since one-eighth of the hydrogen can be replaced, the simplest chemical formula must be C 10 H 8 , and the molecular weight 128. Cryoscopic determinations in benzene gave a value 126, so that naphthalene is present as simple molecules in solution. The Van't Hoff-Raoult formulae (p. 112) on which the determination of molecular weights in solution depend, have been deduced on certain assumptions which hold only for dilute solutions, and it is of the utmost importance to bear in mind that there is no a priori reason why they should give trust- worthy results for concentrated solutions. The question as to how far the gas laws hold for concentrated solution, or what modifications are necessary, has been much debated, but so far no definite conclusions have been arrived at. It is mainly a matter for further experiment. It has already been shown (p. 105) that when V in the general formula is taken as the volume of the solvent, the normal molecular weight is obtained for cane sugar up to very high concentrations on the assumption that the gas laws are valid for these solutions. The same is true for other compounds, more particularly in organic solvents, as may be illustrated by the values obtained by Beckmann for camphor in benzene 1 (theoretical value 152) : Concentration. Value of m. Concentration. Value of m. 0*411 144 I2"ll 149 1-253 143 23-12 152 2791 145 26-59 J 54 5'897 147 The observed molecular weights depend not only on the nature of the solute and on the concentration, but also very largely on the nature of the solvent. Examples will be given in the follow- ing pages showing that in certain solvents the observed mole- 1 Concentration in grams per 100 grams of benzene. DILUTE SOLUTIONS 123 cular weights are often higher than those deduced from the chemical formula of the solute. The solute is then said to form complex molecules or to be associated, and the solvent is termed an associating solvent. In other solvents, on the contrary, the molecular weight may be equal to or less than that deduced from its chemical formula. In the latter case the solute is said to be dissociated, and the solvents in question are termed dissociating solvents. Abnormal Molecular Weights In order to illustrate the results of molecular weight determinations from a slightly differ- ent point of view, the following table contains the values for the molecular freezing-point depression, K, for three typical sol- vents, water, acetic acid and benzene. The data are mainly due to Raoult, and in calculating K it is assumed that the molecular weight corresponds with the ordinary chemical formula of the solute : Solvent Water. Solvent Acetic Acid. Solvent Benzene. Solute. K. Solute. K. Solute. K. Cane sugar 18*6 Methyl iodide . 38-8 Methyl iodide. 50-4 Acetone . 17-1 Ether . . . 39-4 Ether . . .497 Glycerol . 17*1 Acetone . . 38*1 Acetone . . 49-3 Urea . . 187 Methyl alcohol 357 Aniline . . . 46*3 HC1 . .39-1 HC1. . . . 17-2 Methyl alcohol 25*3 HN0 3 . 35'8 H 2 SO 4 . . .18-6 Phenol . . . 3 2 '4 KN0 3 . . 35'8 (CH 3 COO) 2 Mg 18-2 Acetic acid . 25-3 NaCl . . 36-0 Benzoic acid . 25*4 This very instructive table shows that, for all three solvents, there are two sets of values for K, one of which is approximately double the other. The question now arises as to which of these are the normal values, obtained when the solute exists as single molecules in solution. This can at once be settled by using van't HofFs formula, K = (o'o2T 2 )/H (p. 120), and we find that the normal depressions are 18-6, 39-0 and 51-2 for water, acetic acid and benzene respectively. This means that acetic acid, phenol and some other compounds dissolved in i2 4 OUTLINES OF PHYSICAL CHEMISTRY benzene produce only half the depression, in other words, exert only about half the osmotic pressure that would be expected ac- cording to their formulae, whilst in water certain acids and salts have an abnormally high osmotic pressure. The osmotic pressure of certain mineral acids in acetic acid is abnormally low. On the molecular theory, an abnormally small osmotic pressure shows that the number of particles is smaller than was anticipated. The experimental results can be satisfactorily accounted for on the view that acetic acid and benzoic acid exist as double molecules in benzene solution, and that phenol is polymerized to a somewhat smaller extent. This explanation seems the more plausible inasmuch as acetic acid contains com- plex molecules in the form of vapour (p. 41). It is mainly compounds containing the hydroxyl and cyanogen groups which are polymerized in non-dissociating solvents ; in dissociating solvents, such as water and acetic acid, 1 these com- pounds have normal molecular weights. It may be anticipated that the molecular complexity of solutes will be greater in concentrated solutions, and the avail- able data appear to show that such is the case. The results are, however, somewhat uncertain, inasmuch as in concentrated solution the gas laws are no longer valid (p. 122). Solvents such as benzene are sometimes termed associating solvents, but this probably does not mean that they exert any associating effect. There is a good deal of evidence to show that the substances existing as complex molecules in benzene and chloroform solution are complex in the free condition, and that the complex molecules are only partly broken up in so-called associating solvents. The explanation of the behaviour of solutes in water is by no means so simple, and can only be dealt with fully at a later stage. The data in the table indicate that cane sugar, urea, acetone, etc., are present as single molecules in solution, but hydrochloric acid, potassium nitrate, etc., be- have as if there were nearly double the number of molecules to 1 That acetic acid is in some cases at least a dissociating solvent is evident from the fact that the molecular weight of methyl alcohol in it is almost normal. DILUTE SOLUTIONS 125 be anticipated from the formulae. When van't Hoff put forward his theory of solutions he was quite unable to account for this behaviour, and contented himself with putting in the general gas equation a factor, /', to represent the abnormally high os- motic pressure, so that for salts and the so-called " strong " acids and bases in aqueous solution the equation became PV = iRT. The factor / can of course be obtained for aqueous solutions by dividing the experimental value of the molecular depression by the normal constant, 18*6, so that for potassium nitrate, for example, / = 3 5*8/1 8*6 = 1*92. Van't Hoff recalled the fact that ammonium chloride, in the form of vapour, exerts an abnormally high pressure, which is simply accounted for by its dissociation according to the equa- tion NH 4 C1 = NH 3 + HC1, but it did not appear that the results with salts, etc., could be explained in an analogous way. We shall see in detail later that the elucidation of the signifi- cance of the factor / was of the highest importance for the further development of the theory of solution. According to our present views, the substances which show abnormally high osmotic pressures are partially dissociated in solution, not into ordinary atoms, but into atoms or groups of atoms associated with electrical charges. The equation representing the partial splitting up of potassium nitrate, for example, may be written KNO 3 = K + NO 3 , which indicates that the solution contains potassium atoms associated with positive electricity, and an equal number of NO 3 groups, associated with negative elec- tricity. These charged atoms, or groups of atoms, are termed ions. Molecular Weight of Liquids Our knowledge as to the molecular weight of pure liquids is due mainly to the investi- gations of Eotvos (1886) and of Ramsay and Shields (1893), and is based on the remarkable rule, discovered by Eotvos, that the rate of change of the "molecular surface energy " of many 126 OUTLINES OF PHYSICAL CHEMISTRY liquids with temperature is the same. If y represents the sur- face tension and therefore the energy per sq. cm. of surface and s the "molecular sur f ace," the rule in question may be writ en < ....(<> where c is a constant. 1 The molecular surface, s, can be ex- pressed in terms of readily measurable quantities as follows : The molecular volume of any liquid is represented by M# where M is the molecular weight and v the specific volume. If the molecular volume is regarded as a cube, one edge of the cube will measure (Mz;)*, and the area of one side of it (Mv)L (M#)ir may therefore be called the molecular sur- face, s, and just as the relative molecular volumes of different liquids contain an equal number of molecules so the relative molecular surfaces for different liquids are such that an equal number of molecules lie on them. Equation (i) then becomes dt .. , _ , , 1 The student should make himself familiar with this method of repre- senting rate of change, as it is largely used in physical chemistry. It is perhaps most readily understood by considering the rate of change of position of a body as discussed in mechanics. If a body is moving with uniform velocity, the velocity can at once be found by dividing the distance, 5, traversed by the time, t, taken to traverse it, hence velocity = *li. The velocity may, however, be continually altering, and it is often desirable to express the velocity at any instant. It is not at first sight evident how this can be done, as it requires some time for the particle to traverse any measurable distance, and the velocity may be altering during that time. The nearest approach to the real velocity at any instant will be obtained by taking the time, and therefore the distance traversed, as small as possible. We might then imagine an ideal case in which 5 and t are taken so small that any error due to the variation of speed during the time t can be neglected. If we represent these values of s and t by ds and dt respectively, the speed of the particle at any instant will be given by ds{dt. In the example given in the text d(ys)jdt represents the rate of change of the product with temperature, and the equation shows that the rate ol change is constant. DILUTE SOLUTIONS 127 where y l and y 2 are the surface tensions of a liquid at the temperatures / x and / 2 respectively. From equation (2) we obtain, for the molecular weight M, M f_(fiL^\*. . . (3) The surface tension of a large number of pure liquids at different temperatures has been measured by Ramsay and Shields by observing the height to which they rose in capillary tubes. The results show that, if M is taken as the molecular weight corresponding with the simplest formula of the liquid, the value of c for the majority of substances is about 2*12. The method may be illustrated l by a determination of the molecular weight of liquid carbon disulphide. The experi- mental data are that y 33-6 ergs per sq. cm. at i9'4, and 29*4 ergs at 46'!: the specific volume (i/density) of carbon disulphide at 19-4 is 1/1-264; at 46*1 it is 1/1-223. Hence M=/- - 2-12(19-4 - 46-1) i* = ---- as compared with the value 76 calculated from the formula. As already indicated, the surface tension of a liquid in contact with its vapour diminishes as the temperature rises and becomes zero at the critical temperature, where the surface of separation beween liquid and vapour disappears (p. 50). If temperatures are measured downwards from the critical tem- perature as zero, dt in equation (i) p. 126 has a positive value, and therefore c is positive. In the next section for convenience positive values of the constant will be used. It should be added that the rule regarding the constancy of the expression d (ys)jdt only holds for temperatures at some distance (say 50) below the critical temperature. Results of Measurements Among the liquids which give values for c about 2-12 are the following : benzene 2'iy, carbon tetrachloride 2*11, silicon tetrachloride 2-03, ethyl iodide 2-10, ethyl ether 2-17, benzaldehyde 2-16, aniline 2-05. On the other Ramsay and Shields, Trans. Chem. Soc., 1893, 63, 1096. 128 OUTLINES OF PHYSICAL CHEMISTRY hand, many substances give values for c which are much smaller than 2-12 and which vary with the temperature. Thus for ethyl alcohol the values of d [y (Mz>) 2/3 ]/ which gives the connection between the relative lowering of vapour pressure and the osmotic pressure, and the Raoult-van't Hoff formula (P- IX 3). which is readily derived from equation (i) by means of the gas laws, can be deduced by a statical-thermodynamical method due to Arrhenius and also by a cyclical therrnodynamical method due to van't Hoff. These deductions will now be given. (i) The Statical Method A long tube R containing a solution of n mols of a non-volatile solute in N mols of solvent, 1 is closed at its lower end by a semi-permeable membrane and placed upright in a vessel C which contains pure solvent (fig. 20). The arrangement is covered by a bell-jar and all air is removed from the interior. When equilibrium be- tween solvent and solution is established through the semi-permeable membrane it is evident that the osmotic pressure is measured by the hydro- static pressure of the column of liquid (height h) in the tube. Now the pressure of vapour at the level, a, cf the surface of the solution must be the same inside and outside the tube. If this were not the case, evapora- tion or condensation of vapour would take place at the surface, a, and in either case the concentration of the solution would be aliered and the equilibrium between solution and solvent disturbed, which is contrary to the original postulate that the system is in equilibrium. If p 1 is the vapour pressure of the solvent and /> 2 that of the solution, the difference Pi - Pz ' s tne difference of pressure at the surface of the solvent and at 1 In calculating the number of mols of solvent, its molecular weight, M, is taken as that in the form of vapour (p. 112). 132 OUTLINES OF PHYSICAL CHEMISTRY the level a. This difference is due to the weight of a column of vapour of height h on unit area, therefore p^-p^hd. . (a) where d is the density of the^yapour. We have now to express d and h in a different form. If v l is the volume of i mol of the vapour, and M the molecular weight of the vapour in the gaseous form, we have d = M/z^ or t>! = Mfd. When/this value of z>! is substituted in/ the general gas equation p^^ = RT, we obtain , _ M/> t - j^r. Further, as the osmotic pressure, P, is measured by the weight of the column h, therefore P = hs' where s' is the density of the solution. ' If very dilute solutions are used, no appreciable error will be committed by substituting s, the density of the solvent, for 5', the density of the solution. Substituting these values of d and h in equation (a) we obtain RT FIG. 20. Pi ~ * RT ' which is equation (i), p. 112. From this equation, we obtain the formula, as already described (p. 112). (2) The Cyclical Method This thermodynamical proof of the above formula depends upon the performance of a cyclic process in which the system is finally brought back to its initial condition reversibly at con- stant temperature. The fundamental point to bear in mind in connection with such processes is that they must be conducted throughout under equilibrium conditions. It has already been pointed out (p. no) that the thermodynamical proof of the connection between osmotic pressure and the lowering of vapour pressure depends on the work done in removing solvent reversibly from a solution. There are two principal methods by which removal (or addition) of solvent can be accomplished; (a) If the solution is brought into contact with its own saturated vapour at constant temperature, the slightest diminution of the external pressure will effect the removal of part of the solvent ; on the other hand, the slightest increase of the external pressure will bring about condensation of vapour. If the change of volume of the solution is in each case very small compared with the total volume, the change in concentration can be neglected. APPENDIX 133 (b) A solution is placed in a cylinder closed at the bottom with a semi-permeable membrane, the cylinder is immersed in the pure solvent, and a movable piston rests on the upper surface. The solution and solvent will be in equilibrium through the semi-permeable membrane when the pressure on the piston is equal to the osmotic pressure. If the pressure is diminished ever so slightly by raising the piston, solvent will enter ; if the pressure on the piston is slightly increased, solvent will pass out through the membrane. We have, therefore, a second method by which solvent can be separated from a solution in a reversible n.anner, equilibrium being maintained throughout. The cyclic process, in which both these methods are used, will now be described. (1) From a solution containing n mols of solute to N mols of solvent, a quantity of solvent which originally contained i mol of solute is squeezed out reversibly by means of the piston and cylinder arrangement; the quantity thus removed is N/w mols. As the original quantity of solu- tion is supposed to be very great, its concentration, and therefore its osmotic pressure, are not appreciably altered in the process.' As the volume removed is that which contained i mol of solute, the work done on the system, which is the product of the change of volume and the pressure on the piston (the osmotic pressure), is equal to - RT ..... (i) (p. 27) if the gas laws apply. (2) The quantity of solvent is now converted reversibly into vapour by expansion at the pressure, p lt of the solvent ; the work gained is ap- proximately p l v l for i mol of vapour (the volume of the liquid being regarded as negligible in comparison), or -Pi*! - . () altogether. (3) The vapour is now allowed further to expand till its pressure falls to p 2 , the vapour pressure of the solution : in this process, an amount of work is done by the system represented approximately by per mol of vapour, where (p t + /> 2 )/ 2 ' s tne mean pressure during the small expansion. The quantity of vapour actually used is N/n mols, hence the total work done by the system is (4) The vapour, at the pressure p z , is now brought into contact with the solution, with which it is in equilibrium, and condensed reversibly, so that the system regains its initial state. The work done on the system in condensing the gas to liquid at the pressure / 2 i fi approximately - ~M 2 ..... ( iv ) As the entire cycle is carried through at constant temperature, there has on the whole been no transformation of heat into work or vice versa ; as the system is finally brought back to its initial condition, the work done on the system must on the whole be equal to the work done by the system ; in other words (i) + (ii) + (iii) + (iv) must be zero. 134 OUTLINES OF PHYSICAL CHEMISTRY Combining in the first place (ii), (iii), and (iv), we have which reduces to N /a, + zi\ , . , . N ., . - (-~^) Mi ~ PJ = n V ^ 1 ~ ^ where v is the mean volume of i mol of vapour. Substituting for v its value from the general gas equation, v = RT//>, we have finally l n p l as the work done by the system in the last three stages of the cy le. This must be equal to the work done on the system during the osmotic removal of solvent, hence Pi or &JL& = .? A N as before. The same result may be obtained still more simply by integration. The work done by the system in step (ii) is exactly balanced by that done on the system in (iv), as is evident from the factors themselves, if the pas laws hold. In (iii) bot'i the pressure and the volume change during the exoansion, hence work done by the system for i mol of vapour is equal to = I J = RT log 2 = RT log 1 (since p^ = / "V v = - RT log = - RT log, i - Pi \ Pi / Pi approximately, 2 or, for the total volume of vapour, The remainder of the proof is as above. Lowering Of Freezing-point The above formula has been deduced by an isothermal cyclic process, but the cyclic process by which the freezing-point formula is deduced cannot be carried through at constant temperature. We are therefore concerned witfi a new question, that of the relationship between heat and work. The law which applies in this case is the second law of thermodynamics, the deduction of which is to be 1 When the solution is dilute, p in the denominator may be put equal to p l without sensible error. 2 RT ,, >s the first term of the expansion of the logarithmic ,, . Th function. The more accurate form of the van't Hoff-Raoult formula is = CT, to which the usual form approximates in dilute solution. APPENDIX 13$ found in any advanced book on Physics, and which states that the maxi- mum work, <7A, obtainable from a given quantity of heat Q, in a reversible cycle is given by dT dA = q^ where the symbols have the usual significations (p. 151). A solution containing n mols of solute in N mols (W grams) of solvent is contained in the cylinder with semi-permeable membrane and movable piston already described. The freezing-point of the solvent is taken as T and that of the solution as T - dT. The stages in the cyclic process are as follows : 1 i) At the temperature T - dT an amount of solvent which originally contained i mol of solute is frozen out ; the amount in question is N/w mols or MN/w grams. The separation can be carried out at constant temperature provided that the amount of solution is so great that its con- centration is not thereby appreciably affected. The solidified solvent is then separated from the solution and the temperature of both raised to T. (2) The solidified solvent is fused, in which process H . calories are taken up, H being the heat effusion per gram. (3) The fused solvent is then brought into contact with the solution through the semi-permeable membrane under equilibrium conditions, that is, when the pressure on the piston is equal to the osmotic pressure of the solution (p. 133) and is allowed to mix reversibly with the solution. The work done by the system in this process is represented by the product of the osmotic pressure, P, and the volume, v, in which i mol of solute was diss Ived and is, therefore, according to the gas laws, equal to RT. (4) The system is finally cooled to the original temperature, T - dT, in order to complete the cycle. We have now to consider the work done in the different stages of the cycle. The heat expended in warming solution and solvent in (i) is practically compensated 1 by the heat given out in (4). Further, an amount of heat HW/w is taken in at the higher temperature T and a somewhat k ss amount given out at T - dT ; hence, by the second law of thermodynamics, the work done on the system is H W dT H . - . T . The only work done by the system is that expended in the osmotic readmission of the solvent, hence RT H W dT RT = H 'VT JT RT 2 , . or dT = -jj- . ^r . . . , . (i) 1 The two amounts are not exactly equal, but the difference can be made negligible in comparison with the heat taken up in the second stage of the cycle. 136 OUTLINES OF PHYSICAL CHEMISTRY If instead of H we use the molecular heat of fusion, \, we have \ = MH, and, further, N = W/M. Substituting these values in equation (i), the latter reduces to From this it is evident that the lowering of the freezing-point, like the relative lowering of vapour pressure, is proportional to the ratio of the number of mols of solute to the number of mols of solvent. From the above formula, or more readily from equation (i), above, an expression for K, the depression produced when i mol of solute is dissolved in 100 grams of solvent, can readily be obtained. R is approxi- mately = 2 whe.n expressed in calories, n = i and W = TOO. Hence we obtain, for this particular value of dT, aT - K - ^ -L - ' 02T2 (o) - H 'loo" H ' which is the formula given on p. 120. Elevation of Boiling-point By means of a cyclic process exactly corresponding with that already used in establishing the freezing-point formula, the formula connecting the elevation of the boiling-point with the latent heat of vaporisation of the solvent is obtained in the form where H is the heat of vaporisation of i gram of solvent at the tempera- ture of the experiment, and T is the boiling-point of the solvent en the absolute scale. Summary Of Formulae (a) Osmotic pressure and relative lowering of vapour-pressure. From formula (r) (p. 112) we obtain by substitution P = 82 ^ Pi-^P, atmospheres . where P is the osmotic pressure, expressed in atmospheres, s is the density of the solvent at the absolute temperature T, M is the molecular weight of the solvent in the form of vapour, and/> x and p% are the vapour-pressures of solvent and solution respectively. (b) Osmotic pressure and lowering of freezing-point From formula (i) (p. 137), by substitution roooHs dT P = - . -=r- atmospheres ; 24*22 T where H is the latent heat of fusion of the solvent in calories per gram, T is the freezing-point of the solvent on the absolute scale and dT is the freezing-point depression. Osmotic pressure and elevation of boiling-point The formula, which corresponds exactly with that for the freezing-point depression, is _ roooHs dT 24*22 ' T where H is the latent heat of vaporisatipn for i gram of solvent at its boiling-point, T is the boiling-point of the solvent on the absolute scale, and dT is the boiling-point elevation. CHAPTER VI THERMOCHEMISTRY General It is a matter of every-day experience that chemical changes are usually associated with the develop- ment or absorption of heat. When substances enter into chemical combination very readily, much heat is usually given out (for example, the combination of hydrogen and chlorine to form hydrogen chloride), but when combination is less vigorous, the heat given out is usually much less, and, in fact, heat may be absorbed in a chemical change. These facts, which were noticed very early in the history of chemistry, led to the suggestion that the amount of heat given out in a chemical change might be regarded as a measure of the chemical affinity of the reacting substances. Although, as will be shown later, this is not strictly true, there is, in many cases, a parallelism between chemical affinity and heat liberation. In thermochemistry, we are concerned with the heat equivalent of chemical changes. Heat is a form of energy, and therefore the laws regarding the transformations of energy are of importance for thermo- chemistry. It is shown in text-books of physics that there are different forms of energy, such as potential energy, kinetic energy, electrical energy, radiant energy and heat, and that these different forms of energy are mutually convertible. Further, when one form of energy is converted completely into another, there is always a definite relation between the amount which has disappeared and that which results. The 138 OUTLINES OF PHYSICAL CHEMISTRY best-known example of this is the relation between kinetic energy and heat, which has been very carefully investigated by Joule, Rowland and others. Kinetic energy may be measured in gram-centimetres or in ergs, and heat energy in calories (see p. xvii). The investigators just referred to found that i calorie = 42,650 gram-centimetres = 41,830,000 ergs, an equation representing the mechanical equivalent of heat. From the above considerations it follows that when a certain amount of one form of energy disappears an equivalent amount of another form of energy makes its appearance. These results are summarised in a law termed the Law of the Conservation of Energy, which may be expressed as follows : The energy of an isolated system is constant, i.e., it cannot be altered in amount by interactions between the parts of the system. The proof of this law lies in the experimental impossibility of perpetual motion it has been found impossible to construct a machine which will perform work without the expenditure of energy of some kind. In dealing with chemical changes, it has been found con- venient to employ the term chemical energy, and when two substances combine with liberation of heat, we say that chemical energy has been transformed to heat. To make this clear, we will consider a concrete case, the burning of carbon in oxygen with formation of carbon dioxide, a reaction which, as is well known, is attended with the liberation of a considerable amount of heat. The reaction can be carried out under such condi- tions that the heat given out when a definite weight of carbon combines with oxygen can be measured, and it has been found that when 12 grams of carbon and 32 grams of oxygen unite, 94,300 calories are liberated. This result may conveniently be represented by the equation C + O 2 = CO 2 + 94,300 cal. in which the symbols represent the atomic weights of the reacting elements in grams. The above equation is an illus- tration of the conversion of chemical energy into heat 12 THERMOCHEMISTRY 1 39 grams of free carbon and 32 grams of free oxygen possess 94,300 cal. more energy than the 44 grams of carbon dioxide formed by their union. From these and similar considerations it follows that the free elements must have much intrinsic energy, but the absolute amount of this energy in any par- ticular case is quite unknown. Fortunately, this is a matter of secondary importance, as chemical changes do not depend on the absolute amounts of energy, but only on the differences of energy of the reacting systems. So far, we have implicitly assumed that the increase or de- crease of internal energy when a system A changes to a system B is measured by the heat absorbed or given out during the reactions ; but this is not necessarily the case. In particular, external work may be done during the change, by which part of the energy is used up, or heat may be produced at the expense of external work (cf. p. 27). If the total diminution of internal energy in the change A -> B is represented by U, the heat given out by - q, and the external work done by the reacting sub- stances during the transformation by A, we have, by the prin- ciple of the conservation of energy, U = A - q. When no external work is done the total diminution of energy, U, is numerically equal to Q, the heat evolved in the reaction. The factor A is only of importance when gases are involved in the chemical change. Hess's Law It is an experimental fact that when the same chemical change takes place between definite amounts of two substances under the same conditions the same amount of heat is always given out provided that the final product or products are the same in each case. Thus when 12 grams of carbon combine with 32 grams of oxygen with formation of carbon dioxide, 94,300 cal. are always liberated, quite independently of the rate of combustion or of the nature of the intermediate pro- ducts. This law was first established experimentally by Hess in 1840, and may be illustrated by the conversion, by two different methods, of a system consisting of i mol of ammonia and of MO OUTLINES OF PHYSICAL CHEMISTRY hydrochloric acid respectively and a large amount of water, each taken separately, into a system consisting of i mol of ammonium chloride in a large excess of water. By the first method we measure (a) the heat change when i mol of gaseous ammonia and i mol of gaseous HC1 combine, (I)) the heat change when the solid ammonium chloride is dissolved in a large excess of water ; by the second method we measure the heat changes when (c) i mol of ammonia, (d) i mol of hydrochloric acid are dissolved separately in excess of water, and (e) when the two solutions are mixed. The results obtained were as follows : First Way. (a) NH 3 gas + HC1 gas = +42,100 cal. (b) NH 4 C1 + aq = - 3,900 cal. 38,200 cal. Second Way. (c) NH 3 gas -f aq = + 8,400 cal. (d) HClgas + aq + 17,300 cal. (e) HC1 aq + NH 3 <*q = + 12,300 cal. 38,000 cal. As will be seen, a+b=c+d+e within the limits of ex- perimental error. It can easily be shown that Hess's law follows at once from the principle of conservation of energy. This law is of the greatest importance for the indirect deter- mination of the heat changes involved in certain reactions which cannot be carried out directly. For example, we cannot determine directly the heat given out when carbon combines with oxygen to form carbon monoxide. The heat given out when 12 grams of carbon burn to carbon dioxide is 94,300 cal., which is, by Hess's law, equal to that produced when the same amount of carbon is burned to monoxide and the latter then converted to dioxide. The latter change gives out 68,100 THERMOCHEMISTRY 141 cal., and the reaction C + O = CO must therefore be associated with the liberation of 94,300 - 68,100 = 26,200 cal. Representation of Thermochemical Measurements. Heat of Formation. Heat of Solution As has already been pointed out, the results of thermochemical measure- ments may be conveniently represented by making the or- dinary chemical equation into an energy equation, for example, C + O 2 = CO a + 94,300 cal. Sometimes, if the final condition of the system is assumed to be known, the shorter form C, O 2 = 94,300 cal. may be used. When, as is frequently the case, the reacting substances are used in aqueous solution, this is indicated by adding aq to the formula in question. Thus the neutralisation of dilute hydro- chloric acid by sodium hydroxide is represented as follows : NaOH aq + HC1 aq = NaCl aq + 13,700 cal. The heat of formation of a compound is the heat given out when a mol of the compound is formed from its component ele- ments. Thus the heat of formation of carbon dioxide (at constant volume) is 94,300 cal. The above energy equations, e.g., that representing the formation of carbon dioxide, are, however, not complete, inasmuch as we do not know the in- trinsic energy associated with free carbon and oxygen re- spectively, nor do we know the differences of energy between the various elements, as they are not mutually convertible by any known means. We may therefore choose any arbitrary values for the intrinsic energies of the elements, and it has been found most convenient to put them all equal to zero. On this basis the intrinsic energy of carbon dioxide, being 94,300 cal. less than the sum of the intrinsic energies of the component elements, is - 94,300 cal., and, in general, the in- trinsic energy of a compound is numerically equal to its heat of formation, but with the sign reversed. i 4 2 OUTLINES OF PHYSICAL CHEMISTRY When the heats of formation of all the substances taking part in a reaction are known, the heat set free in the reaction can be calculated. One method of doing so is to apply the law that the heat of reaction is equal to the sum of the heats of formation of the substances formed minus the sum of the heats of formation of the substances used up. This law follows at once if we imagine the reacting substances first decomposed into their elements and these elements then combined to form the final products. In the first stage there would be absorbed an amount of heat equal to the sum of the heats of formation of the reacting substances, and in the second stage an amount of heat would be given out equal to the sum of the heats of formation of the products. An alternative method, the basis of which will be evident on a little consideration, is to write an energy equation in which the formulae of the various compounds are replaced by their intrinsic energies (the respective heats of formation with the signs reversed). As an example of the method, we may cal- culate the heat of reaction, x, when copper is displaced from copper sulphate in dilute solution by metallic zinc. The heat of formation of copper sulphate (from its elements) in dilute solution is 198,400 cal. and of zinc sulphate under the same conditions 248,500 cal. The energy equation for the chemical change is therefore Zn + CuSO 4 aq = Cu + ZnSO 4 aq o + ( 198,400) = o + (- 248,500) + x cal. whence x, the total heat liberated in the reaction, is 248,500 - 198,400 = 50,100 cal. In the same way an unknown heat of formation can be cal- culated when all the other heats of formation and the heat of reaction are known a method which, as shown in the last section, is particularly useful for obtaining the heats of forma- tion of substances such as carbon monoxide and methane, which cannot be determined directly, As an example, the THERMOCHEMISTRY 143 heat of formation of methane will be calculated. The heat given out when i mol of this compound is burned completely in oxygen is 213,800 cal., and the heat of formation of the products, carbon dioxide and water, are 94,300 and 68,300 cal. respectively. Representing the heat of formation of methane by x, its intrinsic energy therefore by - x, we have the equation CH 4 + 2O 2 = CO 2 + 2H 2 O -x + o = -94,300 + (-2 x 68,300) + 213,800 cal. Whence x = 17,100 cal. A compound such as methane, which is formed with libera- tion of heat, is termed an exothermic compound, whilst one which is formed with absorption of heat is termed an endo- thermic compound. The majority of stable compounds are exothermic. Among the best-known endothermic compounds are carbon disulphide, hydriodic acid, acetylene, cyanogen and ozone. It is not always easy to determine directly whether a compound is exothermic or endothermic, but this may be done indirectly by carrying out a chemical change with the compound itself and with the components separately and comparing the heat changes in the two cases. The method may be illustrated by reference to carbon disulphide. When burnt completely in oxygen, the gaseous compound gives out 265,100 cal. accord- ing to the equation CS 2 + 3 Q v ; if, on the other hand, (n-^ n 2 ) is negative, Q v > Q p . The heats of formation at constant volume of some important compounds are given in the accompanying table. The state- ments in brackets refer either to the state of the reacting sub- stances or of the product : THERMOCHEMISTRY Substance. Heat of Formation (Calories). H.p ( iquid) + 67,520 CO 2 (diamond) + 94.3 CO (diamond) + 26,600 SO 2 (rhombic sulphur) HF (gaseous fluorine) + 71,080 + 38,600 HC1 (gaseous chlorine) HBr (liquid bromine) + 22,000 + 8,400 HI (solid iodine) - 6,100 NH S + 12,000 NO' - 21,600 NO 9 - 7,700 KCl" + 105,600 KBr + 95,300 Heat of Combustion Whilst a great many inorganic re- actions are suitable for thermochemical measurements, this is .iot in general the case for organic reactions ; in fact, the only reaction which is largely used for the purpose is combustion in oxygen to carbon dioxide and water. The heat given out when a mol of a substance is completely burned in excess of oxygen is termed the heat of combustion^ and from this, by application of Hess's law, the heats of formation can be cal- culated, as has been done for methane and carbon disulphide, in the preceding section. Further, the heat given out in a chemical change can readily be calculated by Hess's law when the heats of combustion of the reacting substances are known it will clearly be equal to the sum of the heats of combustion of the substances which disappear less the sum of the heats of combustion of the substances formed. As an example, the heat of formation of ethyl acetate from ethyl alcohol and acetic acid may be calculated. The heat of combustion of ethyl alcohol is 34,000 cal, of acetic acid 21,000 cal., and of ethyl acetate 55,400 cal., whence the heat of formation of ethyl acetate is 34,000 + 21,000 55,400 = - 400 cal. Thermochemical Methods Two principal methods are employed in measuring the heat changes associated with chemical reactions. If the reaction takes place in solution, the water calorimeter, so largely used for purely physical measure- ments, may be employed. For the determination of heats of i 4 o OUTLINES OF PHYSICAL CHEMISTRY combustion, on the other hand, in which solids or liquids are burned completely in oxygen, special apparatus has been de- signed by Thomsen, Berthelot, Favre and Silbermann and others. (a) Reactions in Solution The change (chemical reaction, dilution or dissolution), the thermal effect of which is to be measured, is brought about in a test-tube deeply immersed in a large quantity of water, and the rise of temperature of the water is measured with a sensitive thermometer. When the weight of the water and the heat capacity of the calorimeter are known, the heat given out in the reaction can readily be calculated. Allowance must, of course, be made for the heat capacity of the solution in the test-tube. A simple modification of Berthelot's calorimeter, used by Nernst, is shown in Fig. 21. It consists of two glass beakers, the inner one being supported on corks, as shown, and nearly filled with water. Through the wooden cover, X, of the outer beaker pass a thin-walled test-tube, A, in which the reaction takes place, an accurate thermometer B, and a stirrer C of brass, or, better, of platinum. The water in the calorimeter is stirred during the reaction, which must be rapid, and the heat of reaction can then be calculated in the usual way when the weight of water in the calorimeter and the rise of temperature are known. Experiments on neutralization and on heat of solution are conveniently made in the inner beaker, the solution itself serving as calorimetric liquid. For dilute aqueous solutions, it is sufficiently accurate to assume that the heat capacity of the solution is the same as that of water. The chief source of error in the measurements is the loss of heat by radiation, which is minimised (a) by choosing for investigation reactions which are complete in a comparatively short time ; (b) by making the heat capacity of the calorimeter system large. It is of advantage so to arrange matters that the temperature of the calorimeter liquid is 1-2 below the atmospheric temperature before the reaction, and 1-2 above it after the reaction. THERMOCHEMISTRY 147 d\\\\\\\\ () Combustion in Oxygen This may conveniently be carried out in Berthelot's calorimetric bomb, a vessel of steel, lined with platinum and provided with an air-tight lid. The sub- stance for combustion is placed in the bomb, which is filled with oxygen at 20-25 atmo- spheres' pressure. The whole apparatus is then sunk in the water of the calorimeter, and the combustion initiated by heating electrically a small piece of iron wire placed in contact with the solid. Results of Thermochemi- cal Measurements Some of the more important results of thermochemical measure- ments have already been inci- dentally referred to in the preceding paragraphs. In stating the results of thermo- chemical measurements, the condition of the substances taking part in the reaction must always be clearly stated. This applies not only to the physical state, in connection with which allowance must be made for heat of vaporization, heat of fusion, etc., but also to the different allotropic modifications of the solid. Thus mono- clinic sulphur has 2300 cal. more internal energy than rhombic sulphur, and yellow phosphorus 27,300 cal. more than the red modification. The correction for change of state is often very great. For the transformation of water to steam at 100, it amounts to i 4 8 OUTLINES OF PHYSICAL CHEMISTRY about 537 x 18 = 9566 calories per mol. If, instead of the heat of formation of liquid water, which is 68,300 cal., the heat of formation of water vapour is required, it is 68,300 - 9570 = 58,730 cal. in round numbers. As regards the thermochemistry of salt solutions, one or two experimental results may be mentioned which will find an interpretation later. When dilute solutions of two salts, such as po'a^sium nitrate and sodium chloride, are mixed, heat is neither given out nor absorbed. This important result is termed the Law of thermoneutrality of salt solutions (p. 279). Further, when a mol of any strong monobasic acid is neutralized by a strong base, the rame amount of heat, 13,700 cal., is always liberated (p. 284). The heat of formation of salts in dilute aqueous solution is obtained by the addition of two factors, one pertaining to the positive, the other to the negative part of the molecule ; in other words, the heat of formation of salts in dilute solution is a distinctly additive property. The same is true to some extent for the heat of combustion of organic compounds. For example, the difference in the heat of combustion of methane and ethane is 158,500 cal., and in general, for every increase of CH 2 , the heat of combustion increases by about 158,000 cal. From these and similar results, we can deduce the general rule that equal differences in composition correspond to approxi- mately equal differences in the heat of combustion. We may go further, and obtain definite values .for the heat of combustion of a carbon atom and a hydrogen atom as has already been done for atomic volumes ; the molecular heat of combustion is then the sum of the heats of combustion of the individual atoms. Experience shows that when allowance is made for double and triple bindings, the observed and calculated values for the heats of combustion of hydrocarbons agree fairly well. Relation of Chemical Affinity to Heat of Reaction- Very early in the study of chemistry, it becomes evident that chemical actions may be divided into two classes : (i) those THERMOCHEMISTRY 149 which under the conditions of the experiment are spontaneous or proceed of themselves, once they are started, e.g., the com- bination of carbon and oxygen ; (2) those which only proceed when forced by some external agency, e.g., the splitting up of mercuric oxide into mercury and oxygen. In this section we are concerned only with spontaneous changes. The direction in which a chemical change takes place in a system depends on the energy relations of the system. We are accustomed to say that the direction of the change is determined by the chemical affinity of the reacting substances, and it is a matter of the utmost importance to obtain a numerical expression for the chemical affinity or driving force in a chemical system, the driving force being defined in such a way that the chemical change proceeds in the direction in which it acts, and comes to a standstill when the driving force is zero. Most reactions in which there is a considerable transformation of chemical energy, and therefore a considerable development of other forms of energy, such as heat or electrical energy, proceed very rapidly (for example, the combination of hydrogen and chlorine), whilst reactions in which less chemical energy is transformed are usually much less vigorous (for example, the combination of hydrogen and iodine). It seems, therefore, at first sight plausible to measure the chemical affinity in a system by the amount of heat liberated in the reaction (Thomsen, Berthelot). As, however, chemical affinity has been defined as acting in the direction in which spontaneous chemical change takes place, it would follow that only reactions in which heat is given out can take place spontaneously. This deduction is contrary to experience. Water can spontaneously pass into vapour, although in the process heat is absorbed, and many salts, such* as ammonium chloride, dissolve in water with absorption of heat. It is clear, therefore, that chemical affinity, as above defined, cannot be measured by the total heat liberated in the reaction. iSc OUTLINES OF PHYSICAL CHEMISTRY The importance for technical purposes of such a reaction as the burning of coal in oxygen is not so much the total heat obtainable by the change as the amount of work which the change may be made to perform. In a similar way, it has been found convenient to measure the chemical affinity of a system by the maximum amount of external work which, under suitable conditions, the reaction may be made to perform* This is a special case of a very comprehensive natural law, which may be expressed as follows : All spontaneous reactions (in the widest sense, including neutralization of electrical charges, falling of liquids to a lower level, etc.) can be made to perform work, and all reactions which can be made to per- form work are spontaneous, /. 2NaCl + CaCO 3 , yet the sodium carbonate found on the shores of certain lakes in Egypt is produced according to the equation 2NaCl + CaCO 3 -> Na 2 CO 3 -f CaCl 2 , the converse of the first equation. In the latter case, the sodium chloride is present in solution in such large excess that the re- action proceeds in the direction indicated by the arrow, so that, according to Berthollet, an excess in quantity can compensate for a weakness in specific affinity. An important step forward was made in this subject by Berthelot and Pean de St. Gilles in 1862, in the course of an investigation on the formation of esters from acids and alcohol. For acetic acid and ethyl alcohol, the reaction may be repre- sented by the equation C 2 H 5 OH + CH 3 COOH ^ CH 3 COOC 2 H 5 + H 2 O. If one starts with equivalent amounts of acid and alcohol, 156 OUTLINES OF PHYSICAL CHEMISTRY the reaction proceeds till about 66 per cent, of the reacting substances have been used up, and then comes to a standstill. Similarly, if equivalent quantities of ethyl acetate and water are heated, the reaction proceeds in the reverse direction (indicated by the lower arrow) until 34 per cent, of the compounds have been used up and the mixture finally obtained is of the same composition as when acid and alcohol are the initial substances. A reaction of this type is termed a reversible reaction, and the facts are conveniently represented by the oppositely-directed arrows. When, however, for a fixed proportion of acid, varying amounts of alcohol are taken, the equilibrium point is greatly altered, as is shown in the accompanying table. The first and third columns show the proportion of alcohol present for i equivalent of acetic acid, and the second and fourth columns the proportion of acid per cent, converted to ester. Ester Formed. 82-8 88-2 93*2 lOO'O We here measure the amount of chemical action by the extent to which the acid is converted into ester, and the table shows very clearly the influence of the mass of the alcohol on the equilibrium. The influence of the relative proportions of the reacting substances on chemical action was thus clearly recognised, but was not accurately formulated till 1867. In that year, two Nor- wegian investigators, Guldberg and Waage, enunciated the Law of mass action, which may provisionally be expressed as follows : The amount of chemical action is proportional to the active mass of each of the substances reacting, active mass being defined as the molecular concentration of the reacting substance. The im- portant part of this statement is that the chemical activity of Equivalents of Alcohol. Ester Formed. Equivalents of Alcohol. 0'2 19*3 2'0 O'S I'O 42*0 66-5 * 4-0 I2'0 1-5 77'9 50*0 EQUILIBRIUM IN HOMOGENEOUS SYSTEMS 157 a substance is not proportional to the quantity present, but to its concentration, or amount in unit volume of the reaction mixture. The law applies in the first instance more particularly to gases and substances in solution ; the active mass of solids will be considered later. The " amount of chemical action " exerted by a certain sub- stance can be measured (a) from its influence on the equilibrium, as in the formation of ethyl acetate, just referred to ; (ft) from its influence on the rate of a chemical action, such as the inver- sion of cane sugar. The law of mass action can therefore be deduced from the results of kinetic or equilibrium experiments. Conversely, once the law is established, it can be employed both for the investigation of rates of reaction and of chemical equilibria, and it is the fundamental law in both these branches of physical chemistry. In the above form, the law of mass action cannot readily be applied, and it will therefore be formulated mathematically. For purposes of illustration, we choose a reversible reaction between two substances in which only one molecule of each reacts ; a typical case is the formation of ethyl acetate and water from ethyl alcohol and acetic acid, already referred to. Calling the molecular concentrations of the reacting substances a and b, the rate at which they combine is, according to the law of mass action, proportional to a and to b separately, and there- fore proportional to their product. We may therefore write for the initial velocity of reaction at the time t Q Rate^ oc ab or Rate The above is the strict mathematical form of the law of mass 160 OUTLINES OF PHYSICAL CHEMISTRY action, which in words may be expressed as follows : At equilibrium the product of the concentrations on one side, divided by the product of the concentrations on the other side, is constant at constant temperature. Thus for the reaction represented by the equation :- 2FeCl 3 + SnCl 2 =SnCl 4 + 2FeCl 2 we have k' CFeCIs CsnCl 3 r rs ^SnC1 4 ^FeCl-j Strict Proof of the Law of Mass Action The law of mass action, the meaning of which has been illustrated in the previous paragraphs, may be strictly proved by a thermo- dynamical method (van't Hoff, 1885, cf. p. 416), or by a molecular-kinetic method (van't Hoff, 1877). The latter proof is comparatively simple, and depends on the assumption that the rate of chemical change is proportional to the number of collisions between the reacting molecules, which, in sufficiently dilute solution, will be proportional to the respective concen- trations. Taking again ester formation as an example, the velocity of the direct change = C a i CO hoi Cadd an( * tnat ^ t ^ ie reverse change = ^jCester C wa ter. At equilibrium, the rates will just balance, and therefore As before, this equation may be put in the form ^alcohol ^acid i -r/- r - r - = T "* K> '-'ester Cwater ^ where the respective concentrations are those under equilibrium conditions, and K is the equilibrium constant. It follows from the assumptions made both in the thermo- dynamical and kinetic proofs that the law of mass action holds strictly only for very dilute solutions, but the experimental results show that it often holds with a fair degree of accuracy even for moderately concentrated solutions.^ EQUILIBRIUM IN HOMOGENEOUS SYSTEMS 161 EQUILIBRIUM IN GASEOUS SYSTEMS (a) Decomposition of Hydriodic Acid A typical example of equilibrium in a gaseous system is that between hydrogen, iodine and hydriodic acid, investigated by Bodenstein. 1 The reaction, which is represented by the equation H 2 + I 2 ^ 2HI, is a completely reversible one, the concentration at equilibrium being the same whether one starts with hydrogen and iodine or with hydriodic acid, if the conditions otherwise are the same. Applying the law of mass action, we get at once as shown in the previous paragraph. It is clear from the equation that if from one observation the respective molecular concentrations of iodine, hydrogen and hydriodic acid are known, K, the equilibrium constant at the temperature in question, can be calculated. The question now arises as to how the progress of the reaction can be followed, so that it may be known when equilibrium is attained. It is further necessary to find a method of measurement such that the equilibrium does not alter while the observations are being made. In this case it happens that both the direct and inverse reactions are extremely slow at room temperature, but are fairly rapid at 445, the tem- perature of boiling sulphur. If then the mixture is heated for a definite time at a high temperature and then cooled rapidly, the respective concentrations at high temperatures can be deter- mined at leisure by analysis. The reacting substances, in varying proportions, are heated at a definite temperature in sealed glass tubes for definite periods, and the amount of hydrogen then present measured after absorption of the iodine and hydriodic acid by means of potassium hydroxide. For the present, only results will be considered in which the tubes were heated so long at 445 that equilibrium was attained. Jn one experiment, 20-55 mols of hydrogen were heated with 1 Zeitsch. physikal. Cliem-, 1897, 2*, I. II 1 62 OUTLINES OF PHYSICAL CHEMISTRY 31*89 mols of iodine, and it was found that the mixture at equilibrium contained 2*06 mols of hydrogen, 13*40 mols of iodine and 36*98 mols of hydriodic acid in the same volume. Hence _ [HJflJ _ (2-06 x 13-40) *~" CTTTT9 7 7 c^\-> " O'O2OO. [HI] 2 (36'98) 2 Equation (i) could, of course, be tested by finding if the same value of K is obtained for different initial concentrations of the reacting substances, but it is in some respects preferable to calculate by means of the equation the proportion of hydriodic acid formed at equilibrium when different initial concentrations of the reacting substances are taken, and to compare the results with those actually observed. In the calculation, K is taken as 0*0200 at 445. If i mol of hydrogen is heated with a mols of iodine, and 2X mols of hydriodic acid are formed, i - x mols of hydrogen and a x mols of iodine will remain behind. Substituting in equation (i), (i - x)(a - x) . N - - ~ - - = K = 0*0200 . . (2) 4# 2 The first and second columns of the accompanying table contain the initial concentrations of hydrogen and iodine respectively, and the fourth and fifth columns the observed and calculated concentrations of hydriodic acid at equilibrium, the latter values being obtained from the expression ' + a ~ ^* + a " as s where s = i - 4K = 0*92 obtained by solving the quadratic equation (2) above. H 2 I a Lj/H 2 = a HI found 2* (calc.) 20*57 5*22 0-254 10-22 10-19 20*6 i4'45 0*702 25-72 25-54 20'55 31*89 1*552 36-98 37-13 20*41 52*8 2-538 38*68 39'oi 20*28 67*24 3*316 39-52 39-25, EQUILIBRIUM IN HOMOGENEOUS SYSTEMS 163 The close agreement between observed and calculated values shows that the law of mass action applies in this case. It can easily be shown from the fundamental equation that in this case the position of equilibrium is independent of the pressure or of the volume. Calling a, b and c the amounts of hydrogen, iodine and hydriodic acid present at equilibrium, the concentrations are a/V, and x molecules each of PC1 3 and C1 2 are formed, the concentrations of PQ 5> PC1 3 and C1 2 at equilibrium are (a x)/V, x/V and x/V re- spectively, and, substituting in the above equation, (a - *)V It will be observed that the equilibrium in this case depends on the volume, and the larger the volume the smaller is (a - x) in other words, the greater is the dissociation. An important point in connection with chemical equilibrium in general is the effect of the addition of excess of one of the products of decomposition (dissociation) on the degree of 164 OUTLINES OF PHYSICAL CHEMISTRY decomposition. If, for example, a mols of PC1 5 are vaporized in a volume V in which b mols of PC1 3 are already present, and if #! is the degree of dissociation of the pentachloride under these conditions, the relative concentrations of trichloride, penta- ci/loride and chlorine will be b 4 x lt a - x lt and x l respec- tively. The equilibrium equation is therefore fa) (b + xj _ (a - Xl )V where K has the same numerical value as for the pentachloride alone, provided that the volume V and the temperature are tfa same. If it is assumed that the degree of dissociation when PC1 6 is heated alone under the same conditions is 'not more than say 25 per cent., it is clear that the proportion of undis- sociated compound cannot bj very seriously increased by the presence of excess of PC1 3 . Hence when &, the initial amount of PC1 3 , is made very large, x lt the amount of chlorine present .at equilibrium must become very small in order that the pro- duct K (a - x-i) may retain approximately the same Value ; in other words, the dissociation of PC1 5 must then be very small. From these considerations we deduce the following important general rule : The degree of dissociation of a compound is diminished by addition of excess of one of the products oj dissociation provided that the volume remains constant. Equilibrium in Solutions of Non-Electrolytes As a* illustration of an equilibrium in solution, that between acid, alcohol, ester and water (p. 156) may be considered rather more fully. For this equilibrium, according to the law of mass action, we have If at the commencement a, b and c mols of acid, alcohol and water respectively are present in V litres, and under equi- librium conditions x mols of water and ester respectively have been formed, the respective concentrations are EQUILIBRIUM IN HOMOGENEOUS SYSTEMS 165 _ a-x r-_* . r - - . r _ + x ^acid y I ^alc. - y > ^ester y I Crater y ' whence, substituting in the above equation, (a-x)(i>-x) _ x(c + x) In this case also, the position of equilibrium is independent of the volume. The value of K may be obtained from the observation already mentioned, that when acid and alcohol are taken in equivalent proportions, two-thirds is changed to ester and water under equilibrium conditions. Hence This equation may now be employed, as in the case of hydriodic acid, to calculate the equilibrium conditions for varying initial concentrations of the reacting substances. As an example, we take the proportion of i mol of acetic acid converted to ester by varying proportions of alcohol, when the initial mixture contains neither ester nor water. The equation in this case simplifies to (I -*)(*-*) X* " ~ * whence x = |(i + b- JW&_ + i). The observed and cal- culated values of x are given in the table, and it will be seen that the agreement is very satisfactory, although the solution is sp concentrated that it is scarcely to be expected that the law of mass action will apply strictly. b x (found) x (calc.) * x (lound) x (calc.) '5 '5 0*049 0-67 0-519 0-528 0-08 0-078 0-078 I'O 0-665 0-667 0-18 0-171 0-17 1 '*5 0-819 o'75 0-28 0*226 0-232 2*0 0-858 0-845 o'SJ 0-293 0-311 2-24 0-876 0-864 0*50 0-414 0-42^ 8-0 0-966 '945 166 OUTLINES OF PHYSICAL CHEMISTRY As regards the practical investigation of this equilibrium, the reacting substances are heated in sealed tubes at constant temperature (say 100) till equilibrium is attained, cooled, and the contents titrated with dilute alkali, using phenolphthalein as indicator. As the concentrations of acid and alcohol before the experiment are known and the acid concentration after the at- tainment of equilibrium is obtained from the results of the titration, the proportion of ester formed can readily be calcu- lated. The equilibrium in salt solutions will be more conveniently dealt with at a later stage (Chapter XL). Influence of Temperature and Pressure on Chemical Equilibrium. General The equations for chemical equi- librium deduced by means of the law of mass action hold for all temperatures provided that all the components remain in the system : the only effect of change of temperature is to alter the value of the equilibrium constant. The displacement of equi- librium is connected with the heat liberated in the chemical change by the equation which shows that the rate of change of the logarithm of the equilibrium constant with temperature is equal to the heat evolved in the complete reaction l divided by twice the square of the absolute temperature at which the change takes place. Strictly speaking, the above equation holds only for the dis- placement of equilibrium due to an infinitely small change of temperature r/T, and must be integrated before it can be applied to a concrete case. This can readily be done on the assumption that Q remains constant between the two temperatures, which is in general only approximately true. Integration between the absolute temperatures Tj and T 2 gives on this assumption log.K, - log.K 2 = , - \ 1 2' 1 The negative sign is taken in order that Q may denote the heat evolved in the forward reaction (from left to right). EQUILIBRIUM IN HOMOGENEOUS SYSTEMS 167 in which K 1 and K 2 are the equilibrium constants at r l\ and T 2 respectively. When transformed to ordinary logarithms (by dividing by 2-3026) and R is put = 1*99 (p. 27), the above equation is obtained in the more convenient form . (2) In this equation, Q refers only to the heat used in doing internal work, and does not include that used in external work (p. 141). It applies, therefore, in the first instance, only to systems in which there is no change of volume, and if there is expansion or contraction, the corresponding correction must be applied (p. 27). The equation shows that Q may be calculated when the equilibrium constants for two near temperatures, T 1 and T 2 , are known. Conversely, when the heat change in a chemical reaction and the equilibrium constant for any one temperature are known, the condition of equilibrium at any other temperature may be calculated. The equation is particularly useful for the indirect determination of the heat of reaction at high temperatures (in gas reactions, for example) when the direct calorimetric determination is difficult or impossible. As an example of the application of the general equation (2), the heat of dissociation, Q, for hydrogen sulphide, represented by the equation 2H.,S; 2H 2 + S 2 , will be calculated. Ac- cording to Preuner, the equilibrium constant K of the equation nf4fvf = K > has the value 2 '9 x I0 ~ 5 at I220 abs< and L"-2^J 10-4 x io~ 5 at 1320 abs. Hence, substituting in equation (2), we have io'4 x io~ 5 Q (1320 - 1220) log 2^90 x io~ 5 45&i * (1320 x 1220) and Q = - 41,000 cal. approximately. A specially interesting case is that in which there is no heat change when the first system changes to the second. Since in this case Q = o, the right-hand side of equation (i) becomes zero, and therefore there should be no displacement of equili- t 1 68 OUTLINES OF PHYSICAL CHEMISTRY brium with temperature. The condition of zero heat of reaction is, as has already been pointed out (p. 145), approximately ful- filled in ester formation, and in accordance with this, Berthelot found that at 10 65*2 per cent, of the acid and alcohol change to ester and at 220 66'5 per cent. ; the displacement of equilibrium with temperature is therefore slight. There are certain rules of great importance which show qualitatively how the equilibrium is displaced with changes of temperature and pressure. If Q is the heat developed when the system A changes to the system B, and is positive, then with rise of temperature A increases at the expense of B ; con- versely, if Q is negative, B increases with rise of temperature at the expense of A. These statements may be summarised as follows : At constant volume increase of temperature favours the system formed under heat absorption and conversely. As an example, we may take nitrogen peroxide, N 2 O 4 ^ 2NO 2 , for which the change represented by the lower arrow is attended with the liberation of a large amount (12,600 cal.) of heat. Increase of temperature favours the reaction for which heat is absorbed, in this case the reaction represented by the upper arrow, so that as the temperature rises N, 2 O 4 is split up more completely into NO 2 molecules. Another interesting example is the relationship between oxygen and ozone, represented by the equation 2O 3 = 3O 2 + 2 x 29,600 cal. The equilibrium for the reaction 2O 3 ^3O,, is very near the oxygen side at the ordinary temperature, but increase of temperature must displace it in the direction repre- sented by the lower arrow, since under these circumstances heat is absorbed ; in other words, ozone becomes increasingly stable as the temperature rises. The experimental results so far obtained are in satisfactory agreement with the theory. 1 Compare Fischer and Marx, Berichte, 1907, 40, 443. At first sight this appears to be in contradiction to the well-known fact that when a mixture of oxygen and ozone is heated to 250 the ozone is pract cally destroyed. It must be remembered, however, that the mixture contains far too much ozone for equilibrium, but owing to the lo\v temperature it attains its true equilibrium very slowly. At 250, however, the attainment of equilibrium is fairly rapid. EQUILIBRIUM IN HOMOGENEOUS SYSTEMS 169 From the above considerations we conclude that endothermic compounds, such as ozone, acetylene and carbon disulphide, become increasingly stable as the temperature rises, whilst exothermic compounds undergo further dissociation. A similar law can be enunciated for the effect of pressure on equilibrium as follows : On increasing th j . pressure at constant temperature the equilibrium is displaced in the direction in which the volume diminishes. Taking as an illustration the gaseous equilibrium, PCl f ^PCl 3 + C1 2 in which the upper arrow indicates the direction of increase of volume, the rule indicates that increase of pressure will displace the equilibrium to the left, whilst decrease of pressure will favour the reverse change. As is well known, these deductions are in complete accord with the experimental facts. For reactions not attended by any appreciable change of volume, such as the decomposition of hydriodic acid at high temperatures, the equilibrium should not be altered by change of volume, a conclusion borne out by experiment (p. 163). Le Chatelier's Theorem Le Chatelier has pointed out that the rules above referred to with regard to the effect of changes of temperature and pressure on equilibria are special cases of a much more general law which may be enunciated as follows : IVhen one or more of the factors determining an equi- librium are altered, the equilibrium becomes displaced in such a way as to neutralize, as far as possible, the effect of the change. A little consideration will show that this rule affords a satisfac- tory interpretation of all the phenomena just mentioned. Relation between Chemical Equilibrium and Tem- perature. Nernst's Views Although the van't Hoff equation connecting equilibrium and temperature enables us to calculate the position of equilibrium at different tempera- tures when the position of equilibrium at one temperature and the heat of reaction are known, it has not until quite recently been possible to calculate chemical equilibria from thermal and thermochemical data alone. Within the last lyo OUTLINES OF PHYSICAL CHEMISTRY two or three years, the latter problem appears to have been to a great extent solved by Nernst. 1 The fundamental as- sumption, on the basis of which it has been found possible to deduce formulae connecting the equilibrium in a system with the thermal data characteristic of the reacting substances, is that the free energy, A, and the total heat of reaction, Q, are not only equal at the absolute zero, as already pointed out (p. 152), but their values coincide completely in the immediate vicinity of that point. It is evident that this assumption cannot be tested directly, but the fact that the formulae deduced on this basis have been to a great extent confirmed by experiment 2 goes far to justify it. There can be no doubt that the results just described con- stitute one of the most important advances in physics and chemistry of recent years. It is beyond the scope of the present book to discuss the question more fully, but it may be mentioned that the theory not only admits of the calcula- tion of equilibria in homogeneous and heterogeneous systems from thermal data, but also gives a formula representing the variation of vapour pressure with temperature. Practical Illustrations The law of mass action may be illustrated most conveniently by the action of water on bismuth chloride, represented by the equation BiCl 3 + H 2 O^BiOCl + 2HCl. When dilute hydrochloric acid is added to a mixture of the salt and water, the equilibrium is displaced in the direction represented by the lower arrow, and a homogeneous solution is obtained. If excess of water is added to this solution, the equilibrium is displaced in the direction represented by the upper arrow, and a precipitate of bismuth oxychloride is formed. The law may also be illustrated qualitatively by the inter- action of ferric chloride and ammonium thiocyanate to form 1 Nernst, Applications of Thermodynamics to Chemistry. London: Constable, 1907. Annual Reports, Chemical Society, 1906, pp. 2.0-22. 2 Nernst, loc. cit. EQUILIBRIUM IN HOMOGENEOUS SYSTEMS 171 blood-red ferric thiocyanate. 1 This reaction is of particular interest, as it was one of the first reversible reactions to be systematically investigated (J. H. Gladstone, i855). 2 The equation representing the reaction is as follows : FeCl 3 + 3NH 4 CNS ^ Fe(CNS) 3 + 3 NH 4 C1. Solutions of the salts are first prepared ; the thiocyanate solution contains 37 grams of the salt to 100 c.c. of water, and the ferric chloride solution 3 grams of the commercial salt and 12*5 c.c. of concentrated hydrochloric acid to 100 c.c. of water. 5 c.c. of each of the solutions are added to 2 litres of water and the solution divided between four beakers. The solutions are pale-red in colour, as the equilibrium lies considerably towards the left-hand side. To the contents of two of the beakers are added 5 c.c. of the ferric chloride and the thiocyanate solution respectively, and it will be observed that the solutions become deep red, owing to the displace- ment of the equilibrium in the direction of the upper arrow. On the other hand, the addition of 50 c.c. of a concentrated solution of ammonium chloride 3 to the solution in the third beaker makes it practically colourless, the equilibrium being displaced in the direction of the lower arrow, in accordance with the law of mass action. 1 Lash Miller and Kenrick, J. Amtf. Chem. Soc., 22, 291. 2 Phil. Trans. Roy. Soc., 1855, 179. :{ Strictly speaking, all the solutions should be made up to the same volume in each case, but for qualitative purposes the method described is sufficiently accurate. The deep-red colour is presumably due to the for- mation ot non-ionised ferric thiocyanate (p. 260) ; it cannot be due to Fe 1 " or to CNS 1 ions, which are practically colourless. CHAPTER VIII HETEROGENEOUS EQUILIBRIUM. THE PHASE RULE General In contrast to homogeneous systems, in which the composition is uniform throughout, heterogeneous systems are made up of matter in different states of aggregation. The separate portions of matter in equilibrium are usually termed phases ; each phase is itself homogeneous, and is separated by bounding surfaces from the other phases. Liquid water in equilibrium with its vapour is a heterogeneous system made up of two phases, the equilibrium in this case being of a physical nature. Another heterogeneous equilibrium, formed by calcium carbonate with its products of dissociation, consists of three phases, two of which are solid, calcium carbonate and calcium oxide, and one gaseous. A still more complicated case is the equilibrium between a solid salt, its saturated solution, and vapour, made up of a solid, a liquid and a gaseous phase. It should be remembered that though each phase must be homogeneous, both as regards chemical and physical pro- perties, it may be chemically complex. For example, a mixture of gases only forms a single phase, since gases are miscible in all proportions. Further, a phase may be of variable composi- tion, thus a solution only constitutes one phase, although it may vary greatly in concentration. Application of Law of Mass Action to Heterogeneoub Equilibrium It has already been shown that equilibria in homogeneous systems may be dealt with satisfactorily by 172 HETEROGENEOUS EQUILIBRIUM 173 means of the law of mass action, provided that the molecular condition of the reacting substances is known. The matter is, however, somewhat more complicated for heterogeneous equi- libria, more particularly when solid substances are present, as in the equilibrium between calcium carbonate, calcium oxide and carbon dioxide already referred to. Debray, who investi- gated this system very carefully, showed that, just as water at a definite temperature has a definite vapour pressure, independent of the amount of liquid present, there is a definite pressure of carbon dioxide over calcium carbonate and oxide at a definite temperature, independent of the amount or the relative propor- tions of the solids present. The question now arises as to how the law of mass action is to be applied to systems in which solids are present. This problem was solved by Guld- berg and Waage, who found that the experimental results, such as those for the dissociation of calcium carbonate, were satis- factorily represented on the assumption that the active mass oj a solid substance at a definite temperature is constant, i.e., inde- pendent of the amount of solid present. It was not at first clear what physical meaning is to be attached to this statement, but Nernst pointed out that for any such system it was sufficient to consider the equilibrium in the gaseous phase, the active mass of a solid being repre- sented as its concentration in the gaseous phase. In other words, a solid, like a liquid, may be regarded as having a definite vapour pressure at a definite temperature, independent of its amount. At first sight it may seem surprising to ascribe a definite vapour pressure to such a substance as calcium oxide, but it is well known that solids like bismuth and cadmium have definite vapour pressures at moderate temperatures, and there is every reason for supposing that the diminution of vapour pressure with fall of temperature is continuous. There is now no difficulty in applying the law of mass action to equilibria in which solid substances are concerned, for example, to the dissociation of calcium carbonate. For convenience, we will 174 OUTLINES OF PHYSICAL CHEMISTRY use the partial pressures, />, of the components in the gaseous phase as representing the active masses. 1 We then obtain CO whence pco = -7* - 3 = constant. / Otherwise expressed, since all the factors on the right-hand side of the equation are constant at constant temperature, the vapour pressure of carbon dioxide must be constant, which is in accordance with the experimental facts. It is clear from the form of the equation that the pressure remains constant only within limits of temperature such that both calcium carbonate and oxide are present. If the tem- perature is so high that no calcium carbonate is present, the pressure is no longer defined, but depends on the size of the vessel, etc. Dissociation of Salt Hydrates Other interesting examples of heterogeneous equilibrium are those between water vapour and salts with water of crystallisation. If, for example, crystallised copper sulphate, CuSO 4 , 5H 2 O is placed in a desiccator over concentrated sulphuric acid at 50, it gradually loses water and. finally only the anhydrous sulphate remains. If arrangements. are made for continuously observing the pressure during dehyd- ration, it will be found to remain constant at 47 mm. until the: salt has lost two molecules of water, it then drops to 30 mm. and remains constant until other two molecules of water have- been lost, when it suddenly drops to 4-4 mm. and v.mains constant till dehydration is complete. The explanation of the successive constant pressures observed during dehydration is similar to that already given for the constant pressure of carbon dioxide over calcium carbonate and oxide. At 50 the hydrates CuSO 4 , 5H 2 O and CuSO 4 , 3H 2 O are in equilibrium with a 1 The partial pressure of a gas is proportional to the number of particles present per unit volume and therefore to its molQQuJar Concentration or . active mass (cf. p. 156). HETEROGENEOUS EQUILIBRIUM 175 pressure of aqueous vapour = 47 mm., and as long as any of the pentahydrate is present, the pressure necessarily remains con- stant. When, however, all the pentahydrate is used up, the trihydrate begins to dehydrate, giving rise to a little of the monohydrate, CuSO 4 , H 2 O. As a new substance is then taking part in the equilibrium, the pressure of aqueous vapour neces- sarily alters, and remains at the new value until the trihydrate is used up. The successive equilibria are represented by the following equations : I. CuSO 4 , 5H 2 O;CuSO 4 , 3H 2 O + 2H 2 O. II. CuSO 4 , 3H 2 O^CuSO 4 , H 2 O + 2H 2 O. III. CuSO 4 , H 2 6^CuSO 4 + H 2 O. By applying the law of mass action to any of the above equations, it may easily be shown that the pressure of aqueous vapour must be constant at constant temperature. Putting the partial pressures of the pentahydrate and the trihydrate as Pj and P 2 respectively, we have from equation I. : whence / 2 H 2 o = 7-77- = constant. *i l 2 It is important to realise clearly that the observed pressure is not due to any one hydrate, it is only definite and fixed when both hydrates are present. The tension of aqueous vapour over hydrates, like the vapour pressure of water, in creases rapidly with the temperature. This is illustrated in the following table, in which the vapour pressures (in mm.) over a mixture of Na 2 HPO 4 , 7H 2 O and Na.,HPO 4 , and those of water at the same temperatures, are given : Temperature . . 12-3 16-3 207 249 31-5 36-4 40-0 Na 2 HPO 4 + o-7H 2 O . 4-8 6-9 9-4 12-9 21-3 30-5 41-2 Water .... 10-6 13-8 18-1 23-4 34-3 45-1 54 - g Ratio salt/water . . 0-46 0-50 0-52 0-55 0-62 0-68 075 The results throw light on the question of the efflorescence (giving up of water) and deliquescence (absorption of water) of .76 OUTLINES OF PHYSICAL CHEMISTRY hydrated salts in contact with the atmosphere. If a hydrate (in the presence of the next lower hydrate) has a higher vapour pressure than the ordinary pressure of aqueous vapour in the atmosphere, it will lose water and form a lower hydrate. For example, the salt Na 2 HPO 4 , i2H 2 O has a vapour pressure of over 1 8 mm. at 25, which is greater than the average pressure of aqueous vapour in the atmosphere at that temperature, though less than the saturation pressure (see table), and therefore the salt is efflorescent under ordinary conditions. On the other hand, the vapour tension of the heptahydrate at 25 is only 13 mm. and it is therefore stable in air. The table shows that the ratio of the vapour pressure of a hydrate to that of water increases rapidly with the temperature and ultimately it becomes greater than unity ; the vapour tension of the hydrate is then greater than that of water. Dissociation of Ammonium Hydrosulphide Solid ammonium hydrosulphide partly dissociates on heating into ammonia and hydrogen sulphide, according to the equation NH 4 HS^NH 3 + H 2 S. This equilibrium is of a different type to those already mentioned, as a solid dissociates into two gaseous components. Representing molecular concentrations as partial pressures, we obtain, on applying the law of mass action, - K/ NH4 Hs = constant, since the partial pressure of solid ammonium sulphide is constant at constant temperature. The equation indicates that the product of the partial pressures of the two gases is constant at constant temperature. When the gases are obtained by heating ammonium hydro- sulphide, they are necessarily present in equivalent amount and exert the same partial pressure. The above formula may, however, be tested by adding excess of one of the products of dissociation to the mixture. This was done by Isambert, with the result indicated in the following table, which holds for 25*1; the volume being kept constant throughout: HETEROGENEOUS EQUILIBRIUM 177 250-5 250-5 62,750 208*0 294*0 60,700 453-0 143-0 64,800 In the first experiment the gases are present in equivalent proportions, in the second experiment excess of hydrogen sulphide, in the third excess of ammonia have been added. The results indicate that the product of the pressures is con- stant within the limits of experimental error, as the theory indicates, and, further, that addition of excess of one of the products of dissociation diminishes the amount of the other, as already shown for phosphorus pentachloride (p. 163). Analogy between Solubility and Dissooiation There is a very close analogy between the solubility of solids in liquids and the equilibrium phenomena just considered, more particularly the dissociation of salt hydrates. In both cases there is equilibrium between the solid as such and the same sub- stance in the other (gaseous or liquid) phase. We have already seen, in the case of the hydrates of copper sulphate, that the vapour pressure (i.e., the concentration of vapour in the gas space) depends on the composition of the solid phases, and it is then easy to see that the solubility of sodium sulphate (its concentration in the liquid phase) must also depend on the composition of the solid phase. The solubility alters when the solid decahydrate changes to the anhydrous salt, just as does the vapour pressure when copper sulphate pentahydrate disappears. A further analogy between the two phenomena is that just as the addition of an indifferent gas to the gas phase does not alter the equilibrium, except in so far as the volume is changed, so the addition of an indifferent substance to a solu- tion does not greatly affect the solubility of the original solute. Distribution of a Solute between two Immiscible Liquids The distribution of a solute such as succinic acid bet-ween two immiscible liquids such as ether and water exactly corresponds with the distribution of a substance between the 12 178 OUTLINES OF PHYSICAL CHEMISTRY liquid and gas phase (p. 83), and therefore the rules already mentioned for the latter equilibrium apply unchanged to the former. The most important results may be expressed as follows (Nernst) : (1) If the molecukr weight of the solute is the same in both solvents, the distribution coefficient (the ratio of the concentra- tions in the two solvents after equilibrium is attained) is con- stant at constant temperature (Henry's law). (2) In presence of several solutes, the distribution for each solute separately is the same as if the others were not present (Dalton's law of partial pressures). The first rule may be illustrated by the results obtained by Nernst for the distribution of succinic acid between ether and water, which are given in the table : C x (in water) C a (in ether) Cj/C, 0*024 0*0046 5*2 0*070 0*013 ' 5'4 o'i2r 0*022 5*4 The results were obtained by shaking up varying quantities of succinic acid with 10 c.c. of water and 10 c.c. of ether in a separating funnel, and determining the concentrations of acid in the two layers after they had separated completely. The fact that the ratio Q/Cg is approximately constant shows that Henry's law applies. When the molecular weight of the solute is not the same in both solvents, the ratio of the concentrations is no longer constant, and, conversely, if the ratio of the concentrations is not constant at constant temperature, the molecular weight cannot be the same in both solvents. This is illustrated by the following results obtained by Nernst for the distribution of benzoic acid between water and benzene : Cj (in water) C 2 (in benzene) Cj/C 2 CJ */C^ 0*0150 0*242 0*062 0*0305 0*0195 0*412 0*048 0*0304 0*0289 0*970 0*030 0*0293 HETEROGENEOUS EQUILIBRIUM 179 As the table shows, the ratio Cj/Cg is not even approximately constant, but on the other hand, the ratio C,/ JC^ is constant (fourth column). A little consideration shows that this is connected with the fact already mentioned, that whilst benzoic acid has the normal molecular weight in water, in benzene it is present almost entirely as double molecules (p. 124). In this case also we may assume that there is a constant ratio between the concentrations of the simple molecules in the two phases, and as it may easily be shown (p. 267) that the concentration of the simple molecules in benzene is proportional to the square root of the total concentration, the results are in accord with the theory. The Phase Rule. Equilibrium between Water, Ice and Steam In the previous sections of this chapter, it has been shown that many heterogeneous equilibria can be dealt with satisfactorily by means of the law of mass action. This holds not only for phases of constant composition, but within limits also for phases of variable composition, such as solutions. With reference to dilute solutions there is, of course, no difficulty, as the active mass of the solute is proportional to its concentra- tion. This is not the case, however, for strong solutions, and the application of the law of mass action to these is attended with considerable uncertainty. As far back as 1874, a complete method for the representa- tion of chemical equilibria was developed by the American physicist, Willard Gibbs, which has come to be known as the phase rule. The first point to notice with regard to this method is that it is entirely independent of the molecular theory ; the composition of a system is determined by the number of in- dependently variable constituents, which Gibbs terms components. He then goes on to determine the number of " degrees of free- dom" of a system from the relation between the number of components and the number of phases. It is for this reason- that his method of classification is termed the phase rule. In order to make clear the meaning of the terms employed' it will be well, before enunciating the rule, to illustrate them by Solid 1 80 OUTLINES OF PHYSICAL CHEMISTRY means of a very ^simple case, namely water. As regards the equilibrium in this case, we may, according to the conditions of the experiment, have one, two or more phases present. Thus, under ordinary conditions of temperature and pressure, there are two phases, water and water vapour, in equilibrium. This equilibrium is represented in the accompanying diagram by the line OA (Fig. 22), temperature being measured along the horizontal and pressure along the vertical axes. It is only at points on the curve that there is equilibrium. If, for example, the pressure is kept below that represented by a point on the curve OA (by continuously increasing the volume) the whole of the water will be converted to vapour ; if, on the other hand, it is kept at a point a little above the curve at a definite temperature, the Vapour whole of the vapour will ulti- mately liquefy. When the temperature is a little below o, only ice and vapour are Temperature-* present, and the equilibrium FIG. 22. between them is represented on the diagram by the line OC, which is not continuous with OA. The two curves meet at O, and O is the point at which ice and water are in equilibrium with water vapour. It is easy to see that at this point ice and water have the same vapour pressure. If this were not so, vapour would distil from the phase with the higher vapour pressure to that with the lower vapour pressure till the first phase was entirely used up, a result in contradiction with the fact that the two phases remain in equilibrium at this point. Since o is the temperature at which ice and water are in equilibrium with their vapour under atmospheric pressure, and as pressure lowers the melting-point HETEROGENEOUS EQUILIBRIUM 181 of ice, the point O, at which the two phases are in equilibrium under the pressure of their own vapour (about 4'6 mm.), must be a little above o ; the actual value is + 0-007 C. The diagram is completed for stable phases by drawing the line OB, which represents the effect of pressure on the melting-point of ice ; the line is inclined towards the pressure axis because in- creased pressure lowers the melting-point. The point O is termed a triple point, because there, and there only, three phases are in equilibrium. At points along the curves two phases are in equilibrium, and under the con- ditions in the intermediate spaces only one phase is present, as the diagram shows. So far, only stable conditions have been considered, but unstable conditions may also occur. Thus water does not necessarily freeze at o ; if dust is carefully excluded, it is pos- sible to follow the vapour pressure curve for some degrees below zero. The part of the curve thus obtained is represented by the dotted line OA' which is continuous with OA and lies above OC, the vapour pressure curve for ice. These results illustrate two important rules : (i) there is no abrupt change in the properties of a liquid at its freezing-point when the solid phase does not separate ; (2) the vapour pressure of an unstable phase is greater than that of the stable phase at the same temperature. The last result may be anticipated, since it is then evident how an unstable phase may change to a stable phase by distillation. The phase rule may now be enunciated as follows : If P represents the number of phases in a system, C the number oj components and F the number of degrees of freedom, the rela- tion between the number of phases, components and degrees oj freedom is represented by the equation C P 4- 2 = F. The meaivng of the terms " component " and " degree of freedom "will become clear as we proceed. The former has already been defined as the smallest number of independent variables of which the system under consideration can be built i82 OUTLINES OF PHYSICAL CHEMISTRY up. Thus in the case of water, considered above, there is only one component, and the system calcium carbonate-calcium oxide-carbon dioxide can be built up from two components, say calcium oxide and carbon dioxide. Particular instances of the application of the phase rule will now be given. If the number of phases exceeds the number of components by 2, the system has no degrees of freedom (F = o), and is said to be non-variant. An illustration of this is the triple point O in the diagram for water (p. 180), where there are three phases (liquid water, ice and water vapour) and one component (water). If one of j:he variables, the temperature or the pressure, is altered and kept at the new value, one of the phases disappears ; in other words, the system has no degrees of freedom. If the number of phases exceeds the number of components by one F = i , and the system is said to be univariant. As an illus- tration, we take the case of water vapour, where there are two phases and one component, say any point on the line OA. In this case the temperature may be altered within limits without altering the number of phases. If the temperature is raised, the pressure will increase correspondingly, and the system will thus adjust itself to another point on the curve OA. Similarly, the pressure may be altered within limits, the system will re-attain to equilibrium by a change of temperature at the new pressure. If, however, the temperature be kept at an arbitrary value and the pressure is then changed, one of the phases will disappear ; the system has therefore one, and only one, degree of freedom. If the number of phases is equal to the number of components, the system lias two degrees of freedom, and is said to be divariant. The areas in the diagram (Fig. 22) are examples of this case there is one phase (vapour, liquid or solid) and one component. If, for instance, we consider the vapour phase, the temperature may be fixed at any desired point within the triangle AOC, and the pressure may still be altered within limits along a line parallel to the pressure axis without alteration in the number of phases, as long as the curves OA and OC are not reached. HETEROGENEOUS EQUILIBRIUM 183 If the number of phases is less than the number of com- ponents by one, the system is trivariant, and so on. This particular instance cannot occur in the case of water, but does so in a four-phase system, as described in the next section. Equilibrium between Four Phases of the same Sub- stance. Sulphur The diagram for water represents the equi- librium between three phases of the same substance. We are now concerned with sulphur, which is somewhat more compli- cated inasmuch as there are two solid phases, monoclinic and rhombic sulphur, in addition to the usual liquid and vapour phases. Rhombic sulphur is stable at the ordinary temperature, and on heating rapidly melts at 1 1 5. On being kept for some time in the neighbourhood of 100, however, it changes completely to monoclinic sulphur, which melts at 120. Monoclinic sulphur can be kept for an indefinite time at 100 without changing to rhombic ; it is therefore the stable phase under these conditions. Thus, just as water is the stable phase above o and ice is stable below o, there is a temperature above which monoclinic sulphur is stable, below which rhombic sulphur is stable, and at which the two forms are in equilibrium with their vapour. This tem- perature is termed the transition point, and occurs at 95 '6. The change of one form into another is under ordinary condi- tions comparatively slow, and it is therefore possible to determine the vapour pressure of rhombic sulphur up to its melting-point, and that of monoclinic sulphur below its transition point. Although the vapour pressure of solid sulphur is comparatively small, it has been measured directly down to 50. The complete equilibrium diagram, which includes the fixed points just mentioned, is represented in Fig. 23. O is the point at which rhombic and monoclinic sulphur are in equilibrium with sulphur vapour, and is consequently a triple point, analogous to that /or water ; OB is the vapour-pressure curve of rhombic sulphur, and OA that of monoclinic sulphur. OA', which is continuous with OA, is the vapour-pressure curve of monoclinic 184 OUTLINES OF PHYSICAL CHEMISTRY sulphur in the unstable or metastable condition ; OB' similarly represents the vapour-pressure curve of rhombic sulphur in the unstable condition, and B' its melting-point. It will be observed that in both cases the metastable phase has the higher vapour pressure (p. 181). The line OC represents the effect of pressure on the transition point O and is therefore termed a transition curve ; since, contrary to the behaviour of water, pressure raises the transition point, the line is inclined away from the pressure Liquid (131, 400atmos.) Vapoui Temperature > FIG. 23. axis. Similarly, the curve AC represents the effect of pressure on the melting-point of monoclinic sulphur, and as it is less inclined away from the temperature axis than OC, the two lines meet at C at 131 under a pressure of 400 atmospheres. The curve AD is the vapour-pressure curve of liquid sulphur above 120, where the liquid is stable, and AB', continuous with DA, is the vapour-pressure curve of metastable liquid sulphur. As already indicated, B' represents the melting-point of metastabl^ HETEROGENEOUS EQUILIBRIUM 185 rhombic sulphur; in other words, it is a uiclastable triple point at which rhombic and liquid sulphur, both in the metastable condition, are in equilibrium with sulphur vapour. OB', as already indicated, represents the vapour-pressure curve of meta- stable rhombic sulphur, and the diagram is completed, both for stable and metastable phases, by B'C, which represents the effect of pressure on the melting-point of rhombic sulphur. Mono- clinic sulphur does not exist above the point C ; when fused sulphur solidifies at a pressure greater than 400 atmospheres, the rhombic form separates, whilst, as is well known, the monoclinic form first appears on solidification under ordinary pressure. The areas, as before, represent each a single phase, as shown in the diagram. Monoclinic sulphur is of particular interest, because it can only exist in the stable form within certain narrow limits of temperature and pressure, represented in the diagram by OAC. The phase rule is chiefly of importance in indicating what are the possible equilibrium conditions in a heterogeneous system, and in checking the experimental results. To illustrate this, we will use it to find out what are the possible non-variant systems in the case of sulphur, just considered. From the formula C P + 2 = F, since C = i, P must be three in order that F may be zero ; in other words, the system will be non-variant when three phases are present. As any three of the four phases may theoretically be in equilibrium, there must be four triple points, with the following phases : (a) Rhombic and monoclinic sulphur and vapour (the point O). (1)) Rhombic and monoclinic sulphur and liquid (the point C). (f) Rhombic sulphur, liquid and vapour (the point B'). (d) Monoclinic sulphur, liquid and vapour (the point A). The phase rule gives no information, however, as to whether the triple points indicated can actually be observed. In this particular case they are all attainable, as the diagram shows, but only because the change from rhombic to monoclinic sulphur above the triple point is comparatively slow. If it 1 86 OUTLINES OF PHYSICAL CHEMISTRY happened to be rapid, the point B' could not be actually observed. Systems of Two Components. Salt and Water The equilibrium conditions are somewhat more corAplicated on passing from systems of one component to those of two com- ponents, such as a salt and water. For simplicity, the equi- librium between potassium iodide and water will be considered, as the salt does not form hydrates with water under the con- ditions of the experiment. There will therefore be only four phases, solid salt, solu- tion, ice and vapour. There are three degrees 30 h :x / of freedom, as, in ad- dition to the tempera- ture and pressure, the concentration of the solution may now be varied. The equilibrium in this system is repre- sented in Fig. 24, the 10 20 30 .jo 50 GO 70 80 90 ordinates representing FlG - 24. temperatures and the abscissae concentra- tions. At o (A in the diagram) ice is in equilibrium with water and vapour, as has already been shown. If, now, a little potassium iodide is added to the water, the freezing-point is lowered, in other words, the temperature at which ice and water are in equilibrium is lowered by the addition of a salt, and the greater the proportion of salt present, the lower is the temperature of equilibrium. This is represented on the curve AO, which is the curve along which ice, solution and vapour are in equilibrium. On continued addition of potassium iodide, however, a point must be reached at which the solution is saturated with the salt, and on further addition of potassium _3o Grams KI in 100 grams solution HETEROGENEOUS EQUILIBRIUM 187 iodide, the latter must remain in the solid form in contact with ice and the solution. It is clear that, since the progressive lowering of the freezing-point depends upon the continuous increase in the concentration of the solution, the temperature corresponding with the point O must represent the lowest temperature attainable in this way under stable conditions. To complete the diagram, it is further necessary to determine the equilibrium curve for the solid salt, the solution and vapour. Looked at in another way, this will be the solubility curve of potassium iodide, which is represented by the curve OB. This curve is only slightly inclined away from the tempera- ture axis, corresponding with the fact that the solubility of potassium iodide only increases slowly with rise of temperature. The point O, which is the lowest temperature attainable with two components, is known as a eutectic point ; in the special case when the two components are a salt and water, it is termed a cryohydric point. The meaning of the diagram will be clearer if we consider what occurs when solutions of varying concentration are pro- gressively cooled. If, for example, we commence with a weak salt solution above its freezing-point (x in the diagram) and continuously withdraw heat, the temperature will fall (along xy) till the line OA is reached ; ice will then separate, and as the cooling is continued the solution will become more con- centrated and the composition will alter along the line AO until O is reached ; salt then separates as well as ice, and the solution will solidify completely at constant temperature, that of the point O. Similarly, if we start with a concentrated salt solution and lower the temperature until it reaches the curve OB, salt will separate and the composition will alter along the curve BO until it reaches the point O, when the mixture solidifies as a whole. Finally, if a mixture corre- sponding with the composition of the cryohydric mixture is cooled, the line parallel to xy representing the fall of tem- perature will meet the curve first at the point O, and the i88 OUTLINES OF PHYSICAL CHEMISTRY mixture will solidify at constant temperature. At the cryohydric temperature, the composition of the solid salt which separates is necessarily the same as that of the solution. Guthrie/who was the first to investigate these phenomena systematically, was of opinion that these mixtures of constant composition were definite hydrates, which were therefore termed cryohydrates. At first sight there seems much to be said for this view, as the separa- tion takes place at constant temperature, independent of the initial concentration, and the mixtures are crystalline. For the following reasons, however, it is now accepted that the cryo- hydrates are not chemical compounds : (a) the properties of the mixture (heat of solution, etc.) are the mean of the pro- perties of the constituents, which is seldom the case for a chemical compound ; (b) the components are not usually present in simple molar proportions ; and (c) the heterogeneous character of the mixture can be recognised by microscopic examination. The magnitude of the cryohydric temperature is 'of course con- ditioned by the effect of the salt in lowering the freezing-point of the solvent, and by its solubility at low temperatures. The eutectic temperatures of solutions of sodium and ammonium chlorides are 22 and 17 respectively, that of a solution of calcium chloride - 37. The application of the phase rule to this system will be readily understood from what has been said above. When there are four phases, ice, salt, solution and vapour, and two com- ponents, we find, by substituting in the formula C-P+2 = F, that F = o, that is, the four phases can only be in equilibrium at a single point, the point O in the diagram. When there are three phases, there is one degree of freedom, and the equi- librium is represented by a line (OA and OB in the diagram). If, for example, the condition of affairs is that represented by a point on the line OA, and the concentration of the solution is increased and kept at the new value (by further addition of salt when necessary) ice will dissolve, and the temperature will fall till it corresponds with that at which ice is in equilibrium ^ Phil. Ma*., 1884, [5], 17,462. HETEROGENEOUS EQUILIBRIUM r 8 9 with the more concentrated solution and vapour. If, then, while the concentration is still kept at the above value, the tempera- ture is altered and kept at the new value, one of the phases will disappear. The system is therefore univariant. If, instead of the concentration, one of the other variables is changed, corre- sponding changes in the remaining two variables take place, and the system adjusts itself till the three phases are again in equilibrium. If there are only two phases, for example, solution and vapour, the phase rule indicates that the system is bivariant, and it can readily be shown, by reasoning analogous to the above, that such is the case. Freezing Mixtures The use of mixtures of ice and salt as " freezing mixtures " for obtaining constant low temperatures, depends upon the principles just discussed. Suppose, for example, we begin with a fairly intimate mixture of ice and salt and a little water. When a little of the salt dissolves, the solution is no longer in equilibrium with ice. It will strive towards equilibrium by some more ice dissolving to dilute the solution, the latter, being now more unsaturated with regard to the salt, will dissolve more of it, more ice will go into solution and so on. As a consequence of these changes, heat must be absorbed in changing ice to water (latent heat of fusion of ice), and in connection with the heat of solution of the salt if, as is usually the case, the heat of solution is negative. The temperature, therefore, falls till the cryohydric point is reached, and then remains constant, since it is under these conditions that ice, salt, solution and vapour are in equilibrium. As the temperature of a cryohydric mixture is so much below atmospheric temperature, heat will continually be absorbed from the surroundings, but as long as both ice and solid salt are present, the heat will be used up in bringing about the change of state, and the temperature will remain constant. When, however, either ice or salt is used up, the temperature must necessarily begin to rise. 1 9 o OUTLINES OF PHYSICAL CHEMISTRY Systems of Two Components. General The particular case of a two-component or binary system already considered potassium iodide and water is very simple, for two reasons f . (i) the solid phases separate pure from the fused mass, in other words, the phases are not miscible in the solid state ; (2) the components do not enter into chemical combination. Com- plications occur when chemical compounds are formed, and when the solid phases separate as mixed crystals (p. 95) con- taining the two components in varying proportions. We will consider three comparatively simple cases of equilibrium in binary systems, the components being in all cases completely miscible in the fused state : (a) The components do not enter into chemical combination, and are not miscible in the solid state. (b) The components do not enter into chemical combination, but are completely miscible in the solid state. (c) The components form one chemical compound, but are not miscible with each other or with the compound in the solid state. Case (a). One example of this case is potassium iodide and water which has just been discussed. Another, which will be briefly considered, is the equilibrium between the metals zinc and cadmium. 1 To determine the equilibrium curves, mixtures of these metals in varying proportions are heated above the melting-point, and then allowed to cool slowly, the rate of cooling being observed with a thermocouple, one junction of which is placed in the mixture and the other kept at constant temperature. If the thermocouple is connected to a mirror galvanometer, the rate of cooling can be followed by the move- ment of a spot of light. Curves in which the times are plotted against the corresponding temperatures of the mixtures are represented in Fig. 256. The curves a, Z and b represent the cooling of mixtures corresponding with the points a, Z, b on the composition axis of the upper figure ; the curves o and 100 1 Hinrichs, Zeitsch. at ^50/^40 = 2 '88. It is import- ant to remember that the rate of most chemical reactions, as in the above example, is doubled or trebled for a rise of 10. This is shown in the accompanying table, which gives the quo- tient for 10 (kt + tflkt) for a few typical chemical reactions. 1 1 The third column contains the average value of the quotient for 10 be- tween the temperatures of observation. As data are not always available at intervals of 10, the average value of kt+iolkt may be calculated approxi- mately from the equation Iog 10 * 2 - Iog 10 *! = A (T 2 - T,) where k^ and h* are the velocity constants at the temperatures Tj and T 2 respectively. (See next section.) This equation gives us the value of A, and the quotient for 10 is given by log lo (**+ io)/*f = IOA or kt \\ As an example, we will work out the quotient for 10 for the inversion of cane sugar from the data given in the table. Log 10 35*5 - Iog 10 0765 is 1*66657 and as T - T : = 30 we obtain A = 0-05555. Hence log lo (kt + w)lkt = 0-5555 and (k t + io)/kt = 3-60 approximately. VELOCITY OF REACTION. CATALYSIS 227 Reaction. CH 3 COOC 2 H 5 CH 2 ClCOONa + NaOH CH 2 ClCOONa+H 2 O . C 2 H 5 ONa + CH 3 I Inversion of cane sugar . H 2 2 = H 2 + . Fermentation by yeast . Velocity Constants. 70 0*00089 0^000042 10-20 30-40 1347 = 44-90 = ^102 ' '648 0-01 5 / 10 = 0-00170 30=2-125 >& lft = o-oi8o Quotient for 10. 1-23 1*17 1-89 3*2 3'34 1*6 The quotient for 10 for reactions in solvents other than water is also between 2 and 3 in the majority of cases. According to the molecular theory, rise of temperature ought to increase the rate of chemical change, owing to the accelerating effect on molecular movements. This effect, however, would only increase proportionally to the square root of the absolute tempera- ture (p. 32), and it can easily be calculated on this basis that the quotient for 10 for a bimolecular reaction at the ordinary temperature would be about 1-04, much too small to account for the large temperature coefficient actually observed. Up to the present, no plausible explanation of the great magnitude of the temperature coefficient of chemical reactions has been given. The only other property which appears to increase as rapidly with temperature is the vapour pressure, and it is not improbable that there is a close connection between vapour pressure and chemical reactivity. At moderate temperatures the temperature coefficients of enzyme reactions are approximately the same as those of chemical reactions in general, but at temperatures in the neigh- bourhood of o, the rate of change of k with the temperature is often abnormally high, as the table shows. It is interesting to note that the rate of development of organisms, for example, the rate of growth of yeast cells, the rate of germination of certain seeds, and the rate of develop- 228 OUTLINES OF PHYSICAL CHEMISTRY merit of the eggs of fish, is also doubled or trebled for a rise of temperature of 10, and it has therefore been suggested that these processes are mainly chemical. Formulae connecting Reaction Yelocity and Tempera- ture As has already been pointed out (p. 167), the law con- necting the displacement of equilibrium with temperature is known. So far, however, no thoroughly satisfactory formula showing the relationship of rate of reaction and temperature has been established, although many more or less satisfactory empirical formulae have been suggested. If the relationship which has been shown to hold approximately for the rate of de- composition of dibromosuccinic acid that the quotient for 10 is the same at high as at low temperatures holds in general, the equation connecting k and T must be of the form dQQgjydT = A where A is constant. On integration, this becomes log* - AT + B, B being a second constant. This formula holds for the decom- position of nitric oxide and for certain other reactions, but is not generally valid. As a matter of fact, the quotient k t +Jk t generally diminishes with rise of temperature. An equation which takes account of this has been proposed by Arrhenius ; in its integrated form the equation is as follows : log* - - A/T + B. For two temperatures, T 1 and T 2 , for which the values of the velocity constant are * x and * 2 respectively, the above equation becomes log,* 2 ~ x M and when A is known (from two observations) the velocity constant for any other temperature can be calculated. Arrhenius showed that the above empirical equation repre- sents satisfactorily the influence of temperature on the rate of hydrolysis of cane sugar and on certain other reactions, and it VELOCITY OF REACTION. CATALYSIS 2*9 has since been employed by many other observers with fairly satisfactory results. A is a constant for any one reaction, but differs for different reactions. Practical Illustrations As the rate of chemical reactions alters so greatly with change of temperature, it is necessary in accurate experiments to work in a thermostat provided with a regulator to keep the temperature constant. For purposes of illustration, however, sufficiently accurate results can be obtained by using so large a volume of solution that the temperature does not alter appreciably during the reaction. Unimolecitlar Reaction. (a) Decomposition of Hydrogen Peroxide * To 200 c.c. of a mixture of one part of defibrinated ox-blood and 10,000 parts of water, an equal volume of about i/ 1 oo molar hydrogen peroxide (0-34 grams per litre) is added, and the mixture shaken. At first every ten minutes, and then at longer intervals, 25 c.c. of the reaction mixture is removed with a pipette, added to a little sulphuric acid, which at once stops the action, and titrated with i/ioo normal potassium permanganate. If pure hydrogen peroxide is not available, the commercial product should be neutralized with sodium hydroxide before use. Another portion of the original hydrogen peroxide solution should be titrated with permanganate, and if the reacting solutions have been measured carefully, the initial concentration in the reaction mixture may be taken as half that in the original solution. The observations should be calculated by substitution in the formula ijt log a/a-x *= 0-4343 k, valid for a unimolecular reaction. A corresponding experiment may be made with double the peroxide concentration, in order to illustrate the fact that the time taken to complete a certain fraction of the reaction is independent of the initial concentration. (b) Hydrolytic Decomposition of Cane Sugar in the Presence of Acids Equal volumes of a 20 per cent, solution of cane 1 Senter, Zeitsch. physikal. Chem., 1903, 44, 257. The amount of or- ganic matter is so small that the error in titration due to its reducing action on permanganate is negligible. 2 3 o OUTLINES OF PHYSICAL CHEMISTRY sugar and of normal hydrochloric acid, previously warmed to 25, are mixed, the observation tube of a polarimeter is filled with the mixture, and an observation of the rotation taken as quickly as possible. The polarimeter tube is then immersed in a thermostat at 25, and kept in the latter except when readings of the rotation are being made. In order that it may be conveniently immersed in a thermostat, the polarimeter tube is provided with a side tube, through which it is filled, and the end of which is not immersed. To prevent alterations while readings are being made, the tube is provided with a jacket filled with water at the temperature of the thermostat. Several chemists have described arrangements according to which the tube remains in the polarimeter throughout an ex- periment, the temperature being kept constant by passing a stream of water at constant temperature through the jacket of the polarimeter tube. 1 With rapid working, however, the simpler method described above gives excellent results. If it is convenient to make an observation after the reaction is complete (say 24 hours), the total change of reading is taken as a in the formula for a unimolecular reaction, and the differ- ence of the initial reading and that at the time t is proportional to x, the amount of sugar split up. If the reaction is not complete in a reasonable time, the final reading can be calculated from the fact that for every degree of rotation to the right in the original mixture, the wholly inverted mixture will rotate 0-315 to the left at 25. (c) Hydrolysis of Ethyl Acetate in the Presence of Hydro- chloric Acid The method of experiment in this case has already been described (p. 206). Bimolecular Reaction, (a) The rate of reaction is proportional to the concentration of each of the reacting substances This state- ment can be illustrated very satisfactorily by a method described by Noyes and Blanchard, and depending upon the fact that the time taken to reach a certain stage of a reaction is inversely proportional to its rate. 1 C/. Lowry, Trans. Faraday Society, 1907, 3, 119. VELOCITY OF REACTION. CATALYSIS 231 In a two-litre flask a mixture of 1600 c.c. of water, 50 c.c. half-normal hydrochloric acid and 20-30 c.c. of dilute mucilage of starch is prepared, and 400 c.c. of this mixture is placed in each of 4 half-litre flasks of clear glass, standing on white paper. For comparison, a fifth halt-litre flask contains 400 c.c. of water, 10 c.c. of starch solution, and sufficient of a n/ioo solution of iodine to give a blue colour of moderate depth. Half-normal solutions of potassium bromate (7 grams per half-litre) and of potassium iodide are also prepared. To the flasks I. and II. 5 c.c. of the bromate solution is added, and to III. and IV. 10 c.c. of the same solution. Then at a definite time, 5 c.c. of the iodide solution is added to flask I., the mixture rapidly shaken, and the time which elapses until the solution has the same depth as the test solution carefully noted. Then to flasks II., III. and IV. are added successively 10 c.c., 5 c.c. and ro c.c. of the iodide solution, and the times required to attain the same depth of colour as the test solution carefully noted in each case. If x is the time required when 10 c.c. of each reagent is used, 2x will be the time required when 10 c.c. of one solution and 5 c.c. of the other is used, and 4% when 5 c.c. of each solution is u^ed. If for some reason the reactions are too rapid, the strengths of the bromate and iodide solutions should be altered till intervals convenient for measurement are observed. (b) Quantitative measurement of a bimolecular reaction The rate of reaction between ethyl acetate and sodium hydroxide may be measured as described on a previous page. From a practical point of view, however, the measurement presents certain draw- backs because it is difficult to prepare a solution of sodium hy- droxide free from carbonate and also to prevent absorption of that gas from the air during the experiment. A reaction 1 free from these disadvantages, which is very rapid in dilute solution, is that between ethyl bromoacetate and sodium thiosulphate, represented by the equation CH 2 BrCOOC 2 H 5 + Na 2 S 2 O 3 = CH 2 (NaS 2 O 3 )COOC 2 H 6 + NaBr. 1 Slator, Trans. Chem. Society, 1905, 87, 484. 232 OUTLINES OF PHYSICAL CHEMISTRY The rate of the reaction can readily be followed by removing a portion of the reaction mixture from time to time and titrating with n/ioo iodine, which reacts only with the unaltered thio- sulphate. 300 c.c. of an approximately 1/60 normal solution of sodium thiosulphate is added to an equal volume of a dilute aqueous solution of ethyl bromoacetate (2-2-1 grams per litre) in a litre flask, the mixture shaken and the flask closed by a cork. At first every 5 minutes, and then every 10 or 15 minutes, 50 c.c. of the reaction mixture is removed with a pipette and titrated rapidly with n/ioo iodine, using starch as indicator. Seven or eight such titrations are made, and then, after an interval of 5-6 hours, when the reaction is presumably complete, a final titration is made in order to determine the excess of thiosulphate remaining. The initial concentration of thiosulphate, expressed in c.c. of the iodine used in titrating the mixture, can be obtained by titrating part of the original thiosulphate solution, and the initial concentration of bromo- acetate in the reaction-mixture is clearly equivalent to the amount of thiosulphate used up. The case is exactly analogous to that quoted on page 209, in which the sodium hydroxide is in excess, and the value of k may be obtained by substitution in equation (3), p. 208. Catalytic Actions The decomposition of hydrogen per- oxide by blood and of cane sugar in the presence of acids are examples of catalytic actions. Hydrogen peroxide can also be decomposed by a colloidal solution of platinum, which may be prepared as follows (Bredig): Two thick platinum wires dip into ice-cold water, and a current of about 10 amperes and 40 volts is employed. When the ends of the wires are kept 1-2 mm. apart, an electric arc passes between them, particles of platinum are torn off and remain suspended in the water. The solution is allowed to stand for some time, and filtered through a close filter. It represents a dark-coloured solution in which the particles cannot be detected with the ordinary VELOCITY OF REACTION. CATALYSIS 233 microscope. A very dilute solution may be used to decompose hydrogen peroxide, and the reaction may be measured as described above when blood is employed. Catalytic Action of Water This may be illustrated by its effect on the combustion of carbon monoxide in air, which does not take place in the entire absence of water vapour. Carbon monoxide is prepared by the action of strong sulphuric acid on sodium formate and is carefully dried by passing through two wash-bottles containing strong sulphuric acid, and finally through a U tube containing phosphorus pentoxide. Some time before the experiment is to be tried, a little strong sulphuric acid is put in the bottom of a wide-mouthed bottle with a close-fitting glass stopper, and the bottle allowed to stand, tightly stoppered, for some time. The carbon monoxide issuing from the apparatus burns readily in air, but is immediately extinguished if the wide- mouthed bottle is placed over it. If, however, a small drop of water is placed in the tube whence the gas is issuing, the gas will continue to burn when the bottle is placed over it. CHAPTER X ELECTRICAL CONDUCTIVITY Electrical Conductivity. General From very early times it was noticed that electricity can be conveyed in two ways : (i) In conductors of the first class, more particularly metals, without transfer of matter ; (2) in conductors of the second class salt solutions or fused salts with simultaneous decom- position of the conductor. We are here concerned only with conductors of the second class, but the use of the terms em- ployed in electrochemistry may be illustrated by reference to conduction in metals. For conductivity in general, Ohm's law holds, which may be enunciated as follows : The strength of the electric current passing through a conductor is proportional to the difference of potential between the two ends of the conductor, and in- versely proportional to the resistance of the latter. Strength of current is usually represented by C, difference of potential or electromotive force by E, and resistance by R ; Ohm's law may therefore be written symbolically as follows : "I The practical unit of electrical resistance is the ohm, that of electromotive force the volt, and that of current the ampere. The strength of an electric current can be measured in various ways, perhaps most conveniently by finding the weight of silver liberated from a solution of silver nitrate in a de finite interval of time. An ampere is that strength of current which in one 234 ELECTRICAL CONDUCTIVITY second will deposit 0*001118 grams of silver from a solution of silver nitrate under certain definite conditions. Quantity of elec- tricity is current strength x time; the amount of electricity which passes in one second with a current strength of i ampere is a coulomb. When there is a difference of potential of one volt between two ends of a conductor, and a current of i ampere is passing through it, the resistance of the conductor is i ohm. The resistance of a metallic conductor is proportional to its length and inversely proportional to its cross-section. Hence if / is the length and s the cross section, the resistance R is given by R = p -, where p is a constant depending only on the material of the conductor, the temperature, etc., and is termed the specific resistance. If both / and s are equal to unity (i cm.) the resistance is equal to p. The specific resistance, p, of a conductor is therefore the resistance in ohms which a cm. cube of it offers to the passage of electricity. If there is a difference of potential of i volt between two sides of the cube, and the current which passes is i ampere, the specific resistance of the cube is, by Ohm's law, = i. A conductor of low resist- ance is said to have a high electrical conductivity, that is, it readily allows electricity to pass. Conductivity is therefore the converse of resistance, and specific conductivity ', K = i//o, where p is specific resistance. Specific conductivity is measured in reciprocal ohms, sometimes termed mhos. In order to illustrate the magnitude of these factors, the specific resistance and the specific conductivity of a few typical substances at 18 are given in the table : 30 per cent Substance. Silver. Copper. Mercury. Gas carbon, sulphuric acid. Sp. resistance, p 0-0000016 o'oooooiy 0*00009 0-0050 0-74 Sp. conductivity, K 624,000 587,000 10,240 200 1-35 Silver has the highest conductivity of all known substances , 236 OUTLINES OF PHYSICAL CHEMISTRY gas carbon is a comparatively poor conductor; and 30, per cent, sulphuric acid, one of the best conducting solutions, is enormously inferior to the metals in this respect. Electrolysis of Solutions. Faraday's Laws We now consider the phenomena accompanying the conduction of electricity in aqueous solutions of salts. If, for example, two platinum plates, one connected to the positive, the other to the negative pole of a battery, are dipped into a solution of sodium sulphate, it will be observed that hydrogen is immediately given off at the plate connected to the negative pole of the battery, and oxygen at the plate connected to the positive pole. Further, if a few drops of litmus have previously been added to the solution, it will be noticed that the solution round the positive plate or pole becomes red, indicating the production of acid, and that round the negative pole becomes blue, showing the formation of alkali. An ammeter placed in the circuit will show that a current is passing through the solution, so that the chemical changes in question accompany the passage of the current. Even if the poles are far apart, the gases are liberated, and the acid and alkali appear immediately connection is made through the solution, and if the current is continued, the acid and alkali accumulate round the respective poles without any apparent change in the main bulk of liquid between the poles. These phenomena can scarcely be accounted for otherwise than by supposing that matter travels with the current, and that part travels towards the positive pole and part towards the negative pole. To these travelling parts of the solution Faraday gave the name of ions. It will be well to mention here the nomenclature used in this part of the subject. A solution or fused salt which con- ducts the electric current is termed an electrolyte. The plate in the solution connected to the positive pole of the battery is termed the positive pole, positive electrode or anode, that connected to the negative pole of the battery the negative pole, negative electrode or cathode. The ions which move ELECTRICAL CONDUCTIVITY 237 towards the anode are often termed ant'ons, those travelling towards the cathode cations. We will now consider the relationship between the amount of chemical action and the quantity of electricity passed through a solution. The amount of chemical action might be estimated by measuring the volume of gas liberated at one of the poles, or by the amount of metal deposited on an electrode. This question was investigated by Faraday, and as a result he established a law which bears his name, and which may be enunciated as follows : For the same electrolyte, the amount of chemical action is proportional to the quantity of electricity which passes. 1 Further, Faraday measured the relative quantities of substances liberated from different solutions by the same quantity of electricity, and was thus led to the discovery of his so-called second law : The quantities of substances liberated at the elec- trodes when the same quantity of electricity is passed through different solutions are proportional to their chemical equivalents. The chemical equivalent of any element (or group of elements) is equal to the atomic weight (or sum of the atomic weights) divided by the valency. The second law, therefore, states that if the same quantity of electricity is passed through solutions of sodium sulphate, cuprous chloride, cupric sulphate, silver nitrate and auric chloride, the relative amounts of hydrogen and the metals liberated are as follows : Electrolyte Na,,SO 4 CuCl CuSO 4 AgNO 8 AuCl 3 Electrochem. A * * o equivalent H= i ; O= f ; Cu = ^- 4 ; Cu = ^; Ag = ^?; Au=^ The above result may also be expresstd rather differently as follows : The electrochemical equivalents (the proportions of different elements set free by the same current) are proportional to the chemical equivalents. That quantity of electricity which passes through an electro- lyte when the chemical equivalent of an element (or group of 1 Faraday measured the amount of electricity by its action on a mag- netic needle. 238 OUTLINES OF PHYSICAL CHEMISTRY elements) in grams is being liberated will obviously be a quantity of very considerable importance in electrochemistry. Since i ampere in i second (a coulomb) liberates 0*00001036 grams of hydrogen, it follows that when the chemical equivalent of hydrogen or any other element is liberated, 1/0*00001036 = 96540 coulombs must pass through the electrolyte. It is often designated by the symbol F (faraday). One cou- lomb will liberate 35*45 x o'ooooio36 =0*000368 grams of chlorine, 127 x o*ooooio36 = o - ooi3i6 grams of iodine, and 108 x 0*00001036 = 0*001 1 1 8 grams of silver. Mechanism of Electrical Conductivity It has already been pointed out (p. 236) that during the electrolysis of sodium sulphate the products of electrolysis appear only at the poles, the main bulk of solution between the poles being apparently unaffected. This is most readily accounted for on the view that part of the solute is moving towards the positive and part towards the negative pole, these moving parts being termed anions and cations respectively. We now assume further that the cations are charged with positive electricity, and move towards the negatively charged cathode owing to electrical attraction ; similarly, the negatively charged anions are attracted to the cathode. When the ions reach the poles, they give up their charges, which neutralize a corresponding amount of the opposite kinds of electricity on the anode and cathode respec- tively, and then appear as the elements or compounds we are familiar with. The process of electrolysis is illustrated in Fig. 29. Into the vessel containing sodium sulphate solution dip two electrodes (on opposite sides of the vessel) connected with the positive and negative poles of the battery respectively. The direction of motion of the ions to the oppositely-charged poles is illustrated by the arrows. It is not always an easy matter to say what the moving ions are. It is only rarely that they are set free as such, since secondary reactions often take place at the electrodes. When a strong solution of cupric chloride is electrolysed, copper ELECTRICAL CONDUCTIVITY 239 and chlorine are liberated at the cathode and anode respectively, and it is probable that these substances are the ions. In the case of sodium sulphate, however, for which hydrogen and oxygen are the products of electrolysis, secondary reactions must take place. The current is in all probability conveyed through the solution by Na and SO 4 ions. When the former reach the cathode, they give up their charges and form metallic sodium, which immediately reacts with the water, forming sodium hydroxide and hydrogen. In the same way the SO 4 ions, on reaching the anode, give up their charges, and the free SO 4 group then reacts with the water according to the equation SO 4 + H 2 O = H 2 SO 4 + O, oxygen being liberated and sul- phuric acid regener- ated. In this way the phenomena al- ready described are readily accounted for. So far, we have assumed that the material of the elec- trodes is not acted on by the products of electrolysis. This is generally true when the electrodes are made of platinum or other resistant FIG. 29. metal, but in other cases secondary reactions take place between the discharged ions and the poles. Thus when a solution of copper sulphate is electrolysed between copper poles, the SO 4 ions, after losing their charges, react with the anode according to the equation Cu + SO 4 = CuSO 4 , so that the net result of the electrolysis of copper sulphate between copper poles is the transfer of copper from the anode to the cathode. 240 OUTLINES OF PHYSICAL CHEMISTRY We have assumed that*m a solution of sodium sulphate the moving ions are Na and SO 4 . As the Na ion moves towards the negative electrode, it must already be positively charged ; + this may be indicated thus : Na (Fig. 29), or, more concisely, by a dot, thus : Na\ As neither positive nor negative elec- tricity accumulates in the solution during electrolysis, the amount of positive electricity neutralized on the anode must be equivalent to that neutralized on the cathode. Hence, since two sodium ions are discharged for every SO 4 ion, the latter must carry double the amount of electricity that a sodium ion carries, and this is indicated by the symbols SO 4 or SO 4 " (Fig. 29). According to our present views, the metallic components of salts in solution are positively charged, the number of charges corresponding with the ordinary valencies of the metals. Some important cations are K*, Na', Ag', NH 4 ', Ca", Hg 2 ", Hg", Fe", Fe , etc. The remainder of the salt molecule constitutes the negative ion, which, like the positive ion, may have one, two or more (negative) electric charges. Among the more important anions are Cl', Br', I', NO 3 ', SO/', CO 3 ", PO 4 '", etc. Acids and bases deserve special consideration from this point of view. Since salts are derived from acids by replacing the hydrogen by metals, it is natural to suppose that the positive ion in aqueous solutions of acids is H", and that the remainder of the molecule constitutes the negative ion. On the other hand, aqueous solu- tions of all bases contain the OH' group. These points are dealt with fully at a later stage. Freedom of the Ions before Electrolysis The fact that the ions begin to move towards the respective electrodes im- mediately the current is made appears to indicate that they are electrically charged in the solution before electrolysis is com- menced. The questions therefore arise as to the state of such a salt as sodium chloride in dilute solution, and as to what occurs when the circuit is completed. The view long held was that the atoms are united to form a molecule, NaCl, at least ELECTRICAL CONDUCTIVITY 241 partly owing to the electrical attraction of their contrary charges, and that the current pulls them apart during electrolysis. Careful measurements show, however, that Ohm's law holds for electro- lytes, from which it follows that the electrical energy expended in electrolysis is entirely used up in overcoming the resistance of the electrolyte, so that no work is done in pulling apart the components of the molecule. On the basis of this observation, and in agree- ment with certain views previously enunciated by Williamson as to the kinetic nature of equilibrium in general (cf. p. 160), Clausius showed that the equilibrium condition in electrolytes cannot be such that the ions of contrary charge are firmly bound together ; on the contrary, the equilibrium must be of a kinetic nature, so that the ions are continuously exchanging partners, and must, at least momentarily, be present in solution as free ions. The average fraction of the ions free under definite conditions of temperature and dilution was not estimated by Clausius, but he considered that the fraction was probably very small. Clausius's theory accounts for the qualitative phenomena of electrolysis, as during their free intervals the ions would be progressing towards the oppositely charged poles, and would finally reach them and be discharged. The views of Clausius were further developed in 1887 by Arrhenius^who first showed how the fraction of the molecules split up into ions could be deduced from electrical conduc- tivity measurements, and independently from osmotic pressure measurements. This constitutes the main feature of the theory of electrolytic dissociation, which is dealt with in detail later (p. 260), and the fact that the two methods for determining the fraction of the molecules present as free ions gave results in very satisfactory agreement contributed much to the general acceptance of the theory. In a normal solution of sodium chlo- ride, then, there is an equilibrium between free ions and non- ionised molecules, represented by the equation NaCl ^ Na* + Cl', in which, according to Arrhenius, about 70 per cent, of the salt is ionised and the remaining 30 per cent, is present as 1 Zeitsch. physikal. Chetn., 1887, I, 631. 16 242 OUTLINES OF PHYSICAL CHEMISTRY NaCl molecules. According to this theory, the electrical con- ductivity is determi?ied exclusively by the free ions, and not at all by the non-ionised molecules or by the solvent. Dependence of the Conductivity on the Number and Nature of the Ions We are now in a position to form a picture of the mechanism of electrical conductivity in a solu- tion. Suppose there are two parallel electrodes i cm. apart (Fig. 29) with the electrolyte between them, and that the differ- ence of potential between the electrodes is kept constant, say at i volt. Before the electrodes are connected with the battery, the ions are moving about in all directions through the solution. When connection is made in other words, when the electrodes are charged they exert a directive force on the charged ions, which move towards the poles with the contrary charges. Those nearest the poles arrive first, give up their charges to the poles, thus neutralising an equivalent amount of electricity on the latter, and then either appear in the ordinary uncharged form (e.g.) copper), react with the solvent (e.g., SO 4 when platinum electrodes are used), with the electrodes (e.g., SO 4 with copper electrodes), or with each other. It will be seen that the process does not consist in the direct neutralisation of the electricity on the positive electrode by that on the negative electrode, but part of the charge on the anode is neutralised by the anions, whilst an equivalent amount of charge on the cathode is neutralised by the cations a process which has the same ultimate effect as direct neutralisation. On this basis it is clear that with a constant E.M.F. the rate at which the charges on our two plates are neutralised, in other words, the conductivity of the solution between them, depends on three things : (i) the number of carriers or ions per unit volume ; (2) the load or charge which they carry ; (3) the rate at which they move to the electrodes. Each of these factors will now be briefly considered. (i) The Number of Ions Other things being equal, the conductivity of a solution will clearly be proportional to the ELECTRICAL CONDUCTIVITY 243 number of ions per unit volume. For the same electrolyte, the number of ions can, of course, be varied by varying the concentration of the solution. In general, it may be said that on increasing of concentration the ionic concentration also in- creases, but the exact relationship will be dealt with later. For different electrolytes of the same equivalent concentration, the conductivity will depend on the extent to which the solute is split up into its ions and on their speed. (2) The Charge Carried by the Ions As has already been pointed out, there is a simple relationship between the capacity of different ions for transporting electricity, since the gram- equivalent of any ion (positive or negative) conveys 96,540 coulombs. Thus if in an hour ( = 3600 seconds) a gram-equiva- lent of sodium (23 grams) and of chlorine (35*47 grams) are discharged at the respective electrodes, the current which has passed through the cell is ^l5!? = 26-8 amperes. 3600 (3) Migration Velocity of the Ions In this section we will for simplicity consider only univalent ions, but the same considerations apply to all electrolytes. Since positive and negative ions are necessarily discharged in equivalent amount (p. 240), and the number of positive and negative univalent ions discharged in a given time is therefore equal, it might be supposed that the ions must travel at the same rate. This, however, is by no means the case. Our knowledge of this subject is mainly due to Hittorf, who showed that the relative speeds of the ions could be deduced from the changes in concen- tration round the electrodes after electrolysis. The effect of the unequal speeds of the ions on the concen- trations round the poles is made clear by the accompanying scheme (Fig. 30), a modified form of one given by Ostwald. The vertical dark lines represent the anode and cathode respec- tively, and the dotted lines divide the cell into three sections, those in contact with the electrodes being termed the. anode 244 OUTLINES OF PHYSICAL CHEMISTRY and cathode compartments respectively. The positive ions are represented by the usual + sign, and the negative ions by the sign. I. represents the state of affairs in the solution before connection is made ; the number of anions is the same as that of the cations, and the concentration is uniform throughout. The remaining lines represent the state of affairs in the solution after electrolysis on different assumptions as to the relative I. Iff. * '-K +> + + + t + + + f + -!- 4- -1- 4- f 4 + 4- + + + + 4- 4 + 4- 4- ' + -1- -h + 4- -r f + f -f -f + 4- 4- 4- 4- f + + -f f + -f + + + FIG. 30. speeds of the ions. Suppose at first that only the negative ions move. The condition of affairs in the solution when all the negative ions have moved two steps to the left is shown in II. Each ion left without a partner is supposed to be dis- charged, and the figure shows that although the positive ions have not moved an equal number of positive ions is discharged. Further, whilst the concentration in the anode compartment has not altered during the electrolysis, the concentration in the cathode compartment has been reduced by half. Suppose now that the positive and negative ions move at the same rate. The state of affairs when each ion, positive or ELECTRICAL CONDUCTIVITY 245 negative, has moved two steps towards the oppositely-charged pole is represented in III. It is evident that four positive and four negative ions have been discharged, and that the con- centration of undecomposed salt has diminished in both com- partments, and to the same extent, namely by two molecules. Finally, let us assume that both ions move, but at unequal rates, so that the positive ions move faster than the negative ions in the ratio 3:2. The state of affairs when the positive ions have moved three steps to the right, and the negative ions two steps to the left, is shown in IV. It is clear that five positive and five negative ions have been discharged, and that whilst there is a fall of concentration of two molecules round the cathode, there is a fall of three round the anode. These results show that the fall of concentration round any one of the electrodes is proportional to the speed of the ion leaving it. In II., for example, there is a fall of concentration round the cathode, but not round the anode, corresponding with the fact that the anion moves, but not the cation. Similarly, in III., the fall of concentration round anode and cathode is equal, corresponding with the fact that the anion and cation move at the same. Finally, in IV., fall round anode : fall round cathode 1:3:2, corresponding with the fact that speed of cation : speed of anion = 3:2. From these examples we obtain the important rule that Fall of concentration round anode _ speed of cation Fall of concentration round cathode ~~ speed of anion ' The student often finds a difficulty in understanding how, as in IV., five ions can be discharged at the anode when only two anions have crossed the partitions. To account for this, it must be assumed that " there is always an excess of ions in contact with the electrodes, so that more are discharged than actually arrive by diffusion. The speed of the cations is often represented by u, and that of the anions by v. The total quantity of electricity (say, unit 246 OUTLINES OF PHYSICAL CHEMISTRY quantity) carried is proportional to (u + v), and, of this total n vj(u + v) is carried by the anions and i - n = u/(u + v) by the cations, n, the fraction of the current carried by the anion, is termed the transport number of the anion ; similarly, i - n is the transport number of the cation. It is evident from the figure that there is a central section of the cell between the dotted lines in which no change of con- centration* takes place when elec- *f f I "I trolysis is not carried too far. Therefore, in order to investigate the changes in concentration, it is simply necessary to remove the solutions round the electrodes after electrolysis and analyse them, but the experiment will only be successful if the intermediate layer has not altered in strength, Practical Determination of the Relative Migration Velo- cities of the Ions The experi- ment may conveniently be made in the modified form of Hittorf s apparatus used in Ostwald's labo- ratory (Fig. 31). It consists of two glass tubes communicating towards the upper ends ; one of them is closed at the lower end, and the other provided with a stopcock, as shown. The elec- trodes, A and K, are sealed into FIG. 31. glass tubes which pass up through the liquid, and communication with a battery is made in the usual way by means of wires which pass down the interior of the glass tubes. As an illustration, the determination of the transport numbers B ELECTRICAL CONDUCTIVITY 247 of the Ag' and NO 3 ' ions in a ^plution of silver nitrate will be described. The anode A is of silver, and should be covered with finely-divided silver by electrolysis just before the experiment ; the cathode is of copper. The electrodes are placed in position, the anode compartment filled up to the connecting tube with 1/20 normal silver nitrate, the cathode compartment up to B with a concentrated solution of copper nitrate, and finally the apparatus is carefully filled up with the silver nitrate solution in such a way that the boundary between the two solutions at B remains fairly sharp. The cell is then connected in series with a high adjust- able resistance, an ammeter, and a silver voltameter, and then joined to the terminals of a continuous current lighting circuit (no volts) in such a way that the silver pole becomes the anode. By means of the variable resistance, the current is so adjusted that a current of about o'oi ampere is obtained (to be read off on the ammeter), and the electrolysis continued for about two hours. Finally, a measured amount (about 3/4) of the anode solution is run off and titrated with thiocyanate in the usual way. The strength of the current can be read off on the ammeter, and from this and the time during which the current has passed, the total quantity of electricity passed through the solution can be calculated. It is, however, prefer- able to employ for this purpose the silver voltameter above referred to. It consists of a tube with stopcock similar to the left-hand part of the transport apparatus (Fig. 31), and is provided with a silver electrode (to serve as anode) similar to that in the other apparatus, and placed in a corresponding position (in the lower part of the tube). The tube is filled to 3/4 of its length with a 15-20 per cent, solution of sodium or potassium nitrate, and carefully filled up with dilute nitric acid so that the two solutions do not mix. The cathode, of platinum foil, dips in the nitric acid. During electrolysis, the NO 3 ' ions dissolve silver from the anode, and by titrating the whole of the contents with ammonium thiocyanate after the experiment, the amount of silver in solution can be determined, and from this 248 OUTLINES OF PHYSICAL CHEMISTRY the quantity of electricity which has passed through the solution can readily be calculated (p. 238). We now return to the transport apparatus. For our purpose it will be sufficient to deal only with the change of concentra- tion in the anode compartment. From this the transport number of the cation is obtained, and the transport number of the anion is then at once obtained by difference. During electrolysis, the silver concentration round the anode diminishes owing to migration of silver ions towards the cathode. The process may conveniently be illustrated by III. of Fig. 30 where the fall owing to migration is from 4 to 2. At the same time, however, NO 3 ions reach the anode, and after being discharged dissolve silver from it, the silver concentration in the anode compartment therefore increasing. The latter effect is the same as that taking place simultaneously in the silver volta- meter, as described above, and therefore, if no silver migrated from the anode, the total increase of concentration in this com- partment would be equal to that in the silver voltameter, which, as explained above, is a measure of the total quantity of electricity which passes ; we will term this a. If b is the (unknown) change in concentration due to the migration of the silver ions, the observed change in concentration at the anode will be a b. As a is known, and a b is found by titrating the anode solution after the experiment, b can readily be obtained. In practice, the greater part of the anode solution after electrolysis is run into a beaker, it is then weighed or an aliquot part measured, and titrated. The calculation of the results will be rendered clear from the details of an experiment made in Ostwald's laboratory. Before the experiment 12-31 grams of the silver nitrate solution re- quired 26-56 c.c. of a 1/50 n potassium thiocyanate solution, so that i gram of solution contained 0*00739 grams of silver nitrate. After the experiment, 23-38 grams of the anode solution required 69-47 c.c. of the thiocyanate solution, cor- ELECTRICAL CONDUCTIVITY 249 responding to 0*2361 grams of silver nitrate. The solution, therefore, contained 23*14 grams of water, which before the experiment contained 23*14 x 0*00739 = o'lyio grams of silver nitrate, hence the increase of concentration at the anode is 0*065 l grams = a b. The contents of the silver volta- meter required 36*16 c.c. of thiocyanate = 0*1229 grams of silver nitrate = a ; the same amount is dissolved at the anode in the transport apparatus. As the actual increase of con- centration was only 0*0651 grams, 0*1229 - 0*0651 = 0*0578 grams of silver must have left the anode compartment by migra- tion. Hence the transport number for silver is u 0*0578 u + v 0*1229 and for the NO' ion 0*470, n = u + v 0*1229 Hence, of the total current 47 per cent, is carried by the silver ions, and 53 per cant, by the NO 3 ' ions. It was shown by Hittorf that the transport numbers are practically independent of the E.M.F. between the electrodes, but depend to some extent on the concentration and on 'the temperature. It is remarkable that at higher temperatures they tend to become equal. Some of the numbers are given in the next section. Specific, Molecular and Equivalent Conductivity Just as in the case of metallic conduction, the resistance of an electro- lyte is proportional to the length, and inversely proportional to the cross-section of the column between the electrodes. Hence we may define the specific resistance of an electrolyte as the resistance in ohms of a cm. cube, and its specific conductivity as i /specific resistance, expressed in reciprocal ohms. Sines, however, the conductivity does not depend on the solvent but on the solute, it is much more convenient to deal with solutions containing quantities of solute proportional to the respective molecular weights. The so-called molecular conductivity, ^ is 250 OUTLINES OF PHYSICAL CHEMISTRY most largely used in this connection ; it is the conductivity, in reciprocal ohms, of a solution containing i mol of the solute when placed between electrodes exactly i cm. apart. It may also be defined as the specific conductivity, /c, of a solution, multiplied by v, the volume in c.c. which contain a mol of the solute. Hence we have /x- = KV. As an example, the following values for the specific and mole- cular conductivities of solutions of sodium chloride at 18, as given by Kohlrausch, may be quoted. Sp. Con- Molecular Concentration of Solution. ductivity, Conductivity, K. KV, I'o molar (v= 1,000) 0*0744 74-4 0*1 molar (v= 10,000) 0*00925 92-5 o'oi molar (v= 100,000) 0*001028 102*8 o'ooi molar (v= 1,000,000) 0-0001078 107*8 0*0001 molar (v 10,000,000) 0*00001097 I0 9'7 It will be noticed that the molecular conductivity as defined above increases at first with dilution, but beyond a certain point remains practically constant on further dilution. These numbers enable us to illustrate more fully the physical meaning of the molecular conductivity. Imagine a cell of i cm. cross-section and of unlimited height, two opposite walls through- out the whole height acting as electrodes. If a litre of a molar solution of sodium chloride is placed in the cell, it will stand at a height of 1000 cms. We may regard the solution as made up of cm. cubes, 1000 in number, and if the con- ductivity of one of these cubes the specific conductivity is K r the total conductivity (in other words the molecular con- ductivity) is loooKj. If now another litre of water is added, the height of the solution will be 2000 cms. and its molecular con- ductivity is now 2oooK 2 , where * 2 is the specific conductivity of the half-molar solution. In exactly the same way, the mole- cular conductivity may be determined at still greater dilutions. From the above it is clear that a measure of the conducting ELECTRICAL CONDUCTIVITY 251 power of a mol of the electrolyte in different dilutions is ob- tained by multiplying the volume in c.cs. in which the electrolyte is dissolved by its specific conductivity at that dilution, or in symbols JU= KV as given above. A glance at the last two lines in the table helps us to under- stand the approximately constant value of /x in very dilute solutions. When the solution is diluted from i/iooo to 1/10,000 molar, the specific conductivity is reduced to about i/ 10, but as the volume is ten times as great, the molecular conductivity is only slightly altered. Besides the molecular conductivity, the term equivalent con- ductivity, A, is sometimes used. As the name implies, it is the specific conductivity of a solution multiplied by the volume in c.c. which contains a gram-equivalent of the solute. Kohlrausch's Law. Ionic Yelocities The numbers in the third column of the above table show that the molecular rt conductivity of sodium chloride increases, at first rapidly and \|then very slowly, with dilution. This subject was investigated for a number of solutions by Kohlrausch, who found that for solutions of electrolytes of high conductivity (salts, so-called " strong " acids and bases) the molecular conductivity increases with dilution up to about i/ioooo molar solution, and beyond that point remains practically constant on further dilution. Kohlrausch showed further that this limiting value of the mole- cular conductivity, which may be represented by p^, is different for different salts, and may be regarded as the sum of two inde- pendent factors one pertaining to the cation or positive part of the molecule, the other to the anion, or negative part of the molecule. This experimental result is termed Kohlrausch's law, and is readily intelligible on the basis of the theory of electrical conductivity developed above. The limiting value of the mole- cular conductivity is reached when the molecule is completely split up into its ions ; under these circumstances the whole of the salt takes part in conveying the current. For simplicity we will consider solutions of binary electrolytes. In very dilute 252 OUTLINES OF PHYSICAL CHEMISTRY equimolar solutions of different electrolytes, the number of the ions and their charges are the same, and the observed differences of /AOQ can only be due to the different speeds of the ions. The limiting molecular conductivities of binary electrolytes are therefore proportional to the sum of the speeds of the ions, and when the units are properly chosen we have Moc = + where u is the speed of the cation, v that of the anion. This is the mathematical form of Kohlrausch's law, and expresses the very important result that in sufficiently dilute solution the speed of an ion is independent of the other ion present in solution. From the results of conductivity measurements, only the sum of the speeds of the ions can be deduced, but, as has already been shown, the relative values of u and v can be obtained from the results of migration experiments (p. 246). It was found by Kohlrausch that the value of /A^ = u + v for silver nitrate at 18 is 115*5. The accurate value for the transport number of the anion, NO 3 ', is n = vj(u- + v) = 0-518. Hence v 0^518 x 115-5 = 60*8 and u = 0-482 x 115*5 = 557. The values of u and v, expressed in these units, are termed the ionic velocities, under the conditions of the experi- ment. The accompanying table gives the ionic velocities, calculated from the results of conductivity and transport measure- ments, for some of the more common ions in infinite dilution * at 1 8, expressed in the same units as the molecular conductivity of sodium chloride (p. 250): H- = 318 Li- = 36 OH' = 174 K* 65 NH 4 - = 64 Cr = 66 Na- - 45 Ag- =56 T = 67 NCV= 6 1 It is interesting to observe that the velocity of the H* ion is relatively very high, about five times as great as that of any of the metallic ions. The ion which comes next to it is the OH' ion, 1 The more concentrated the solution, the smaller are the ionic velocities, owing to the increased resistance to their motion. ELECTRICAL CONDUCTIVITY 253 the speed of which is more than half that of the H* ion, and much greater than that of any of the other ions. Since the conductivity of a solution is, as we have already seen, propor- tional to the speed of the ions, it follows that the solutions of highly ionised acids and bases will have a relatively high con- ductivity. Thus, under conditions otherwise equal as regards concentration, ionisation, temperature, etc., the conductivities of dilute solutions of hydrochloric acid and of sodium chloride will be in the ratio (318 + 66) = 384 to (45 + 66) = in, or about 3-5:1. Absolute Velocity of the Ions. Internal Friction The absolute velocity of the ions is proportional to the E.M.F. between the electrodes, and inversely proportional to the re- sistance offered to their passage by the solvent. When the fall of potential is one volt per c.m. (i.e., when the difference of potential between the electrodes is x volts and the distance be- tween them is x cm.) it can be shown (p. 414) that the absolute velocities, in cm. per second, are obtainable from the values for the ionic velocities given above by dividing by 96,540 or, what is the same thing, by multiplying by 1*036 x io~ 5 . Hence the absolute velocity of the hydrogen ion is, under the conditions described, 318 x 1-036 x io~ 5 = 0*00332 cm. per second, and of the potassium ion 0-00067 cm - P er second at infinite dilution. The speed of the ions is therefore extremely low ; even the hydrogen ions, under a driving force of i volt per cm., only move about twice as fast as the extremity of the minute hand of an ordinary watch. This very slow motion of the moving particles indicates that the resistance to their passage through the solvent is very great. Kohlrausch has calculated that the force required to drive a gram of sodium ions through a solution at the rate of i cm. per second is 153 x io 6 kilograms weight, or about 150,000 tons weight. The absolute velocity of the ions can also be measured directly by a method the principle of which is due to Lodge, and which may be illustrated by an experiment described by 254 OUTLINES OF PHYSICAL CHEMISTRY Danneel. A U-tube is partly filled with dilute nitric acid, and in the lowest part of the tube a solution of potassium permanganate, the specific gravity of which has been increased as much as possible by the addition of urea, is carefully placed, by means of a pipette, in such a way that the boundary between the acid and the permanganate remains sharp. When platinum electrodes are dipped in the nitric acid in the two limbs, and a current passed through the solution, the violet boundary (due to the coloured MnO 4 ' ion) moves towards the anode. From the observed speed of the boundary and the difference of potential between the poles, the speed of the ion for a fall of potential of i volt/cm, is obtained, and has been found to agree exactly with the value obtained by conductivity and transport measurements. This method is not confined to salts with coloured ions, but the moving boundary can also be observed with colourless solutions when, as is usually the case, the refractive index of the two solutions is different. There are, of course, two boundaries, one due to the positive ions moving towards the cathode, and the other due to the negative ions moving towards the anode. When the conditions are such that both can be observed, the relative speeds give the ratio u/v directly. Measurements of ionic velocities on this principle have been made by Masson, Steele and others, and the results are in entire agreement with those obtained indirectly. Experimental Determination of Conductivity of Elec- trolytes The measurement of the conductivity of conductors of the first class is a very simple operation. Until compara- tively recently, however, no very satisfactory results for the conductivity of electrolytes could be obtained, because when a steady current is passed through a solution between platinum electrodes the products of electrolysis accumulate at the poles and set up a back E.M.F. of uncertain value, a phenomenon known as polarization (p. 373). This difficulty is, however, com- pletely got over by using an alternating instead of a direct ELECTRICAL CONDUCTIVITY 255 current (Kohlrausch, 1880) ; by the rapid reversal of the current the two electrodes are kept in exactly the same condition, and there is no polarization. The arrangement of the apparatus, which in principle amounts to the measurement of resistance by the Wheatstone bridge method, is shown in Fig. 32. R is a resistance box, S a cell with platinum electrodes, between which is the solution the resistance of which is to be measured, ab is a platinum wire of uniform thickness, which may conveniently be a metre long, and is stretched along a board graduated in millimetres, c is a sliding contact. By means of a battery (not shown in the figure) a direct current is sent through a Ruhm- korff coil, K, the latter then gives rise to an alter- nating current, which divides at a into two branches, reach- ing b by the paths adb and acb re- spectively. As a galvanometer is not affected by an alter- nating current, it is in this case replaced by a telephone T, which is silent when the points c and d are at the same potential. The contact-maker, c, is shifted along the wire till the telephone no longer sounds. Under these circumstances, the following relationship holds Length of ac Length of cb FIG. 32. and since ac, cb and R are known, S, the resistance of the part of the electrolyte between the electrodes, can ?t once be calculated. As the resistance of electrolytes varies within wide limits, 256 OUTLINES OF PHYSICAL CHEMISTRY different forms of cell are employed according to circum- stances. For solutions of small conductivity, the Arrhenius form represented in Fig. 33. is very suitable. The electrodes, which are stout platinum discs 2-4 cm. in diameter, are fixed (by welding or otherwise) to platinum wires, which are sealed into glass tubes A and B, as shown in the figure. These glass tubes are fixed firmly into the ebonite cover of the cell, so that the distance between the electrodes remains constant, and electri- cal connection is made in the usual way by wires passing down the interior of the glass tubes. In order to expose a larger surface, FIG. 33. FIG. 34. and thus minimise polarization effects, which would interfere with the sharpness of the minimum in the telephone, the elec- trodes are coated with finely-divided platinum by electrolysis of a solution of chlorplatinic acid. For electrolytes of high conductivity, a modified form of conductivity vessel, with smaller electrodes placed further apart, has been found con- venient (Fig. 34). Experimental Determination of Molecular Conduc- tivity It is clear that the observed resistance of the electro- lyte must depend on what is usually termed the capacity of the ELECTRICAL CONDUCTIVITY 257 cell, that is, on the cross-section of the electrodes and the distance between them. The specific conductivity, and hence the specific resistance, of the electrolyte could be calculated if these two magnitudes were known (p. 235); but it is much simpler to determine the " constant " of the vessel, which is proportional to its capacity, by using an electrolyte of known conductivity. For this purpose, a 1/50 molar solution of potas- sium chloride may conveniently be used for cells of the first type. The method of procedure will be clear from an example, Referring to the figure, we have, for the resistance, S, of the electrolytic cell R'fo , i ac b = - and conductivity (^ = - = =-. ac S R'&r Further, since the specific conductivity, *, must be proportional to the observed conductivity, we have A/^ ac = where A is a constant. Since all the other factors, including *, the specific conductivity of potassium chloride, are known, A, the constant of the cell, can be calculated. If, now, with the same distance between the electrodes, a solution of unknown specific conductivity, K lt is put in the cell, and for the resistance R' the new position of the contact is c, the specific conductiv- ity in question is given by the formula ac *' = A RW' By multiplying /^ by the number of c.c. containing i mol of the solute, the molecular conductivity is obtained. An alternative method of calculating KJ without reference to the cell constant is as follows. If S and S x represent the resist- ances of the cell containing N/5oKCl and the solution of specific conductivity K-^ respectively, then KS 258 OUTLINES OF PHYSICAL CHEMISTRY From the results of conductivity measurements in different dilutions, ya^ can readily be obtained directly for salts, strong acids and bases ; it is the value to which /x, approximates on progressive dilution. /x^ cannot, however, be obtained directly for weak electrolytes, such as acetic acid and ammonia ; before the limiting value of the conductivity is reached with these electrolytes, the solutions would be so dilute as to render accu- rate measurement of the specific conductivity impossible. This difficulty is got over by making use of Kohlrausch's law. The value of /X-OQ for acetic acid must be the sum of the velocities of the H* and CH 3 COO' ions. The former is obtained from the results of conductivity and transport measurements with any strong acid, and has the value 318 at 18. In a similar way the velocity of the CH 3 COO' ion can be obtained from ob- servations with an acetate for which the value of /^ can con- veniently be found, e.g., sodium acetate, /x^ for the latter salt at 18 is 78-1, and as the velocity of the Na* ion is 44*4 at infinite dilution, that of the CH 3 COO' ion must be 78-1 -44*4 = 33*7. Hence for acetic acid /AGO = + v = 337 + 318 = 351-7 at 1 8. Results of Conductivity Measurements In general, it may be said that the conductivity of pure liquids is small. Thus the specific conductivity of fairly pure distilled water is about io~ 6 reciprocal ohms at 18, and even this small con- ductivity is largely due to traces of impurities. It is a remark- able fact that the specific conductivity of a number of other liquids, which have been purified very carefully by Walden, 1 is of the same order as that given above for water. Mixtures of two liquids have in many cases a very small conductivity, not appreciably greater than that of the pure liquids themselves ; this is true of mixtures of glycerine and water, and of alcohol and water. On the other hand, a mixture of two liquids which are practically non-conductors may have a very high conductivity for example, mixtures of sulphuric acid and water. The results obtained for this 1 Zeitsch. Physikal Chern., 1903, 46, 103. ELECTRICAL CONDUCTIVITY 259 ture are represented in Fig. 35, the acid concentration being measured along the horizontal axis, and the specific conductivity along the vertical axis. The figure shows that, on gradually adding sulphuric acid to water, the specific conductivity of the mixture increases till 30 per cent, of acid is present, reaches a maximum value at that point, and on further addition of acid diminishes. When pure sulphuric acid is present (100 per' cent, on curve), the conductivity is practically zero, and is increased 07 0-6 0-5 0-4 r-e/ 0-3 H 2 SO \ Concentration 40 50 60 FIG. 35. 70 80 90 TOO per cent. both by the addition of water (left-hand part of curve) and of sulphur trioxide (right-hand part of curve). Further, the curve has a minimum between 84 and 85 per cent, of acid, which, it is interesting to note, exactly corresponds with the composition of the monohydrate H 2 SO 4 , H 2 O. According to the electro- lytic dissociation theory, the conductivity depends on the pres- ence of free ions, and the curve for sulphuric acid and water shows in a very striking way that the condition most favourable for ionisation is the presence of two substances. Why ions are formed in a mixture of sulphuric acid and water, and not appreciably, if at all, in a mixture of alcohol and water, is not well understood (cf. p. 317). Analogous phenomena are met with for solutions of solids 260 OUTLINES OF PHYSICAL CHEMISTRY and of other liquids in liquids. An aqueous solution of sugar has no appreciable conducting power. The so-called " strong " acids and bases form well-conducting liquids with water. The conductivity of most organic acids and bases is small, and in corresponding dilution ammonium hydroxide is a much poorer conductor than potassium hydroxide. On the other hand, all salts, even the salts of organic acids which are themselves weak, have a very high conductivity. The conductivity of substances in solvents other than water is usually small, but solutions in methyl and ethyl alcohols and in liquid ammonia are exceptions. The dependence of electrical conductivity on the nature of the solvent will be discussed later It is interesting to note that many fused salts, such as silver nitrate and lithium chloride, are good conductors, and thus form an exception to the rule that pure substances belonging to the second class of conductors have a very small conductivity. Electrolytic Dissociation It has already been pointed out (p. 124) that solutions of salts, strong acids and bases, have a much higher osmotic pressure in aqueous solution than would be the case if Avogadro's hypothesis was valid for these solu- tions. According to the molecular theory, the solutions behave as if there were more particles of solute present than would be anticipated from the simple molecular formula, and van't Hoff expressed this by a factor /, which represented the ratio between the observed and calculated osmotic pressures. This was the position of the theory of solution in 1885. About that time, Arrhenius pointed out that there is a close connection between electrical conductivity and abnormally high osmotic pressures ; only those solutions which, according to van't Hoff 's theory, have abnormally high osmotic pressures, conduct the electric current. Kohlrausch had previously shown that the molecular conductivity increases at first with dilution, and for many electrolytes attains a limiting value in a dilution of 10,000 litres (p. 251). Arrhenius accounted for this increase on the assumption that the solute consists of "active" and ELECTRICAL CONDUCTIVITY 261 " inactive " parts, and that only the active parts, the ions, convey the current. The extent to which the solute is split up into ions increases with the dilution until finally (when the molecular conductivity has attained its maximum value) it is completely ionised or completely " active " as far as the conduction of electricity is concerned. The theory of Arrhenius is based upon the views of Clausius on conductivity, as has already been pointed out. Arrhenius, however, went much further, inasmuch as he showed how, from the results of conductivity and of osmotic pressure measure- ments, the degree of dissociation can be calculated, as shown in the following section. Degree of lonisation from Conductivity and Osmotic Pressure Measurements According to the theory of electro- lytic dissociation, the conductivity of a solution depends only on the number of the ions per unit volume, on their charges (which are the same for equivalent amounts of different electrolytes) and on their speed. For the same electrolyte we may assume that the velocities remain practically unaltered on dilution (the friction in a dilute solution being practically the same as that in pure water), therefore the increase of molecular conductivity with dilution must depend almost entirely on an increase in the number of the ions. The molecular conductivity at infinite dilution is given by the formula where u and v are the speeds of cation an d anion respectively and the molecular conductivity at any dilution, v , must therefore be represented by the formula p v = a(u + v), where a represents the fraction of the molecules split up into ions. Hence, dividing the second equation by the first, we have 262 OUTLINES OF PHYSICAL CHEMISTRY that is, the degree of dissociation, a, at any dilution, is the ratio of the molecular conductivity at that dilution to the mole- cular conductivity at infinite dilution. For example, p v for molar sodium chloride is 74-3 and /x,^ = 110-3, hence a = /A X ,//* oc = 74'3/iio'3 = 0*673. Hence sodium chloride in molar solution is about two-thirds split up into its ions. We have now to consider the deduction of the degree of dissociation from osmotic measurements. The assumption made in this case is that the osmotic pressure is proportional to the number of particles present, the ions acting as separate entities. If a molecule is partially dissociated into n ions and the degree of dissociation the ionised fraction is a, then the number of molecules will be i a, and the number of ions na. Hence the ratio of the number of particles actually present to that deduced according to Avogadro's hypothesis (van't Hoffs factor i) will be I = I a + a = I + o.(n - i), i I or a n i As an illustration, de Vries obtained for a 0^14 molar solution of potassium chloride /= 1*81, hence, since n = 2, a = o'8i, or the salt is dissociated to the extent of 81 per cent, into its ions, /for a 0-18 molar solution of calcium nitrate is 2-48, therefore, since = 3, a = - - = 074 in this case. The agreement in the values of / obtained from conductivity and osmotic measurements is strikingly shown in the accom- panying table (van't Hoff and Reicher, 1889). The values of i (osmotic) are from the results of de Vries, those of / (freezing point) mainly from the observations of Arrhenius, and those of i (conductivity) are calculated by means of the formulae a = /AV//XQC and / = i + a(n - i) as explained above. It is not certain that the results obtained by the different methods can be expected to agree absolutely (cf. p. 281). ELECTRICAL CONDUCTIVITY 263 Concentration . (freezi . f (conduc- Substance. (gram equiv. ^ .. * (osmotic). t i v i ty ). per litre). KC1 0*14 1-82 1*81 r86 LiCl 0-13 1-94 1-92 1-84 Ca(N0 3 ) 2 0-18 2-47 2*48 2*46 MgCl 2 0*19 2-68 279 2-48 CaCL 0-184 2-67 2-78 2-42 As regards the mode of ionisation, it is clear that univalent compounds, such as potassium chloride, can ionise only in one way, thus, KC1;K* + Cl'. For more complex molecules, how- ever, there are other possibilities, thus calcium chloride may ionise as follows : CaCl 2 ^ CaCl* + Cl' as well as in the normal way CaClg^tCa" + 2C1'. If ionisation were complete according to the last equation, / would be = 3, as compared with the observed value, 2-67 for 0*184 normal solution, given in the table. Similarly, sulphuric acid may dissociate according to the equation H 2 SO 4 ^H* + HSO/, the latter ion then under- going further ionisation as follows : HSO 4 'JH* + SO 4 ". Effect of Temperature on Conductivity The conduc- tivity of electrolytes increases considerably with rise of tempera- ture. The temperature coefficient for salts is 0*020 to 0*023, for acids and some acid salts 0*009 to 0*016, for caustic alkalis about 0*020, and does not vary much with dilution. Conduc- tivity data are usually given for 18, and the specific conductivity, K, at any other temperature, is given by the formula K t = K lg [l + C(t - 1 8)] where c is the temperature coefficient. As the conductivity of an electrolyte depends both on the number and velocity of the ions, the question arises as to whether the change of conductivity with temperature is due to the alteration of only one or of both these factors. The matter can be at once decided by calculating the degree of dissociation at the higher temperature from conductivity measurements in the ordinary way, and comparing with that at the lower temperature. For normal sodium chloride at 50, the value of a = /*//*< = 132/203*5 = 0*65, which is 264 OUTLINES OF PHYSICAL CHEMISTRY only slightly less than the value at 18, 0*678. Hence, as the considerable increase of conductivity with temperature cannot be due to an increase in the number of ions, it must be due to an increase in their speed. This increased velocity is doubt- less connected with the diminution in the internal friction of the medium with rise of temperature, and the consequent diminished resistance to the passage of the ions (p. 253). Basicity of Acids from Conductivity Measurements (Empirical) The conductivity of N/32 and N/I024 solutions (equivalent normal) of the sodium salt of the acid is deter- mined. For monobasic acids the difference A 102 4 - A 32 is about 10, for dibasic acids about 20, and so on (Ostwald). Grotthus' Hypothesis of Electrolytic Conductivity- Long before the establishment of the electrolytic dissociation theory, Grotthus put forward a hypothesis to account for the conductivity of electrolytes which is of considerable historical interest. He assumed that under the influence of the charged electrodes the molecules of the salt, e.g., potassium chloride, arrange themselves in lines between the electrodes so that the potassium atoms are all turned to the negative electrode, and the chlorine atoms to the positive electrode. Electrolysis takes place in such a way that the external potassium atom is liberated at the cathode and the chlorine atom at the anode. The potassium atom which is left free at the anode unites with the chlorine atom of the molecule next to it, the chlorine atom of the latter with a potassium atom of the molecule next in the chain, and so on. A similar process takes place starting at the anode, in other words, an exchange of partners takes place right along the chain, from one electrode to the other. Under the influence of the charged electrodes, the new molecules twist round till they are in the former relative position, when the end atoms are again discharged, and so electrolysis proceeds. The fatal objection to this ingenious theory is that a con- siderable E.M.F. would have to be employed before any decomposition whatever takes place, hence Ohm's law would not hold (cf. p. 241). Practical Illustrations The following experiments, which ELECTRICAL CONDUCTIVITY 265 are fully described in the course of the chapter, may readily be performed by the student : (1) Experiment on the migration velocity of the ions (p. 246). (2) Rough determination of the absolute velocity of the MnO 4 ' ion (p. 254). (3) Determination of the constant of conductivity vessel with n /5 potassium chloride. (The specific conductivity, K, of this solution at different temperatures is as follows : 0-001522 at o, 001996 at 10, 0-002399 at 18, and 0-002768 at 25.) (4) Determination of the specific and molecular conductivities of solutions of sodium chloride and of succinic acid. As the conductivity of solutions varies greatly with the tem- perature, the conductivity vessel must be partially immersed in a thermostat while measurements are being made. In the case of sodium chloride, measurements may be made with n/i t n/io and n/ioo solutions, and the values obtained for the molecular conductivity compared with those given in Kohlrausch's tables. 1 The results in very dilute solutions are not trustworthy unless great attention is paid to the purification of the water used in making up the solutions. * In the case of succinic acid, it is usual to start with a 1/16 Mwlar solution; 20 c.c. of this solution is placed in the con- ductivity cell in the thermostat, and when the temperature is constant the resistance is determined. 10 c.c. of the solution is then removed with a pipette, 10 c.c. of water at the same temperature added, the resistance again determined after thoroughly mixing the solution, and so*on. Measurements are thus made in dilutions of 16, 32, 64, 128, 256, 512 and 1024 litres. From the values of /* thus obtained, the degree of dissociation can be calculated by the usual formula a = pJn^ . /XOQ in this case can only be determined indirectly ; its value at 25 is about 381. From the values of a in different dilutions, K, the dissociation constant of the acid may then be calculated ; according to Ostwald, K = 0*000066 at 25. 1 Full details of electrical conductivity measurements and a large amount of conductivity data are given by Kohlrausch and Holborn, Leilvermogen der Elektrolyte, Leipzig, 1898. CHAPTER XI EQUILIBRIUM IN ELECTROLYTES. STRENGTH OF ACIDS AND BASES. HYDROLYSIS The Dilution Law In a previous chapter it has been shown that chemical equilibria, both in gaseous and liquid systems, can be represented satisfactorily by means of the law of mass action. We have now to apply this law to binary electrolytes, on the assumption that the ions are to be re- garded as independent entities. According to the electrolytic dissociation theory, an aqueous solution ot acetic acid contains molecules of non-ionised acid in equilibrium with its ions, represented by the equation CH 3 COO' + H-^CH 3 COOH. Suppose in the volume v of solution the total concentration of the acid is i, and that a fraction of it, represented by a, is split up into ions. The concentration of the undissociated acid is , that of each of the ions (since they are neces- sarily present in equivalent amount) -. Hence, from the law of mass action, 2 /i - a\ a 2 , \ = K( - ) or 7 r- = K . . (i) \ V ) (i - a)v where K, as before, is the equilibrium constant. For conduc- tivity measurements, the above formula may be put in a rather different form by substituting pvlpvz for a. It then becomes 266 EQUILIBRIUM IN ELECTROLYTES 267 It is preferable, however, to remember the dilution formula in the first form, or in the form a?cl(i - a) = K. This relationship, which is known as Ostwald's dilution law, may be tested by substituting a value for a (from conductivity or osmotic observations) at any dilution v, and calculating K, the equilibrium constant ; the value of a at any other- dilution may then be obtained from the formula and compared with that determined directly. This was done (from conductivity measurements) by van't Hoff and Reicher, and the results are given in the accompanying table : Acetic acid: K = 0-0000178 at 14*1; /A^, = 316. v (in litres) , . 0-994 2-02 15*9 i8'i 1500 3010 7480 15000 A*. 1*27 i'94 5'26 5*63 46-6 64-8 95-1 129 rooa (observed) . 0*40 0-614 I66 1 '7 8 *4*7 20-5 30-1 40-8 looo (calculated) . 0-42 0-6 1-67 178 15-0 20-2 30-5 40-1 The agreement between observed and calculated values is excellent ; it is, in fact, much closer than for any case of ordinary dissociation so far investigated. The table also shows how small is the dissociation of acetic acid solutions under ordinary conditions ; a molar solution is ionised only to the extent of 0*4 per cent, and even a 1/1500 molar solution rather less than 15 per cent. The dilution law holds for nearly all organic acids and bases, but does not hold for salts, or for certain mineral acids and bases. The latter point is discussed in a later section. When the deg ree of dissociation is small, as in the case of acetic acid for fairly concentrated solution, a can be neglected in comparison with i, and the dilution law then becomes 2 = K or a = xKz . . . ( 2 ) that is, for weak electrolytes the degree of dissociation is approxi- mately proportional to the square root of the dilution. When 268 OUTLINES OF PHYSICAL CHEMISTRY a cannot be neglected in comparison with i, a is given by the equation (3) obtained by solving equation (i) for a. In order to familiarise himself with the use of the dilution formula, the student should calculate a for acetic acid in different dilutions from the value of K given above both by the approximate and accurate formula. The physical meaning of the constant K will be clear if a in the dilution formula (i) is put = -J. Then 2K = i/z>, that is, 2K is the reciprocal of the volume at which the electrolyte is dissociated to the extent of 50 per cent. Acetic acid, for instance, will be half dissociated at a dilution of - o* = 2 7>777 ntres (ff- table). 2 x 0-000018 As the method of deriving it indicates, the dilution law applies only to binary electrolytes, i.e., electrolytes which split up into two ions only, and it is not therefore a priori probable that it will hold for dibasic acids, such as succinic acid, which presumably dissociate according to the equation C 2 H 4 (COOH) 2 ^C 2 H 4 (COO) 2 " + 2 H-. It is, however, an experimental fact that when the concentration of succinic acid is expressed in mols (not in equivalents) per litre, the values of K obtained by substitution in the dilution formula remain constant through a wide range of dilution. This indicates that the acid at first splits up into two ions only, doubtless according to the equation /COO' . 4 H and that the second possible stage, represented by the equation /COO' - CH / COO "+H- <-^ 2 4 \COO 1 EQUILIBRIUM IN ELECTROLYTES 269 is hot appreciable under the conditions of the experiment. In other cases, however, e.g., fumaric acid, the value of K increases with dilution before the dilution has progressed very far, which indicates that the second stage of the dissociation early becomes of importance. Strength of Acids We are accustomed to estimate the strength of acids in a roughly qualitative way by their relative displacing power. Sulphuric acid, for example, is usually re- garded as a strong acid, because it can displace such acids as acetic and hydrocyanic from combination. This principle can be developed to a quantitative method for estimating the rela- tive strengths of acids (and bases) if care is taken to make the comparison under proper conditions. This is sufficiently secured by making the experiments in a homogeneous system under such conditions that all the reacting substances and products of reaction remain in the system. We learn in studying inorganic chemistry that many reactions proceed wholly or partially in a particular direction for two main reasons : (a) because an insoluble (or practically insoluble) product is formed which is thus removed from the reacting system, e.g., Na 2 SO 4 + BaCl 2 -> 2NaCl + BaSO 4 (insoluble) ; (b] because a volatile product is formed which under the con- ditions of experiment leaves the reacting system, e.g., 2NaCl + H 2 SO 4 - Na 2 SO 4 + 2 HC1 (volatile). Such reactions are obviously unsuitable for determining the relative strengths of the acids concerned. Bearing these considerations in mind, we now proceed to investigate the relative strengths of, say, nitric and dichloracetic acids by bringing them in contact with an amount of base insuffi- cient to saturate both of them, and find how the base distri- butes itself between the two acids. If, for example, the acids are taken in equivalent amount, and sufficient base is taken to saturate one of them, we have to determine the position of equilibrium represented by the equation 270 OUTLINES OF PHYSICAL CHEMISTRY CHCl a COOK + HN0 3 ^CHC1 2 COOH + KNO 3 . It is evident that no chemical method would answer the purpose, because it would disturb the equilibrium. When, however, a physical property of one of the components, which alters with the concentration, can be measured, the position of equilibrium can be determined. A method used for this purpose by Ostwald, depending on the changes of volume on neutralization, will be readily understood from an example. When a mol of potassium hydroxide is neutralized by nitric acid in dilute solution, there is an increase of volume of about 20 c.c. When, on the other hand, the same quantity of alkali is neutralized by dichloracetic acid, the increase of volume is about 13 c.c. It is therefore clear that the complete displace- ment of dichloracetic acid by nitric acid, according to the equation CHC1 2 COOK + HNO 3 -CHC1 2 COOH + KNO 3 / would give an increase of volume of (20 - 13) = 7 c.c. ; if no displacement took place, there would, of course, be no change of volume. The change actually observed was 5*67 c.c., which means that the reaction represented by the equation has gone from left to right to the extent of - - = 80 per cent, approxi- 7-0 mately; in other words, the nitric acid has taken 80 per cent, of the base, and 20 per cent, has remained combined with the dichloracetic acid. The relative strength, or relative activity, of the acids under these conditions is therefore 80 : 20 or 4 : i. Any other physical property, which is capable of quantitative measurement and differs from the two systems, can be equally well employed for the determination of equilibrium. The heat of neutralization has been used for this purpose by Thomsen, and the measurement of the refractive index by Ostwald ; the principle of the methods is exactly the same as in the example just given. Thomsen's therm ochemical measurements were the first to EQUILIBRIUM IN ELECTROLYTES 271 be made on this subject, and he arranged the different acids in the order of their " avidities " or activities. Ostwald then showed that the same order of the avidities was obtained by the volume and refractivity methods, and, further, that the results were independent of the nature of the base competed for, so that the avidities are specific properties of the acids. The relative strength of acids can also be determined on an entirely different principle, depending on kinetic measurements. It has already been pointed out that acids accelerate, in a catalytic manner, the hydrolysis of cane sugar, of methyl acetate, acetamide, etc. Ostwald made many experiments on this sub- ject and reached the very important conclusion that the order of the activity of acids is the same, whether measured by the distribution method (which is, of course, a static method), or by a kinetic method. This affords further evidence in favour of the conclusion just mentioned, that the activity or affinity is a specific property of the particular acid, independent of the method by which it is measured. Thus far had our knowledge of the subject progressed when in 1884 the first paper of Arrhenius appeared. He showed that the order of the "strengths" of the acids as determined by the methods just described is also that of their electrical conductivities in equivalent solution. This fundamentally im- portant fact is illustrated in the accompanying table, in which the conductivities of the acids in normal solution are quoted, that of hydrochloric acid being taken as unity. Relative Activity. Acid. Thermochemical. Cane Sugar. Conductivity. Hydrochloric 100 100 100 Nitric 100 100 99-6 Sulphuric 49 53-6 65-1 Monochloracetic 9 4-8 4-9 Acetic 0-4 1-4 We have seen that, according to the electric dissociation theory, the electrical conductivity of an acid is mainly deter- 272 OUTLINES OF PHYSICAL CHEMISTRY mined by its degree of dissociation; for example, the con- ductivity of a normal solution of acetic acid is small because it is ionised only to a very small extent. Further, owing to the predominant share taken by the hydrogen ions in conveying the current (p. 252), the relative conductivities of acids will be approximately proportional to their H' ion concentrations. It is therefore natural to suppose that the activity of acids, as illustrated by distribution and catalytic effects, is also due to that which all acids have in common, namely, hydrogen ions, This assumption is in complete accord with the experimental results, as the following illustration shows. The velocity con- stant for the hydrolysis of cane sugar in the presence of 1/80 normal hydrochloric acid is 0-00469 at 54-3 (time in minutes) ; as the acid may be regarded as completely dissociated CH- = 0-0125. CH- for 1/4 normal acetic acid (# = 4, cf. p. 267) may be calculated from the dilution formula or directly from the equilibrium equation as follows : [H-][CH 3 COO'] [H-] 2 [H-] 2 [CH 3 COOH] [CH 3 COOH] [0-25 - H-]" whence CH- = 0-002. On the assumption that the catalytic effect of acids is propor- tional to the H* ion concentration, the value of the velocity constant, x, for the hydrolysis of cane sugar by 0-25 normal acetic acid at 54*3 should be 0-0125 : 0*00469 : : 0-002 : x, whence x = 0-00075. This is identical with the result obtained experimentally by Arrhenius, and we have here a very striking confirmation of the electrolytic dissociation theory. From the above considerations, we conclude that the charac- teristic properties which acids have in common, such as sour taste, action on litmus, catalytic activity, property of neutralizing bases, etc., are due to the presence of H- ions. It must be remembered that direct proportionality between H- ion .concen- tration and conductivity is neither observed nor to be expected EQUILIBRIUM IN ELECTROLYTES 273 from the theory ; the approximate proportionality is due to the great velocity of the hydrogen ions, and would be altogether absent if the anions were the more rapid. As there is a simple relationship between the H> ion con- centration of weak acids and their dissociation constants (p. 267), it is clear that the behaviour of an acid can be to a great extent foretold when its dissociation constant has been measured. Such determinations have been made for a great number of weak acids by Ostwald and others, and some of the results are given in the accompanying table,. which shows very clearly how greatly the value of K differs for different acids, and the influence of substitution : Acid. Acetic H-CH 3 COO Monochloracetic H CH 2 C1COO Trichloracetic H C1 3 COO Cyanacetic H CH 2 CNCOO Formic H HCOO Carbonic H HCO 3 Hydrogen sulphide H SH Hydro yanic H CN Phenol H OC 8 H 5 Value of K at 25 (v in litres). 0-000018 = 180,000 x io~ 10 3040 x io- 10 570 x io- 10 13 x io~ 10 i '3 x io~ 16 1*21 0-0037 0*000214 For a weak acid, a= >jKv, where a is the degree of dis- sociation at the volume v. Hence, for two acids at the same dilution a/a' = \/K/K', or the ratio of the degrees of dissocia- tion is equal to the square root of the ratio of the dissociation constants. From the data given in the table it can readily be calculated that in solutions of monoch loracetic and acetic acid of the same concentration the ratio of the H- ion concentrations is approximately 9-3 : i. The effect of replacing one of the hydrogens in acetic acid by chlorine is thus to form a much stronger acid and the CN group has a still greater effect, as the table shows. A further important point is the effect of dilution on the "strength" of an acid. As the degree of dissociation in- creases regularly with dilution, it is evident that the activity of a weak acid will approach nearer and nearer to that of a strong 18 274 OUTLINES OF PHYSICAL CHEMISTRY acid (which is completely active in moderate dilution) until finally, when the weak acid is completely ionised, it will have the same strength as the strong acid in equivalent dilution. It follows that the strength of acids is the more nearly equal the more dilute the solution, and that at " infinite dilution " all acids are equally strong. It can readily be calculated from the conductivity tables that the relative strengths of hydrochloric and acetic acids in different dilutions are as follows : Concentration n/i n/io H/IOO w/iooo n/io,ooo a for HC1 0*81 0-91 0-97 0-99 i-o a for HC 2 H 3 O 2 0-004 0-013 0-04 0*13 0-4 Ratio HC1/HC 2 H 3 O 2 200 70 24 7-5 2-5 Strength of Bases Just as the strength of acids depends on their concentration in hydrogen ions, so the strength of bases depends on the concentration in hydroxyl ions. On this view, potassium hydroxide is a strong base, because in moderate dilution it is almost completely ionised according to the equa- tion KOH 1^ K* + OH' ; ammonium hydroxide, on the other hand, is a weak base, because its aqueous solution contains only a relatively small concentration of OH' ions. Since certain organic compounds, including amines and alkaloids, have basic properties, their aqueous solutions must also contain OH' ions. Thus, solutions of pyridine, C 5 H 5 N, contain not only the free base, but a certain concentration of C 5 H 6 N' and OH' ions, in equilibrium with the undissociated hydrate, as represented by the equation C 5 H 6 NOH;C 5 H 6 N- + OH'. The strength of bases may be determined by distribution or catalytic methods, corresponding with those already described for determining the strength of acids, as well as by conductivity methods. A fairly satisfactory catalytic method is the effect on the rate of condensation of acetone to diacetonyl alcohol, 1 represented by the equation 2CH 3 COCH 3 -> CH 3 COCH 2 C(CH 3 ) 2 OH. 1 Koelichen, Zeitsch. Physikal.Chem., 1900, 33, 129. EQUILIBRIUM IN ELECTROLYTES 275 The order of the strength of bases as determined by this method agrees with the results of conductivity measurements. Another method, which is not purely catalytic, since the base is used up in the process, is the effect on the hydrolysis or saponification of esters (p. 207). This process is usually represented by the typical equation CH 3 COOC 2 H 5 + KOH = CH 3 COOK + C 2 H 5 OH. Experience shows, however, that for the so-called strong bases, which are almost completely ionized in moderate dilution, the rate of hydrolysis is practically independent of the nature of the cation (whether K, Na, Li, etc.), a fact which is readily accounted for on the view that the ions exist free in solution, as the ionic theory postulates, and that the OH' ions are alone active in saponification. The general equation for the hy- drolysis of ethyl acetate by bases may, therefore, be written as follows CH 3 COOC 2 H 5 -i- OH' = CH 3 COO' + C 2 H 5 OH. The relative strength of bases, as obtained from their efficiency in saponifying esters, is in excellent agreement with their strength as deduced from conductivity measurements. The ionization view of the saponification of esters is further sup- ported by the fact that the reaction between ethyl acetate and barium hydroxide is bimolecular and not trimolecular, as would be anticipated if it proceeded according to the equation 2CH 3 COOC 2 H 5 + Ba(OH) 2 = (CH 3 COO) 2 Ba + 2 C 2 H 5 OH. The alkali and alkaline earth hydroxides are very strong bases, being ionized to about the same extent as hydrochloric acid in equivalent dilution. Bases differ as greatly in strength as do acids; the dissociation constants for a few of the more important are given in the table. Base. Ammonia NH 4 'OH Methylamine CH 3 NH 3 'OH Trimethylamme (CH 3 ) 3 NH-OH Pyridine C 5 H 6 N-OH Aniline C 6 H 5 NH 3 -OH Value of K (25) (v in litres) 0*000023 = 230,000 x 10 0*00050 0*000074 23 x io~ 10 4*6 x io~ 10 -10 276 OUTLINES OF PHYSICAL CHEMISTRY Interesting results have been obtained as to the effect of sub- stitution on the strength of bases. Thus the table shows that the basic character is increased by replacing one of the hydrogen atoms in ammonia by the CH 3 group, but is greatly diminished by the C 6 H 5 group. Mixture of two Electrolytes with a Common Ion The dissociation of weak acids and bases is greatly diminished by the addition of a salt with an ion common to the acid or base. For example, the equilibrium in a solution of acetic acid is re* presented by. the equation [H-] [CH 3 COO'] = K [CH 3 COOH], and if by adding sodium acetate the CH 3 COO' ion con- centration is greatly increased, the H* ion concentration must correspondingly diminish, since the concentration of the undis- sociated acid cannot be greatly altered (nearly the whole of the acid being present in that form in the original solution) and therefore the right-hand side of the equation is practically constant. The exact equations representing the mutual influence of electrolytes with a common ion are somewhat complicated, but an approximate formula which is often useful can be obtained as follows : If the total concentration of a binary electrolyte is c and its degree of dissociation is a, we have, from the law of mass action, ^W K. ':. (i) (l -a)c If now an electrolyte with a common ion is added, and the concentration of the latter is c ot the above equation becomes (a!c}(a'c + c ) _ K ,. (l - a> This equation is quite accurate. As K, c and c are known, a', where a is the new degree of dissociation, can be calculated, perhaps most readily by successive approximations. If the degree of dissociation of the first electrolyte is small, i - of can be taken as unity without appreciable error ; further, EQUILIBRIUM IN ELECTROLYTES 277 if the second electrolyte is highly ionised and is added in con- siderable proportion, aV can be neglected in comparison with c ot an d equation (2) simplifies to (aV) C = K, . . . . (3) Otherwise expressed, the concentration of one of the ions of a weak electrolyte is inversely proportional to the ionic concentra- tion of a highly-dissociated salt having an ion in common with the other ion of the weak electrolyte. As an illustration of the application of the last equation, we will consider the effect of the addition of an equivalent amount of sodium acetate on the strength of 0*25 molar acetic acid. In this dilution a for the acid is 0-0085 and ac = 0*0085 x 0*25 = 0-0021 = C H \ In 0*25. molar solution, sodium acetate is dissociated to the extent of 69-2 per cent., hence c = 0*25 x 0*692 = o'i73. We have, therefore, a' x 0*173 0*000018, whence a' = 0*0001. aV is therefore 0*25 x 0*0001 =0*000025= C n . in presence of 0*25 molar sodium acetate, so that the strength of the acid is diminished in the ratio 85 : i. In an exactly similar way, the strength of ammonia as a base is greatly reduced by the addi- tion of ammonium salts. This action of neutral salts on weak bases and acids is largely taken advantage of in analytical chemistry. For example, the concentration of OH' ions in ammonia solution is sufficient to precipitate magnesium hydroxide from solutions of magnesium salts, but in the presence of ammonium chloride the OH' ion concentration is so greatly reduced that precipitation no longer occurs. Similarly, the addition of hydrochloric acid diminishes the concentration of S" ions in hydrogen sulphide to such an extent that zinc salts are no longer precipitated (cf. p. 300). Isohydric Solutions It is of particular interest to inquire what must be the relation between two solutions with a common ion two ^acids, for example in order that, when mixed, they may exert no mutual influence. This problem was investigated 278 OUTLINES OF PHYSICAL CHEMISTRY both theoretically and practically by Arrhenius, who showed (cf. p. 414) that no alteration in the degree of dissociation of either of the salts (acids or bases) takes place when the con- centration of the common ion in the two solutions before mixing is the same. Such solutions are termed isohydric. The relative dilutions in which two acids or other electrolytes with a common ion are isohydric can readily be calculated from their dissociation constants. The value of K for acetic acid is o-ooooj.8, and for cyanacetic acid 0-0037, both at 25. Since a = The most logical method so far suggested for dealing with the problem of strong electrolytes is due to Nernst. He considers that, owing to their mutual influence, the activity of the various substances (ions and non-ionised substances) present is not pro- portional to their respective concentrations, but certain correct- ing factors have to be applied depending on the extent of the mutual influence. Among these effects, that of the ions on each other and on the non-ionised part of the molecules, as well as the mutual influence between ions and solvent, seem to be of special importance, but so far comparatively little progress has been EQUILIBRIUM IN ELECTROLYTES 283 made with the determination of the relative magnitudes of the correcting factors. Electrolytic Dissociation of Water, Heat of Neutral- ization So far we have regarded the usual solvent water simply as a medium for dissociation, but there is evidence to show that it is itself split up to a very small extent into ions, according to the equation Applying to this equation the law of mass action, we have, as usual, [H-][OH'] = K[H 2 0], where K is the dissociation constant for water. As the ionic concentrations are extremely small the concentration of the water is practically constant, and therefore the product of the concentration of the ions [H-] [OH'] = K w , a constant. It has been found by different methods, which will be re- ferred to later (p. 293), that the value of the above constant at 25 is about 1*2 x io 14 . In pure water the concentrations of the ions are necessarily equal, hence CH = COH' = N/i'2 x io~ 14 = i -i x 10 ~ 7 at 25. Otherwise expressed, this means that pure water contains rather more than i mol of H* and OH' ions, that is, i gram of H' ions and 17 grams of OH' ions, in io 7 or 10,000,000 litres. The ionic product is independent of whether the solution is acid or alkaline, and therefore in a normal solu- tion of a (completely dissociated) acid, since CH- = i, COH' is only io ~ 14 , and in a solution of a normal alkali Cu- is corre- spondingly small. These considerations are of great importance in connection with the process of neutralization. Assuming that the solutes are completely ionised, the neutralization of i mol of sodium hydroxide by hydrochloric acid in dilute solution may be repre- sented as follows : Na + OH' + H- + Cl' = Na- + Cl' + H 2 O. 284 OUTLINES OF PHYSICAL CHEMISTRY Since Na* and Cl' ions occur in equivalent amount on each side, they may be neglected, and the equation reduces to or, otherwise expressed, the combination of hydrogen and hydroxyl ions to form water. The same equation applies to the neutralization of any other strong base by a strong acid ; provided that the solutions are so dilute that dissociation is prac- tically complete, the process in all cases consists in the combination of H' and OH' ions to ?ion-ionised water. It may, therefore, be anticipated that for equivalent amounts of different strong bases and acids the heat of neutralization will be the same, and that this is actually the case is shown in the first part of the table. The magnitudes of the heats of neutralization apply for molar quantities. Heats of Neutralization. Acid and Base. Heat of Neutralization. HC1 and NaOH 13,700 cal. HBr and NaOH 13,700 cal. HNO 3 and NaOH 13,700 cal. HC1 and JBa(OH) 2 13,800 cal. NaOH and CH 3 COOH 13,400 cal. NaOH and HE 16,300 cal. HC1 and ammonia 12,200 cal. HC1 and dimethylamine n, 800 cal. The fact that the heat of neutralization of strong acids and bases is independent of the nature of the acid and base was long a puzzle to chemists, and the simple explanation given above is one of the conspicuous triumphs of the electrolytic dissociation theory. Below the dotted line in the above table are given the heats of neutralization of two weak acids by a strong base and of two weak bases by a strong acid. As the table shows, the heat development in these cases may be more or less than 13,700 cal. for molar quantities, and a little consideration affords a plausible explanation. The neutralization of acetic acid, which EQUILIBRIUM IN ELECTROLYTES 285 is very slightly ionised, by sodium hydroxide, may be repre- sented by the equation which may be regarded as taking place in two stages (i) CH 3 COOH = CH 3 COO' + H-; (2) H- + OH' = H 2 O. The heat of neutralization is, therefore, the sum of two effects (i) the heat of dissociation of the acid ; (2) the reaction H' + OH' = H 2 O, which gives out 13,700 cal. Hence, since the observed thermal effect is 13,400 cal. the dissociation of the acid must absorb 300 calories. For hydrofluoric acid, on the other hand, the reaction HF= H' + F' is attended by a heat development of 16,300 - 13,700 = 2,600 cal. We have thus, an approximate method of determining the heat of ionisation of electrolytes, which may be positive or negative. In the above paragraphs the total heat change has been regarded as the algebraic sum of the heats of neutralization and of ionisation, but it is probable that other phenomena, for example, changes of hydration, also play a part. Hydrolysis It is a well-known fact that salts formed by a weak acid and a strong base, such as potassium cyanide, show an alkaline reaction in aqueous solution, whilst salts formed by the combination of a weak base and a strong acid, for example, ferric chloride, have an acid reaction. In the previous section it has been mentioned that water is slightly ionised, according to the equation H 2 O = H- + OH', and may therefore be re- garded as at the same time a weak acid (since H- ions are present) and a weak base (owing to the presence of OH' ions). It will now be shown that the behaviour of aqueous solutions of such salts as potassium cyanide and ferric chloride are quanti- tatively accounted for on the assumption that water is electro- lytically dissociated. In a previous section (p. 271) it has been pointed out that when two acids are allowed to compete for the same base, the latter distributes itself between the acids in proportion to their 286 OUTLINES OF PHYSICAL CHEMISTRY avidities, and it has also been shown that the ratio of the avidities of two acids is the ratio of the extent to which they are electrolytically dissociated. The same applies to a salt in aqueous solution, water, in virtue of its hydrogen ion concen- tration, being regarded as one of the competing acids. In the case of a salt of a strong acid, such as sodium chloride, it would not be anticipated that such a weak acid as water would take an appreciable amount of the base, and the available experimental evidence quite bears out this expectation. In other words, an aqueous solution of sodium chloride contains only Na* and Cl' ions and undissociated sodium chloride in appreciable amount, and is therefore neutral. The case is quite different for a salt formed by a strong base and a weak acid, such as potassium cyanide. Here water as an acid is comparable in strength to hydrocyanic acid, and therefore there is a distribution of the base between the acid and the water according to the equation KCN + H 2 O ^ KOH + HCN, the proportions of potassium cyanide and potassium hydroxide depending upon the relative strengths of water and hydrocyanic acid. From the equation it is evident that potassium hydroxide and hydrocyanic acid must be present in equivalent amount ; and since the hydroxide is much more highly ionised than hydro- cyanic acid, the solution contains an excess of OH' ions, and must therefore be alkaline, as is actually the case. This process is termed hydrolysis, i.e., decomposition by means of water. Similar considerations apply to the salts formed by combination of weak bases and strong acids, such as aniline hydrochloride. As water is comparable in strength to aniline as a base, an equilibrium is established according to the equation C 6 H 5 NH 3 C1 + HOH^C C H 6 NH 3 OH + HC1. In this case there is an excess of H* ions, as hydrochloric acid EQUILIBRIUM IN ELECTROLYTES 287 is much more highly ionised than anilinium hydroxide, and therefore the solution has an acid reaction. A salt formed by the combination of a weak acid and a weak base, e.g., aniline acetate, is naturally hydro lysed to a still greater extent. These three types of hydrolytic action will now be considered quantitatively. (a) Hydrolysis of the Salt of a Strong Base and a Weak Acid A typical salt of this type is potassium cyanide, the hydrolytic decomposition of which is represented by the equation KCN + HOHJKOH + HCN, or, according to the electrolytic dissociation theory, K- + CN' + HOH ^ K- + OH' + HCN, on the assumption, which is only approximately true, that potassium cyanide is completely ionised and hydrocyanic acid non-ionised. The equilibrium can now be investigated, and the extent of the hydrolysis determined, if a means can be found of deter- mining the equilibrium concentration of one of the reacting substances, for example, the OH' ions. This could not, of course, be done by titrating the free alkali, as the equilibrium would thus be disturbed, but one of the methods given on p.ayi may conveniently be used. The method which has been most largely used is to determine the effect of the mixture on the rate of saponification of methyl acetate, which, as has already been pointed out, is proportional to the OH' ion con- centration. The amount of hydrolysis per cent., loox, for different concentrations, c, of potassium cyanide (mols per litre) at 25, determined by the above method, is as follows: c . 0*947 0*235 '95 0*024 IQOX . 0*31 0*72 i'i2 2*34 K* . 0'9 I'2 I'2 I^XIO 5 The table shows that, as is to be expected, the degree of hydrolysis increases with dilution. 288 OUTLINES OF PHYSICAL CHEMISTRY A general equation, by means of which the equilibrium con- dition can be calculated when the acid and base are not neces- sarily present in equivalent proportions, can readily be obtained by applying the law of mass action to the general equation B* + A' + H 2 ; B* + OH' + HA, where B' and A' represent the positive and negative ions respec- tively. As B' occurs on both sides of the above equation, the latter can be simplified to A' + H 2 O ^ OH' + HA. As the salt and the base are practically completely ionised, and the acid is not appreciably ionised, A' and OH' are proportional to the concentrations of salt and base respectively, and HA to that of the acid. Hence, from the law of mass action, [OH'][HA] _ [base][acid] A' ~ [unhydrol. salt] " ( ' a constant, as the concentration of the water may be regarded as constant. KA is termed the hydrolysis constant, and, like the ordinary equilibrium constant, is independent of the relative concentrations of the substances present at equilibrium, but de- pends on the temperature. In order to illustrate the use of the above formula, the values of K;, may be calculated from the data for potassium cyanide already quoted. In 0*095 molar solution, potassium cyanide is hydrolysed to the extent of 1-12 per cent., hence 0-095 x I<12 V-base = Cacid = = O*OOIOO4, IOO and C sa it = 0*095 0*001064 = 0*094. (o*ooio64)(o*ooio64) Hence K A = * 22 Z> = r2 x io~ 5 . 0*094 The values of the hydrolysis constant, calculated from the other observations, are given in the table, and are approxi- mately constant, thus confirming the above formula. Con- versely, when from one set of observations the value of EQUILIBRIUM IN ELECTROLYTES 289 K A has been obtained, the degree of hydrolysis at any other dilution can be obtained by substitution in the general formula. For convenience of calculation, the simple formula in which the acid and base are present in equivalent proportions, may be written in the form in which x represents the proportion of acid and base formed by hydrolysis from i mol of the salt and v is the dilution. This form of the equation shows at a glance that the degree of hydrolysis, that is, the value of x, increases with dilution. More- over, from the great similarity of the formula (10) to the dilution formula, it is evident that when the hydrolysis is small it is greatly diminished by the addition of a strong base, just as the degree of dissociation of acetic acid is greatly diminished by the addition of an acetate. The quantitative relation between the hydrolysis constant, KA, and the dissociation constants for the weak acid and water respectively may be obtained as follows : The electrolytic dis- soc'ation of the acid, HA, is represented by the equation [H-][A'] - K, [HA] . . . . (2) where K fl is the dissociation constant of the acid. In the solution there is the other equilibrium [H - ] [OH'] = K w (3) where K w is the ionic product for water. Dividing equation (3) by equation (2) we obtain [OH'] [HA] K w A' B K~ w The left-hand side of the above equation is simply equation (i) for the hydrolytic equilibrium (p. 288), hence [base] [acid] K, , [unhydrol. salt] " ' K fl that is, tJie hydrolysis constant Kh is the ratio of the ionic product fig, for water to thf. dissociation constant of the acid. 2 9 o OUTLINES OF PHYSICAL CHEMISTRY It has already been deduced from general principles (p. 286) that the hydrolysis is the greater the more nearly the strength of water as an acid approaches that of the competing acid, and the above important result is the mathematical formulation of that statement. In order to illustrate this point more fully, the degree of hydrolysis of a few salts in i/io molar solution at 25 is given in the accompanying table. Salt. Degree of hydrolysis. Sodium carbonate . . . 3-17 per cent. Sodium phenolate . . . 3-05 Potassium cyanide . , . 1*12 Borax ..... 0*05 Sodium acetate . . ... 0*008 The numbers illustrate in a very striking way the fact that only the salts of very weak acids are appreciably hydrolysed. Thus although acetic acid is a fairly weak acid (K = i'8 x 10 ~ 5 ), sodium acetate is only hydrolysed to the extent of 0*008 per cent, at 25, and even potassium cyanide is only hydrolysed to the amount of about i per cent, in i/io normal solution, although the dissociation constant of the acid is only 1-3 x 10 ~ 9 . A com- parison of the above table with the dissociation constants of the acids (p. 273) is very instructive. From the known values of K a and K w for hydrocyanic acid and water respectively at 25, we have X lO " 14 .-3 x xe- m very satisfactory agreement with the observed value of n x io~ 6 (p. 288). As a matter of fact, however, it is easier to deter- mine the hydrolysis constant than the dissociation constant for a very weak acid, and therefore the latter is often calculated from the observed value of the hydrolysis constant by means of the above formula* EQUILIBRIUM IN ELECTROLYTES 291 (<*) Hydrolysis of the Salt of a Weak Base and a Strong Acid The same considerations apply in this case as for the salt of a strong base and a weak acid. The general equation for the equilibrium is of the form B- + A' + H 2 O ^ BOH + H- + A' which simplifies to B- + H 2 O^BOH + H\ Applying the law of mass action, we obtain [BOH][H-] [base] [acid] B- [unhydrol. salt] V } exactly the same equation as is applicable to the hydrolysis of he salt of a strong base and a weak acid. Further, it may be shown, by a method exactly analogous to that employed in the previous section, that in this case *-. . . . w that is, the hydrolysis constant Khfvr the salt of a weak base and a strong acid is the ratio of the ionic product for water, K^, and the dissociation constant of the base, K&. A typical case is the hydrolysis of urea hydrochloride, 1 which may be represented thus CON 2 Hg + Cl' + H 2 O^CON 2 H 5 OH + H- + CY. It is clear that the degree of hydrolysis can at once be obtained when the H- ion concentration in the solution has been deter- mined, and for this purpose any of the methods previously described can be employed (p. 275), such as the effect on the rate of hydrolytic decomposition of cane sugar or of methyl acetate or by electrical conductivity measurements. In the experiments quoted in the table, gradually increasing amounts of urea were added to normal hydrochloric acid, and the H' ion concentration deduced from a comparison of the velocity constant for the hydrolysis of cane sugar in the presence of the free acid (k ), and with the addition of urea (k). Walker, Proc. Roy. Soc. (Edin.), 1894, 18, 255. 292 OUTLINES OF PHYSICAL CHEMISTRY Normal hydrochloric acid + c normal urea. k/k l-k/ko C-I + kjko c. k. =free HC1. = salt formed. = free urea. Kh. o 0*00315=^0 i 0-5 0-00237 0753 0-247 '253 '77 ro 0-00184 o'5 8 5 o'^S '5 8 5 ' 8 2 2-0 0*00114 0-36 0-64 1-36 0-77 4-0 0*0006 0-19 0*81 3*19 0*75 On the assumption that the rate of hydrolytic decomposition is proportional to the H* ion concentration, kjk represents the concentration of the --free" hydrochloric acid, and (i - kjk ) that of the bound acid, which is, ofcourse, that of the unhydro- lysed salt. The concentration of the free urea, that is, of the hydrolysed salt, is therefore c - (i + k\k^. Substituting in the general formula [base] [acid] fr-(i +*/*,)] [*/*] [unhydrol. salt] i - k\k The values of the hydrolysis constant are given in the sixth column of the table, and are approximately constant, as the theory requires. The degree of hydrolysis of a few salts of weak bases and strong acids in i/io molar solution at 25 is given in the table, and the results should be compared with the values for the dissociation constants of weak bases (p. 275) in order to illustrate equation (2). Salt. Degree of hydrolysis. Ammonium chloride . . . 0-005 P er cent - Aniline hydrochloride . . . 1*5 Thiazol hydrochloride . . .19 Glycocoll hydrochloride . 20 Hydrolysis of the Salt of a Weak Base and a Weak Acid The hydrolysis of aniline acetate, a typical salt of this classes represented by the equation C 6 H 5 NH 3 CH 3 COO + HOH ^ C 6 H 5 NH 8 OH + CH 3 COOH, EQUILIBRIUM IN ELECTROLYTES 293 which, on the assumption that the salt is completely, the base and acid not at all, ionised, may be written as follows C 6 H 5 NH 3 - + CH 3 COO' + HOH^C 6 H 5 NH 3 -OH + CH 3 COOH. Applying the law of mass action, and using the former sym ols, [BOH][HA] [basejacid] K w [B-][A-J ~ [unhydrol. salt]' " h ~ K a K 6 * If we express the amounts (in mols) of the base, acid and salt respectively in volume v of the solution by b, a and s respectively, the above equation becomes K;,, that is, the degree of hydrolysis of the salt of a weak base and a weak acid is independent of the dilution. Experiment shows that in dilutions of 12*5 and 800 litres, aniline acetate is hydrolysed to the extent of 45-4 and 43-1 per cent, respectively ; the slight deviation from the requirements of the theory is doubtless due to the fact that the assumptions made in deducing the above formula are only approximately true. Determination of the Dissociation Constant for Water It has been shown above that the process of hydrolysis in the case of a salt of a strong base and a weak acid may be looked upon as a distribution of the base between the weak acid and water acting as an acid, and the degree of hydrolysis therefore depends on the relative strengths of the weak acid and water. The relationship between these three factors is expressed by the equation [acid][base] K. [unhydrol. salt] * = K a where K/, is the hydrolysis constant, K a the dissociation con- stant for the acid, and K w the ionic product for water. It is clear that if the degree of hydrolysis of a salt and the dissocia- tion constant of the acid are known, K w can be calculated, and 294 OUTLINES OF PHYSICAL CHEMISTRY this is one of the most accurate methods for determining the degree of dissociation of water. As an illustration, we may calculate K w from Shields's value for the hydrolysis of sodium acetate crooS percent, in o'i molar solution at 25 (Arrhenius, Feb., 1893). We have Cacid = Cbase = O'OOOoS X O'l, Csait = 0*1 (the amount hydrolysed being negligible in comparison). (o'ooooS x o'i) 2 Hence v - '- = 0-64 x io~ 9 = K h . ' O'I Now K w = K h K a = (0-64 x io- 9 ) x (1-8 x icr 5 ) = ri6 x lo" 14 . Since [H-][OH'] is thus found to be approximately 1-2 x io~ 14 , the concentration of H* or OH' ions (mols per litre) in water at 25 is i'i x io~ 7 . K w can also be calculated from measurements of the hydro- lysis of salts of strong acids and weak bases, and, perhaps with still greater accuracy, from measurements with salts of weak ac.ds and weak bases l by means of the formula Kfc = Ku,/K a Kft. The degree of dissociation of water has been determined by three other methods at 25 with the following results : E.M.F. of hydrogen-oxygen cell (Ostwald, January, 1893) (corrected value), i-o x io - 7 at 25. Velocity of hydrolysis of methyl acetate (Van't Hoff- Wijs, March, 1893), 1-2 x io ~ 7 at 25. Conductivity of purest water (Kohlrausch, 1894), 1*05 x io " 7 at 25. When it is borne in mind how small the dissociation is, the close agreement in the values obtained by these four inde- pendent methods is very striking, and forms a strong justifica- tion for the original assumption that water is split up to an extremely small extent into ions. The question can be still further tested by applying van't 1 Lunden, jf. Chim. Phys., 1907, 5, 574 ; Kanolt, J. Amer. Chem. Soc., 1907, 29, 1402. EQUILIBRIUM IN ELECTROLYTES 295 HofFs equation connecting heat development and displacement of equilibrium to the equilibrium between water and its ions. For the degree of dissociation at different temperatures, the following values were obtained by Kohlrausch from conduc- tivity measurements : Temperature . . o 2 10 15 26 34 42 50 Degree of dissociation 035 0-39 0-56 0*8 1-09 1-47 1-93 2-48 xio~ 7 From any two of these measurements the heat development, Q, of the reaction, H 2 O ^ H* + OH', can be calculated by sub- stitution in the general formula (p. 167). log loKl - log 10 K 2 = - From the values l of K at o and 50, Q = - 13,740 cal., and from that at 2 and 42, Q = 13,780 cal. In a previous section (p. 284) it has been pointed out that, according to the electrolyte dissociation theory, the neutraliza- tion of a strong base by a strong acid consists essentially in the combination of H* and OH' ions to form water. The heat given out in the reaction is about 13,700 cal. for molar quanti- ties, in excellent agreement with the above value. This sup- ports the assumption that the variation of the conductivity of pure water with temperature is due to the displacement of the equilibrium H' + OH' ^H 2 O, in the direction indicated by the lower arrow. The value of Q, obtained directly as above, may be termed the heat of ionisation of water ; it is the heat given out when i mol of H* and OH' ions combine to form water. The heat of ionisation of any electrolyte can naturally be calculated in the same way from the displacement of the equili- brium with temperature. The effect of increased temperature on the degree of ionisation is almost always slight, and in the majority of cases the ionisation is slightly diminished. As an illustration, the degree of electrolytic dissociation for i/io molar sodium chloride over a wide range of temperature, as deter- 1 K, = (2-48 x io- 7 ) 2 at 50; K! = (0-35 x io- 7 ) 2 at o (p. 283). 296 OUTLINES OF PHYSICAL CHEMISTRY mined by Noyes and Coolidge, 1 may be quoted. The values obtained were 84 per cent, at 18, 79 per cent, at 140, 74 per cent, at 218, 67 per cent, at 281, and 60 per cent, at 306. Corresponding with the small variation in the degree of ionisa- tion with temperature, the heat of ionisation is small, and may be positive (as in the present case) or negative. Theory of Indicators The indicators used in acidimetry and alkalimetry have the property of giving different colours depending on whether the solution is acid or alkaline. Ac- cording to Ostwald's theory, which has met with fairly general acceptance, such indicators, including methyl-orange, phenol- phthalein and /-nitrophenol, are weak electrolytes, and their use depends on the fact that the ions and the non-ionised com- pounds have different colours. Since salts are almost always highly ionised, it is clear that only weak acids and bases can be employed as indicators. Phenolphthalein is a very weak acid, the non-ionised acid is colourless, and the negative ion red. In aqueous solution it is ionised according to the equation HP^H- + P'(red) (where P' is the negative ion), but so slightly that the solution is practically colourless. If now sodium hydroxide is added, the highly-dissociated sodium salt is formed, and the solution is deeply coloured owing to the presence of the red anion, P'. If, on the other hand, the solution contains a slight excess of acid, the increased H- ion concentration drives back the ioni- sation of the phenolphthalein in the direction indicated by the lower arrow, and the solution becomes colourless (cf. p. 277). Finally, if a weak base, such as ammonium hydroxide, is added, the ammonium salt will be partly hydrolysed, according to the equation NH 4 P + HOH^NH 4 OH + HP, and excess of the base will be required in order to drive back 1 Zeitsch. Physikal Chem., 1904, 46, 323. EQUILIBRIUM IN ELECTROLYTES 297 the hydrolysis (p. 289) ; in other words, there will not be a sharp change of colour when ammonium hydroxide is added. Methyl-orange is an acid of medium strength, the non-ionised acid is red, the negative ion yellow. As the acid is ionised in aqueous solution to some extent, according to the equation HM(red)^H- + M' (yellow), the solution shows a mixed colour. The effect of the addition of acids and alkalis is similar to that on phenolphthalein, and only differs in degree. Since the aqueous solution already con- tains a considerable proportion of H* ions, it is evident, from the considerations advanced on p. 276, that a considerable excess will be required to drive back the dissociation in the direction indicated by the lower arrow, so as to turn the solu- tion red. The proportion of H* ions in such a weak acid as acetic acid is not sufficient for this purpose, and therefore methyl-orange should not be employed as an indicator for weak acids. It is, on the other hand, a suitable indicator for weak bases, such as ammonia, as the salt formed is much less hydrolysed than the corresponding phenolphthalein salt, and therefore the change of colour is sharper. Basic indicators are not in use. The considerations to be borne in mind in selecting an indicator, or in choosing a suitable alkali for titrating an acid, or vice versa, may be put concisely as follows (Abegg) : Solutions used. Acid. Base. Strong Strong Any Any Strong Weak Weak Strong Strong acid Weak acid Methyl-orange, /-nitrophenol Phenolphthalein, litmus Weak Weak None satisfactory Should be avoided Some investigators maintain that the ionisation theory does not give a satisfactory representation of the behaviour of indi- 298 OUTLINES OF PHYSICAL CHEMISTRY % cators, but that the changes of colour are due to changes of constitution, usually from the benzenoid to the quinonoid type and vice vetsd. 1 In an aqueous solution of phenolphthalein, for instance, there are only traces of the quinonoid (coloured) modifi- cation, and the solution is colourless, but on the addition of alkali the phenolphthalein salt is formed, the negative ions of which, being of the quinonoid type, are strongly coloured. The Solubility Product We have now to consider an equilibrium of rather a different type in which the solution is saturated with regard to the electrolyte. In such a case there is equilibrium between the solid salt and the non-ionised salt in the solution, so that the concentration of the non-ionised salt remains constant at constant temperature. Further, there is equilibrium in the solution between the non-ionised salt and its ions, which may be represented, in the case of silver chloride, for example, by the equation Ag* + Cl'^AgCl. Applying the law of mass action, we have, for the latter equilibrium, [Ag-][Cl'] = KfAgCl] = S, where S is the product of the concentrations of the two ions the so-called solubility product and is constant, since the right-hand side of the above equation is constant. The equi- libria in the heterogeneous system may be represented as follows : Ag- + Cl' ^ AgCl (in solution) I t AgCl (solid). As will be shown later, the solubility product for silver chloride at 25 is 1-56 x io- 10 , when the ionic concentrations are ex- pressed in mols per litre. If the solution has been prepared by dissolving the salt in water, the ions are necessarily present in equivalent proportions, so that a solution of silver chloride, saturated at 25, contains x/i'56 x io- 10 = 1-25 x io~ 6 mols of Ag' and of Cl' ions. The ions need not, however, be present in equivalent propor- 1 C/. Hewitt, Analyst, 1908, 33, 85. EQUILIBRIUM IN ELECTROLYTES 299 tions ; if by any means the solubility product is exceeded, for example, by adding a salt with an ion in common with the electrolyte, the ions unite to form undissociated salt, which falls out of solution, and this goes on till the normal value of the solubility product is reached. Perhaps the best-known illustra- tion of this is the precipitation of sodium chloride from its saturated solution by passing in gaseous hydrogen chloride. In this case the original equilibrium between equivalent amounts of Na* and Cl' ions is disturbed by the addition of a large excess of Cl' ions, and sodium chloride is precipitated till the original solubility product is regained, when the solution con- tains an excess of Cl' ions and relatively few Na' ions. As already mentioned, the difference between the present form of equilibrium and those previously considered is that the concentration of the non-ionised salt in the solution is constant at constant temperature. If it is diminished in any way, salt is dissolved till the original value is reached ; if it is exceeded, as in the case just mentioned, salt falls out of solution till the original value is reached. Since the equilibrium equation for a binary salt is symmetrical with regard to the two ions, it follows that the solubility of such a salt should be depressed to the same extent by the addition of equivalent amounts of its common ions, whether positive or negative. This consequence of the theory was tested by Noyes, who determined the influence of the addition of equivalent amounts of hydrochloric acid and of thallous nitrate on the solubility of thallous chloride, with the following results : Solubility of thallous chloride at 25 : Concentration of Substance added (mols per litre). T1NO S added. HC1 added. O 0*0283 0-147 0*0161 0*0084 0*0032 0*0161 0*0083 0*0033 300 OUTLINES OF PHYSICAL CHEMISTRY The figures in the first column show the amounts of thallous nitrate and of hydrochloric acid added, those in the second and third columns represent the solubility of thallous chloride in mols per litre. The results show that the requirements of the theory are satisfactorily fulfilled. The above results hold independently of the relative amounts of ions and non-ionised salt in the solution. Since in dilute solution all salts are highly ionised, it may, however, be as- sumed that difficultly soluble salts, such as silver chloride, are almost completely ionised in solution ; in other words, the con- centration of non-ionised salt in solution may be regarded as negligible in comparison with that of the ions. This deduction is of great importance in estimating the solubility of difficultly soluble salts (see next page). Applications to Analytical Chemistry The above con- siderations with regard to the solubility product are of the greatest importance for analytical chemistry. A precipitate can only be formed when the product of the ionic concentrations attains the value of the solubility product, which for every salt has a definite value depending only on the temperature. For example, magnesium hydroxide is precipitated from solutions of magnesium salts by ammonia because the solubility product [Mg"] [OH'] 2 is exceeded. When, however, ammonium chloride is previously added in excess to the hydroxide, the OH' ion concentration is diminished to such an extent (p. 277) that the solubility product is not reached, and precipitation no longer occurs. Similarly, zinc sulphide is precipitated when the product [Zn"][S"J exceeds a certain value. In alkaline solu- tion, an extremely small concentration of hydrogen sulphide suffices for this purpose, as the sulphide is considerably ionised, but in acid solution the depression of the ionisation of the hydrogen sulphide, in other words, the diminution in the con- centration of S" ions, is so great that the solubility product is not reached. On the other hand, the solubility product for certain heavy metals, such as lead, copper, and bismuth, is so EQUILIBRIUM IN ELECTROLYTES 301 small that it is reached even in acid solution. It is, however, possible to increase the acid concentration (and therefore to diminish the S" ion concentration) to such an extent that the ionic product is not reached even for some of the above metals, for example, lead sulphide in concentrated hydrochloric acid is not precipitated by a current of hydrogen sulphide. On the same basis, a fact which has long been familiar in quantitative analysis, that precipitation is more complete when excess of the precipitant is added, can readily be accounted for. A saturated aqueous solution of silver chloride contains about 1*25 x io~ 5 gram equivalents of the salt per litre, and the ad- dition of ten times that concentration of Cl' ions (added in the form of sodium chloride) will diminish the amount of silver in solution to about i/io of its original value (on the assumption that the concentration of the non-ionised salt is negligible in comparison with that of the ions) (cf. p. 277). It is thus evident that in the gravimetric estimation of combined chlorine as silver chloride there might be considerable error owing to the solubility of silver chloride in water, but if a fair excess of the precipitant is used, the error is quite negligible. The concentration in saturated solution at 25, and the solubility product of a few difficultly soluble salts are given in the accompanying table. Salt. Saturation Concentration Solubility Product (mols per litre). (mols per litre). Silver chloride Ag* = 1*25 x io~ 5 1*56 x io~ 10 bromide ,, = 6-6 x io~ 7 4-35 x io~ 13 iodide = i'o x io~ 8 i'o x io~ 16 Thallous chloride Tl- = 1-6 x io~ 2 2-6 x IQ- 4 Cuprous chloride Or = i'i x io~ 3 1-2 x io~ 6 Lead sulphide Pb" = 5'i x io~ 8 2*6 x io- 15 Copper sulphide Cu" = IT x io~ 21 1*2 x'io~ 42 Experimental Determination of the Solubility of Diffi- cultly Soluble Salts When a saturated solution of a rt-la- 302 OUTLINES OF PHYSICAL CHEMISTRY lively insoluble salt is so dilute that complete ionisation may be assumed (//, = /x^ ), the solubility of the salt may readily be obtained from electrical conductivity measurements. The molecular conductivity at infinite dilution, p,^ , can be obtained indirectly (p. 258), the specific conductivity of the saturated solution is determined in the usual way, and, by substitution in the formula /-i^-, = KV, we obtain the value of v, that is, the volume in c.c., in which a mol of the substance is dissolved. If the solubility is required in mols per litre, then v = 1000 V, and /A oo = i ooo *V, where V is the volume in litres in which a mol of the sub- stance is dissolved. As the specific conductivity of such a solution is small, the conductivity of the water becomes of importance, and it is necessary to subtract from the observed specific conductivity of the solution the conductivity of the water, determined directly. For such measurements, "con- ductivity " water, of a specific resistance not much less than io 6 ohms, should be used. As an example of the determination of solubilities by this method, Bottger found that a solution of silver chloride saturated at 20 had K = 1-33 x io ~ 6 after subtracting the specific con- ductivity of the water. Hence, as /XQQ for silver chloride at 20, determined indirectly (p. 258), is i25'5, we obtain, by substitu- tion in the above formula, 125*5 = 1000 x i '33 x io~ 6 V, that is, 94,400 litres of a solution of silver chloride, saturated at 20, contain i mol of the salt. In one litre of solution there is, therefore, 1/94,400 = 1*06 x io ~ 5 mol, or 0-00152 grams of silver chloride. The values for the solubility of a number of difficultly soluble salts obtained by this method are given in the previous section (p. 301), EQUILIBRIUM IN ELECTROLYTES 303 Complex Ions Complex ions have already been defined as being formed by association of ions with non-ionised molecules It is well known that though silver halogen salts are only slightly soluble in water they are readily soluble in the presence of ammonia. This phenomenon is due to the formation of complex ions (p. 281), in which the Ag' ions are associated with ammonia molecules, fprming univalent ions of the type Ag(NH 3 )^. As nearly all the silver is present in this form and very little in the form of Ag' ions, it is evident that a solution may contain a very considerable amount of a silver salt before the solubility product [Ag-] [X'] is reached. The determination of the exact composition of the complex ions in a solution is sometimes a matter of difficulty, but the law of mass action is often of great assistance in this respect. If, for example, the solution of a silver salt in ammonia contains mainly complex ions of the formula Ag(NH 3 )-, there must be an equilibrium represented by the equation Ag(NH 3 )j ^ Ag- + 2NH 3 , and by the law of mass action the expression , ^ * must be constant. To test this point Ag(NH 3 )- the concentrations of the ammonia and of the silver ions were systematically varied, and it was found that the above expres- sion remained constant, thus showing that the assumption as to the composition of the complex ions is correct. The azure blue solutions obtained by adding ammonia in excess to solu- tions of cupric salts appear from the results of distribution (p. 178) and optical measurements to contain the copper exclusively as Cu(NH 3 ) 4 - ions. The solutions obtained by the action of ammonia on cobalt and chromium salts have been thoroughly investigated by Werner : l they contain complex ions of the formulae Co(NH 3 ) 6 - and Cr(NH 3 ) 6 -. Other compounds besides ammonia can become associated with positive ions to form complex cations. For example, Werner has shown that the ammonia groups in the com- plex cobalt ions mentioned above can be successively dis- 1 Summary, Anorganischf Chemie* 2nd edition, Brunswick, 1909. 304 OUTLINES OF PHYSICAL CHEMISTRY placed by water molecules, forming compounds of the type [Co(NH 3 ) 5 H 2 0]-, [Co(NH 3 ) 4 (H 2 0) 2 ]- . . . and finally [Co(H 2 0) 6 ]- It is probable that in the aqueous solutions of many salts com- plex ions containing water are present. Complex anions, formed by th^ association of negative ions with neutral molecules, are also known. Solutions of cadmium iodide contain CdI 4 " ions (p. 281), and the solution obtained by the addition of excess of potassium cyanide to solutions of silver salts contains potassium silver cyanide, KAg(CN) 2 , which is largely ionised according to the equation Influence of Substitution on Degree of lonisation Reference has already been made to the influence of substitu- tion on the strength of acids. As the effect of substitution on the degree of ionisation has been most extensively investigated for this class of compound, a few further examples may be given. In the accompanying table, the affinity or dissociation constants for some mono-substituted acetic acids are given, the value of K holding for 25 (concentrations in mols per litre). Acetic acid CH 3 COO'H . . . . t , ^ j . 0-000018 Propionic acid CH 3 CH 2 COO'H * . 0*000013 Chloroacetic acid CH 2 C1COO'H . . 0-00155 Bromoacetic acid CH 2 BrCOO'H . *. 0-00138 Cyanacetic acid CH 2 CNCOO'H ;;- . 0*00370 Glycollic acid CH 2 OHCOO-H r; . 0-000152 Phenylacetic acid C 6 H 5 CH 2 COO'H . 0-000056 Amidoacetic acid CH 2 NH 2 COO'H -"..-'.- 3-4 x lo" 10 As the carboxyl group only is concerned directly in ionisation, the above table affords an excellent illustration of the influence of a group on a neighbouring one. The table shows that when one of the alkyl hydrogens in acetic acid is displaced by Cl, Br, CN or OH or C 6 H 5 an increase in the activity of the EQUILIBRIUM IN ELECTROLYTES 305 acid is brought about ; the effect is least for the phenyl group and greatest for the cyanogen group. On the other hand, the methyl group (in propionic acid) diminishes the activity slightly, and the amido group diminishes it enormously. These observations can readily be accounted for 1 on the assumption that the atoms or groups take their ion-forming character into combination. Thus the Cl, Br, CN and OH groups, which tend to form negative ions, increase the tendency of the groups into which they enter to form negative ions. The " negative favouring " character of the phenyl group is slight but distinct. On the other hand, the so-called basic groups, such as NH 2 , lessen the tendency of the group into which they enter to form negative ions, as is very strikingly shown in the case of amidoacetic acid. The methyl group has also a slight diminishing efiect on the tendency of a group to form negative ions. The magnitude of the influence of a substituent on a particu- lar group depends on its distance from that group. This is very well shown by the influence of the hydroxyl group on the affinity constant of propionic acid. Propionic acid CH 3 CH 2 COO'H . . . 0*0000134 Lactic acid CH 3 CHOHCOO'H . . 0-000138 /?-oxypropionic acid CH 2 OHCH 2 COO'H . 0-0000311 When the OH group is in the a (neighbouring) position its effect on the dissociation constant is more than four times as great as when it is in the @ position. It seems plausible to suppose that a comparison of the influence of groups in the ortho, meta and para positions on the carboxyl group of benzoic acid might throw some light on the question of the relative distances between the groups in the benzene nucleus. The dissociation constants of benzoic acid and the three chlor-substituted acids are as follows: 1 A complete theory of the phenomena in question has recently been worked out by Flurscheim (Trans. Chem. Soc. t 1909, 95, 718 ; Proc., 1909, J 93)- 2O 3 o6 OUTLINES OF PHYSICAL CHEMISTRY Benzoic acid C 6 H 5 COOH . . . 0-000060 o- Chlorobenzoic acid C 6 H 4 C1COOH . . 0*00132 m- 0-000155 p- .1 0-000093 It will be observed that the presence of the halogen in the ortho position greatly increases the strength of the acid, and it is a general rule that the influence of substituents is always greatest in this position. The effect of substituting groups in the meta and .para positions is much smaller, and the order of the two is not always the same. As the table shows, ;;*-chlorobenzoic acid is rather stronger than the para acid, but on the other hand />-nitrobenzoic acid is somewhat stronger than the ?neta acid. Similar considerations apply to the influence of substituents on the strength of bases, but, as is to be expected, the effect of the various groups is exerted in the opposite direction to that on acids. Thus the displacement of a hydrogen atom in ammonium hydroxide by the methyl group gives a stronger base (methyl amine) but the entrance of a phenyl group gives a much weaker base (aniline) (cf. p. 275). Reactivity of the Ions It is a well-known fact in qualita- tive analysis that in the great majority of cases the positive component of a salt (e.g., the metal) answers certain tests, quite independently of the nature of the acid with which it is combined, and in the same way acids have certain characteristic reactions, independent of the nature of the base present. These facts are plausibly accounted for on the electrolytic dissociation theory by assuming that the positive and negative parts of the salts (the ions) exist to a great extent independently in solution, and that the well-known tests for acids and bases are really tests for the free ions. Thus silver nitrate is not a general test for chlorine in combination, but only for chlorine ions. It is well known that potassium chlorate gives no precipitate with silver nitrate, although it contains chlorine ; this is readily accounted for on the electrolytic dissociation theory because the solution of the salt contains no Cl' ions, but only C1O 3 ' ions, which give EQUILIBRIUM IN ELECTROLYTES 307 their own characteristic reactions. These views appear still more plausible when cases are considered in which the usual tests fail, for example, mercuric cyanide does not give all the ordinary reactions for mercury. This could be accounted foi by supposing that the compound is not appreciably ionised in solution, so that practically no Hg" ions are present, and as a matter of fact the aqueous solution of mercuric cyanide is practically a non-conductor. The chief characteristic of ionic reactions is their great rapidity ; they are for all practical purposes instantaneous, and it is doubt- ful if the speed of a purely ionic reaction has so far been measured. It is well known that silver nitrate reacts with the chlorine in organic compounds such as ethyl chloride and chlor- acetic acid, but very slowly as compared with its action on sodium chloride. There is good reason for supposing that the reactions last mentioned are not ionic actions, but that the changes take place between the silver salt and combined chlorine. The great reactivity of the ions in cases where it is known that they are actually present has led Euler and others to postulate that all reactions are ionic, and that in very slow reactions we are dealing with excessively small ionic concen- trations. 1 This question cannot be adequately considered here, but it may be mentioned that the available experimental evi- dence does not seem to lend any support to Euler's theory. There is good reason to suppose that chemical reactions may take place between non-ionised molecules as well as between ions. Amphoteric Electrolytes. It is a familiar fact that the hydroxides of certain polyvalent metals show both basic and acidic properties, since they form salts both with acids and bases, e.g., lead hydroxide, Pb(OH) 2 ; aluminium hydroxide A1(OH) 3 . In terms of the ionisation theory, these compounds must give both hydrogen and hydroxyl ions on dissociation. Substances of this type, which can ionise in more than one way, are termed amphoteric electrolytes. Lead hydroxide, Pb(OH) 2 , can dissociate according to the following equations : 1 Compare Arrhenius, Electrochemistry (English Edition), p. 180. 308 OUTLINES OF PHYSICAL CHEMISTRY (i.a)Pb(OH) 2 ^Pb(OH)- + OH'; (i.b)Pb(OH)-^Pb- + OH' (2.a)Pb(OH) 2 ^PbO(OH)'+H- ; (2.b)PbO(OH)'^PbO a "+H- and doubtless all these compounds are present in greater or less concentration in an aqueous solution of lead hydroxide. It will of course be understood that the concentrations of H' and of OH' ions cannot both be considerable in the same solu- tion since the equilibrium [H*] [OH 7 ] = k always holds (p. 283). When an acid is added to the hydroxide, the OH' ions com- bine with the H' ions of the acid to form water, more hydr- oxide dissociates according to equations la and ib, the fresh OH' ions combine with the H- ions to form water, and so on, till ultimately, if sufficient acid is added, the solution contains chiefly Pb" ions and anions derived from the acid. If, on the other hand, alkali is added to the hydroxide, the OH' ions combine with the H' ions derived from the hydroxide and dis- sociation proceeds progressively according to the upper arrows in equations 2a and 2b till ultimately the solution contains chiefly PbO 2 " ions and cations derived from the alkali added. The proof of the above statements is that on electrolysis the lead in acid solution travels to the cathode, in alkaline solution to the anode. Some more complicated compounds can split off both H- and OH' from a single molecule, leaving an uncharged ion or rather an ion which is both positively and negatively charged. For glycine (amidoacetic acid) we have the following equilibrium : + OH-H 3 NCH 2 COOH^H 3 NCH 2 COO + H- + OH'. Ions of this type are termed zwitter ions or hermaphrodite ions. Since they are electrically neutral, they are not affected by an electric current. Practical Illustrations. Dilution Law. Conductivity of Acids and Salts. Many of the results discussed in this chapter can be conveniently illustrated by means of the apparatus 1 shown in Fig. 36. The glass vessels each contain two circular electrodes of platinized platinum, the lower one is connected with a wire which passes through the bottom of the vessel and is connected through a lamp to the wire E. The upper electrode, which is movable, is connected to a wire which 1 Noyes and Blanchard, J. Amer. Chem. Soc.. 1900, 22, 726. EQUILIBRIUM IN ELECTROLYTES 39 passes through the cork loosely closing the vessel, and is connected to the upper wire F. The electrodes in each vessel should be of approximately the same cross-section, and the four lamps of equal resistance. The wires E and F are connected to the terminals of a source of alternating current, and as they are at constant potential throughout, the fall of potential through each of the vessels from E to F must be the same when a current is passing. FIQ. 36. The use of the arrangement may be illustrated by employing it to prove the dilution law in the form a = >Jkv. Solutions of monochloracetic acid containing i mol of the salt in i, 4 and 1 6 litres respectively are prepared, and the vessels A, B and C nearly filled with them. When connection is made with the alternating current, it will be found that the brightness of the lamps is very different, but the positions of the upper electrodes can be so adjusted that the lamps are equally bright. Under these circumstances it is evident that the resistance of each 310 OUTLINES OF PHYSICAL CHEMISTRY solution is the same. On measuring the distances between the electrodes, it will be found that for the solutions v = i, v = 4, v = 1 6, the distances are in the ratio 4:2:1. Hence, as the conductivities are inversely proportional to the distances between the electrodes, aoc *Jv. Further, it may be shown that, although acids differ very greatly in conductivity, neutral salts, even of weak acids, have a conductivity nearly as great as that of strong acids. The vessels are filled with 1/4 normal solutions of hydrochloric acid, sulphuric acid, monochloracetic acid and acetic acid respectively, and when the distances are altered till the lamps are equally bright, it will be found that ths electrodes are very near in the acetic acid solution, far apart in the hydrochloric acid solution, and at intermediate distances for the other two acids. Sufficient sodium hydroxide to neutralize the acid is now added to each vessel, and after stirring and again adjusting to equal brightness of the lamps, it will be found that the distances for all four solutions are approximately equal. Eqtdlibrium Relations as shoivn by Indicators The equi- librium relations in the case of weak acids and bases may be shown very well by means of indicators. Each of two beakers contains 100 c.c. of water, i c.c. of n/i sodium hydroxide, and a few drops of methyl-orange. To the con- tents of one beaker n hydrochloric acid is added drop by drop by means of a pipette, and to the other n acetic acid is added in the same way till both solutions just become red. It will be observed that whereas about i c.c. of hydrochloric acid brings about the change of colour (owing to its relatively high concentration in H' ions), several c.c. of acetic acid are required to produce the same effect, owing to the much smaller H' ion concentration of the latter solution. If now a strong solution of sodium acetate is added to the last solution, the yellow colour of the methyl-orange will be restored; the acetate reduces the strength of the acid to such an extent (p. 277) that the H' ion concentration is no longer sufficient to drive back the ionisation of the methyl-orange. EQUILIBRIUM IN ELECTROLYTES 311 The effect of hydrolysis may be illustrated with indicators as follows : Each of two beakers contains 50 c.c. of 1/2 n hydro- chloric acid and a few drops of methyl-orange and phenol- phthalein respectively. If n ammonium hydroxide is slowly added to the solution containing methyl-orange, the colour will change when about 25 c.c. of ammonia has been added, but a much greater quantity of the same solution will be re- quired to redden the phenolphthalein solution. The explanation of this behaviour has already been given. Owing to the fact that the ammonium salt of phenolphthalein is considerably hydrolysed, it is necessary to add a fair excess of the base before the coloured phenolphthalein ions are produced in considerable amount. The Solubility Product The conception of the solubilit) product may be illustrated by the method employed by Nernst in proving the formula experimentally. A saturated solution of silver acetate is prepared by shaking the finely-powdered salt with water for some time. To a few c.c. of the solution in a test-tube a few c.c. of a fairly concentrated solution of silver nitrate are added, and to another portion of the acetate solution a solution of sodium acetate equivalent in strength to the silver nitrate solution, and the mixtures are well shaken. In each tube a precipitate of silver acetate will be formed. Complex Ions The evidence in favour of the view that in solutions of silver salts in potassium cyanide the silver is mainly present as a constituent of a complex anion, Ag(CN)' 2 , is that the silver migrates towards the anode during electrolysis. The copper in Fehling's solution is also mainly present as a component of a complex anion, as may readily be shown qualitatively by a simple experiment described by Kiister. A U-tube is about half-filled with a dilute solution of copper sulphate, and the two limbs are then nearly filled up with a dilute solution of sodium sulphate in such a way that the boundaries remain sharp. A second U-tube is filled in an exactly similar way with Fehling's solution in the lower part and an alkaline solution of sodium tartrate in the upper part, 3 i2 OUTLINES OF PHYSICAI CHEMISTRY the arrangement being such that the Fehling's solution in the one tube stands at the same level as the copper sulphate solu- tion in the other tube. The U-tubes are then connected by a bent glass tube, filled with sodium sulphate solution, and with the ends dipping in the sulphate and tartrate solutions respectively. A small current is then sent through the U-tubes in series, by means of poles dipping in the outer limbs of the tubes, and after a time it will be observed that the copper sulphate boundary has moved with the positive current, whilst the coloured boundary in the other tube has moved against the positive current towards the anode. It is therefore evident that in the latter case the copper is present in the anion, as stated above. Chemical Activity and lonisation The great difference in chemical and electrical activity produced by ionisation is well shown by comparing the properties of solutions of hydrochloric acid gas in water and in an organic solvent such as toluene. Whilst the former solution conducts the electric current and dissolves calcium carbonate rapidly, the latter solution is a non- conductor, and has little or no effect on calcium carbonate. The same fact is illustrated by the interaction of silver nitrate with potassium bromide, ethyl bromide and phenyl bromide respectively in alcoholic solution. Approximately 5 per cent, solutions of the bromides in ethyl alcohol are prepared, and to each solution is added a few c.c. of a saturated solution of silver nitrate in alcohol. With the potassium bromide there is an immediate precipitate, the action being ionic. With ethyl bromide the reaction is very slow, and there is no apparent reaction with phenyl bromide. The reaction between silver nitrate and ethyl bromide is a good example of a chemical change which is not ionic, as far as one of the reacting substances (the ethyl bromide) is concerned. Non-ionic chemical changes may, however, be very rapid. A solution of copper oleate in perfectly dry benzene reacts immediately with a solution of hydrochloric acid gas in dry benzene, with precipitation of cupric chloride (Kahlenberg), CHAPTER XII COLLOIDAL SOLUTIONS. 1 ADSORPTION Colloidal Solutions. General Up to the present we have dealt with substances which on the basis of their osmotic and electrical behaviour may be classed either as electrolytes or non -electrolytes. In the present chapter we are concerned with a new type of substance which differs in many respects both from typical electrolytes and non-electrolytes. The first discoveries in this field we owe to Thomas Graham (1861) who found that whilst certain substances diffuse rapidly in solution and readily pass through animal and vegetable membranes, other substances diffuse very slowly in solution and are unable to pass through membranes. To the first class of substances, which can readily be obtained in crystalline form, Graham gave the name crystalloids, whilst the members of the other class, which cannot as a rule be obtained in crystalline form, were termed colloids. Most inorganic acids, bases and salts and many organic compounds, such as acetic acid, cane sugar and urea are crystalloids ; starch, gum, gelatine, caramel and pro- teins in general belong to the group of colloids. The dif- ferences in the rates of diffusion in aqueous solution of typical crystalloids and colloids are illustrated in the following numbers, valid for 10, which represent the relative times required for the same amount of diffusion of different substance's. 1 For fuller details of the subjects treated of in this chapter see Philip, Physical Chemistry : Its Bearing on Biology and Medicine (Arnold, 1910) ; Freundlich, Kapillarchemie (Leipzig, 1909) ; Wolfgang Ostwald, Kolloid* chemie (Dresden, 1911). 314 OUTLINES OF PHYSICAL CHEMISTRY Crystalloids. Colloids. Substance Relative times of equal diffusion . HC1 i NaCl 2-3 Cane Sugar 7 Albumen 49 Caramel 98 As under equivalent conditions the rate of diffusion is pro- portional to the osmotic pressure of the solute, it follows that the osmotic pressure of dissolved colloids is very small and therefore that their molecular weights are very high. This view as to the high molecular weight of colloids was held by Graham, who suggested that the differences in behaviour of the two classes of substance might be connected with the much greater size of colloidal particles as compared with dissolved particles of crystalloids. It may be said at once that later investigation has fully confirmed the view as to the high molecular weight of colloids in solution. As was to be anticipated, the later developments of the subject have led to modifications of Graham's views in some essential respects. In the first place it has been shown that colloids are not a special class of substances ; the colloidal state is a condition into which practically all chemical substances can be brought by suitable methods. For example, metals such as silver and platinum, and even salts such as silver chloride and sodium chloride, all of which are ordinarily met with in crystalline form, can be obtained in colloidal solution. There are, however, great differences in the readiness with which dif- ferent substances can be brought into the colloidal state, and some substances, such as starch and gelatine, are only met with in solution in the colloidal form. A further point, which has been established within the last few years, is that colloidal solutions are not solutions in the ordinary sense of the term. A true solution has been defined as a homogeneous mixture, and therefore consists of a single COLLOIDAL SOLUTIONS. ADSORPTION 315 phase. A colloidal solution, on the other hand, such as col- loidal platinum, can be shown to be heterogeneous ; that is, it consists of two phases at least. As we shall see later, however, all intermediate stages exist between colloidal solutions and true solutions on the one hand, and between colloidal solutions and ordinary suspensions on the other. Within the last few years it has become usual to speak of the phase present in separate particles as the disperse phase and the liquid in which it is distributed as the dispersion medium. The preparation of some typical colloidal solutions, and the properties characteristic of the colloidal state, will now be considered. Preparation of Colloidal Solutions A suitable colloidal solution for demonstration purposes is that of arsenious sul- phide. It is prepared by passing hydrogen sulphide through a cold aqueous solution of arsenious oxide, free from electrolytes, sufficiently long to ensure conversion to arsenious sulphide. Excess of hydrogen sulphide is then removed as far as possible by a stream of hydrogen. The resulting solution, after filtra- tion, is yellowish in colour and clear by transmitted light, but appears turbid by reflected light. The degree of dispersion of the sulphide (that is, the size of the particles) varies greatly with the mode of preparing the solution. Silicic acid is obtained in colloidal solution by slowly add- ing a solution of sodium silicate to excess of hydrochloric acid and then removing the sodium chloride and free hydrochloric acid by dialysis. The simplest form of dialyser is a tube of parchment paper into which the mixture is poured. The tube is then suspended by its ends in water which is continually re- newed, and in course of time the crystalloids are completely removed by diffusion through the membrane, leaving a pure colloidal solution of silicic acid. Ferric hydroxide is obtained in colloidal solution (so called " dialysed iron ") by dissolving the freshly precipitated hydrox- ide in a dilute solution of ferric chloride, and removing the 316 OUTLINES OF PHYSICAL CHEMISTRY ferric chloride by dialysis. Other colloidal hydroxides may be obtained by an analogous method. The preparation of colloidal platinum according to Bredig has already been described (p. 232). Other colloidal metals (e.g. gold, silver, palladium) have been prepared by the same method. Colloidal gold and other metals can also be pre- pared by reducing the corresponding salts in aqueous solution. Gelatine, gum and certain other substances form colloidal systems on simple solution in water. Osmotic Pressure and Molecular Weight of Colloids It has already been mentioned that, corresponding with their slow rate of diffusion, the osmotic pressure of colloidal solutions is very small. This is fully confirmed by recent investigations, but direct quantitative measurements by different observers have not led to very concordant results. One of the principal sources of error has been the difficulty of freeing colloids com- pletely from electrolytes, which even in very small concentra- tion have considerable osmotic pressure. This difficulty is to some extent overcome by using another colloid, such as parch- ment paper, as semi-permeable membrane ; one colloid, whilst usually permeable for crystalloids, is impermeable to other col- loids. Hence, as parchment paper and other membranes are permeable for dissolved salts, the latter cannot set up a lasting osmotic pressure, and a pressure which persists for a consider- able time may be regarded as due to the colloid only. As illustrating the nature of the results obtained, Lillie, 1 using a collodion membrane, found that a solution of egg albu- men containing 12*5 grams per litre gave an osmotic pressure of 20 mm. of mercury at room temperature. According to Waymouth Reid the osmotic pressure of a i per cent, solution of haemoglobin is about 4 mm. of mercury, but much higher values, indicating a molecular weight of about 16,000, were ob- tained by Roaf (1910). 1 Amer. Journal of Physiology, 1907, 30, 127. COLLOIDAL SOLUTIONS. ADSORPTION 317 Moore and Roaf l observed a pressure of about 70 mm. of mercury for a 10 per cent, solution of gelatine, which remained fairly steady fur two months. The effect of electrolytes on the magnitude of the osmotic pressure depends on the nature of the colloid. Neutral salts in many cases lower the osmotic pressure of colloids, a result probably due to partial coagulation of the colloidal particles. Acids and bases often raise the osmotic pressure of colloids, probably in consequence of chemical combination. As the osmotic pressure of colloids is so small when measured by the direct method it will readily be understood that the freezing points and boiling points of colloidal solutions scarcely differ from those of pure water. This is evident when we consider that a solution of osmotic pressure 70 mms. (as observed in the experiments just described) would have a freezing-point less than yj^ below that of water. Optical Properties of Colloidal Solutions The majority of colloidal solutions appear homogeneous even under the highest power of the microscope, but their heterogeneous char- acter is established by means of the so-called "Tyndall phe- nomenon ". When a ray of light enters a darkened room its path is recognised by the scattering of the light at the surface of dust particles. Similarly, the path of a beam passed through a colloidal solution can be detected by the scattering of the light at the surface of the ultramicroscopic particles, whereas no indication is afforded of the path of a beam passed through a solution which contains no particles exceeding a certain magnitude. Light which has passed through a colloidal solu- tion is partially or completely polarised. The Tyndall phenomenon has recently been utilised in the construction of the ultra microscope, by means of which our knowledge of colloidal solutions has been greatly extended. An intense beam of light (the arc light or, better, sunlight) is 1 Moore and Roaf, Biochem. Jonrn. 1906, 2, 34. 3 i8 OUTLINES OF PHYSICAL CHEMISTRY directed on a very thin layer of the colloid and the latter examined by a microscope at right angles to the direction of the beam, the entrance of light from other sources being pre- vented. When a homogeneous liquid is used the field remains quite dark, but when the liquid contains discrete particles their presence is indicated by the appearance of colourless or (for smaller particles) characteristically coloured luminous moving points on a dark background. It must be emphasised that the ultramicroscope does not render the particles themselves visible, but only shows the light reflected from them, so that such observations afford no information as to the shape, colour, etc., of the particles. The average size of the particles in a colloidal solution can be estimated indirectly by counting the number in a given volume and determining the total amount of substance by analysis. In this way it has been shown that the particles vary greatly in magnitude, depending on the nature and mode of preparation of the colloidal solution, from such as are visible in the ordinary microscope to those not resolvable even by the ultramicroscope. Particles visible in the ordinary microscope (diameter exceeding 250 /A/A, where /x = 0*001 mm. and /A/A = o-oooooi mm.) are termed by Zsigmondy microns, those detected only by the ultramicroscope (diameter 6-250 /A/A) are termed submicronS) and those of diameter less than 6 /A/A amicrons. For comparative purposes it may be mentioned that the wave- length of sodium light is 589 /A/A, It has been calculated l that the diameter of an ether molecule is about o'6 x io~ 6 mm. = 0-6 /A/A, so that the smallest particle which can be detected by the ultramicroscope has a diameter only ten times greater than that of an average chemical molecule. Brownian Movement When a colloidal solution contain- ing microns (e.g. mercuric sulphide, suspension of gum mastic) is examined under the microscope, the particles are seen to be 1 Perrin, loc. /., p. 50. COLLOIDAL SOLUTIONS. ADSORPTION 319 performing continuous irregular movements (R. Brown, 1827) "They go and come, stop, start again, mount, descend, remount again, without in the least tending towards immobility " (Perrin). Observations with the" ultra-microscope show that the move- ments are the more brisk the smaller the particles and the less the viscosity of the liquid, and they become more rapid with rise of temperature. The phenomenon persists for years; it is not due to any external cause, such as alterations of temperature or of illumination, and it is now generally agreed that it is a consequence of " the incessant movements of the molecules of the liquid which, striking unceasingly the observed particles, drive them about irregularly through the fluid, except in the case where these impacts exactly counterbalance one another " (Perrin, loc. "/.). It has been shown within the last few years, . more particularly by Perrin, that the rates of movement of the particles are in entire accord with those deducted on the basis of the molecular -kinetic theory, which amounts to an experi- mental proof of the atomic constitution of matter and of the kinetic nature of heat J (cf. p. 32). Electrical Properties of Colloids When two plates are placed at some distance apart in a colloidal solution and con- nected with a source of E.M.F. it will be found as a rule that the particles move slowly towards the anode or cathode ; in other words, they behave as if they are electrically charged. The simplest method of making the experiment is to place the colloidal solution in the lower part of a U-tube, which is filled up on both sides with distilled water in which the electrodes are placed. The latter are then connected with the terminals of the lighting circuit (100-200 volts) and the speed of the moving boundary observed directly. The results show that particles of all kinds move at the rate of 10-40 x io~ 5 . cm per second for a potential gradient of i volt per cm. As we have seen, this is also the order of the migration velocity of the ions 'Ostwald, Giundriss der Allg. Chemie., p. iv, 545. 320 OUTLINES OF PHYSICAL CHEMISTRY (p. 253) and we have therefore the remarkable fact that particles of all sizes microns, submicrons, amicrons, ions move with approximately the same speed in the electric field. In the case of the noble metals (gold, platinum, silver, etc.) and the sulphides (arsenic and antimony trisulphides) the particles are negatively charged and move towards the anode, whilst hydroxides (ferric and aluminium hydroxides, etc.) and haemo- globin are positively charged. The charge on some colloids can, however, be altered in sign by certain additions to the medium. Thus Hardy has shown that when acid is added to egg albumen it migrates to the cathode, whilst in alkaline solu- tion it moves towards the anode. The condition in which the colloid is uncharged is known as the isoelectric point> which in the case of egg albumen occurs in approximately neutral solu- tion. Precipitation of Colloids by Electrolytes It is a re- markable fact that many colloidal solutions are readily coagu- lated by the addition of electrolytes. When, for example, a few drops of barium chloride solution are added to a colloidal solution of arsenic sulphide the solution becomes turbid, and in a few minutes the sulphide has completely separated in flocks. The process can be followed under the ultramicroscope, and is seen to consist in a gradual aggregation of the particles (amicrons to submicrons, then to microns and finally to large flocks) the Brownian movement becoming slower and slower and finally ceasing. The efficiency of different electrolytes in the coagulation of arsenic sulphide depends mainly on the valency of the anion and is largely independent of its nature. The molar concen- trations of A1C1 3 , BaCl 2 , and KC1 required to produce same degree of coagulation under conditions otherwise equivalent areas follows: i: 7*4: 532 (Freundlich). With solutions of ferric hydroxide, on the other hand, the coagulating power of electrolytes is practically independent of the valency of the cation, and is determined chiefly by the valency of the anion. COLLOIDAL SOLUTIONS. ADSORPTION 321 Thus the molar concentrations of K 2 SO 4 and KC1 which pro- duced the same effect are in the ratio i : 45. When it is remembered that the particles of arsenious sul- phide are negatively charged and those of ferric hydroxide positively charged the bearing of these results at once becomes evident. The ion which brings about the coagulation of a colloidal solution is the one carrying a charge of opposite sign to that on the colloidal particles (Hardy). Further investigation has shown that this rule can be extended to the reciprocal action of colloidal particles, inasmuch as two colloidal solu- tions containing particles of contrary sign coagulate on mixing (e.g. colloidal platinum and ferric hydroxide) whilst colloids of the same sign are practically without influence on each other. As regards the nature of the coagulation, it has been shown that in certain cases at least the electrolyte is partially decom- posed, the precipitating ion being carried down along with the precipitate and the inactive ion left in solution in combination with another ion. In order to understand this phenomenon it is necessary to consider rather more fully the question of the stability of a colloidal solution. It has been shown by Hardy, Burton and others that certain colloids reach their point of maxi- mum instability (that is, coagulate most readily) when the charge on the particles (as indicated by their behaviour under the influence of a potential gradient) reaches a minimum. Taking as illustration the coagulation of arsenious sulphide by potassium chloride solution we may assume that some of the salt is taken up by the colloidal particles, the negative charges on the latter are neutralized by the K- ions, with the result that the particles become unstable, aggregate and fall out of solution carrying the K- ions along with them (presumably as a salt). The Cl* ions are left in the solution along with an equivalent of H- ions derived from the hydrogen sulphide always associated with the colloidal sulphide. This is the so-called "adsorp- tion " theory of coagulation. Other theories of the pheno- 322 OUTLINES OF PHYSICAL CHEMISTRY menon, notably Billiters "condensation" theory, have also been proposed, but cannot be dealt with here. 1 Suspensions, Suspensoids and Emulsoids All the pro- perties discussed in the previous sections (with the possible exception of the action of electrolytes on the stability) are characteristic of colloidal solutions in general, as well as of suspensions of particles easily visible under the microscope. As typical ' suspensions " may be mentioned clay, finely divided charcoal or gum mastic stirred up with water. They consist of a practically insoluble solid phase, distributed in a liquid, usually water. The particles settle to the bottom of the vessel more or less rapidly, depending on their magnitude, but the system " clears " much more rapidly when electrolytes are added (cf. previous section). From the suspensions we pass through a series of intermediate stages to the suspensoids or suspension colloids, the heterogeneous character of which is only recognised by Tyndall's phenomenon or by the ultramicroscope. Like the suspensions, they consist of a solid phase distributed in a liquid, generally water. " Colloidal solutions " are divided into two fairly well-defined classes, the suspension colloids or sus- pensoids just mentioned and the emulsion colloids or emulsoids. The suspensoids are scarcely more viscous than water, do not gelatinise and are readily precipitated by electrolytes. The emulsoids are viscous, become gelatinous under certain condi- tions and are not readily precipitated by electrolytes. The colloidal metals, sulphides and hydroxides are suspensoids ; silicic acid, gelatine, gum, mucilage of starch and proteins in general are emulsoids. Emulsoids, like suspensoids, are two- phase systems, but consist of two liquid phases, one a honey- comb-like structure, rich in coJloid, in the meshes of which the other phase, composed of a dilute solution of the colloid, is distributed. Thus an aqueous solution of gelatine is made up of two phases, one rich in water and containing a 1 Wo. Ostwald, Kolloidchemie, p. 499. COLLOIDAL SOLUTIONS. ADSORPTION 323 little gelatine in true solution, the other rich in gelatine, but containing a little water (Hardy). It is a familiar fact that an emulsoid such as silicic acid can be obtained as a clear, apparently homogeneous solution (p. 315) which on long standing, more rapidly on boiling or on treatment with electrolytes, changes to a semi-solid amorphous mass. The clear solution is termed a so/, the gelatinous mass a gel. The term sol is also applied to suspensoids. When the electrolyte is removed by washing and the gel is again treated with water certain emulsoids, such as the proteins, return to the sol modification (more readily on warming) and are therefore termed reversible colloids. Suspensoids in general and certain emulsoids, such as silicic acid, do not return to the soluble form under these conditions and are therefore known as irre- versible colloids. The coagulation of emulsoids by electrolytes seems to be entirely different to the action on suspensoids, but is by no means well understood. Whether the electrical character of the particles and of the electrolyte plays any part in the process is doubtful ; in fact silicic acid sol seems to be most stable in the electrically neutral condition. The addition of neutral salts in considerable concentration causes the separation of the solid phase, but the ratio of the activities of different electrolytes is quite different from that observed for suspension colloids and resembles the "salting out " observed, for instance, in the effect on the solubility of gases in water (p. 84). Filtration of Colloidal Solutions It has already been pointed out that systems of all degrees of dispersion are met with, from those containing large particles easily visible under the microscope to molecular dispersed systems, which we term true solutions. It is evident, however, that true solutions are only apparently homogenous ; the solute particles are so minute as to escape our present methods of detecting heterogeneity. As already explained, the size of colloidal particles can be roughly estimated by counting the number in a given volume 324 OUTLINES OF PHYSICAL CHEMISTRY of solution containing a known weight of the disperse phase. Another method which has recently come into use for this pur- pose is to use filters with pores of different sizes. Bechhold, 1 who has done much work on this subject, uses filter- papers impregnated with gelatine solutions of different concentrations, and finds that a filter with 2 per cent of gelatine retains all particles of diameter less than 44/^, one containing 4-4*5 P er cent, is required to retain the much smaller particles of serum- albumen, the average molecular weight of which is about 10,000 (3,000-15,000). The permeability of such filters is of course influenced by the pressure under which filtration is carried out. A very early form of the "ultra-filter," introduced by Martin, consists of an ordinary porcelain filter impregnated with gela- tine. Adsorption. General It is a familiar fact that when water containing a colouring matter such as caramel or litmus is shaken up with finely divided charcoal the latter on settling carries down the colouring matter with it, leaving the water practically colourless. Further investigation shows that other substances, including electrolytes and non-electrolytes as well as colloids, are largely taken up by charcoal from aqueous solu- tion, and that other finely divided substances have the same property. Charcoal has also the power of taking up gases, es- pecially those which are easily liquefied, such as ammonia and sulphur dioxide. The nature of this phenomenon will be more readily under- stood in the light of some quantitative observations, and for this purpose the results of a series of experiments carried out by Schmidt 2 on the taking up of acetic acid from aqueous solution by charcoal are quoted. Animal charcoal (in quan- tities of 5 grams) was shaken up with aqueous solutions of acetic acid (100 ccs. in each case) of different concentrations and the 1 Zeitsch. Chem. Ind. Kolloide, 1907, 2, 3. 2 Zeitsch. physikal Chem., 1910, 74, 689. COLLOIDAL SOLUTIONS. ADSORPTION 325 amount of acid remaining in the water phase determined by titration. In the accompanying table A c represents the amount of acetic acid taken up by the charcoal and A w the amount left in solution at equilibrium. DISTRIBUTION OF ACETIC ACID BETWEEN WATER AND CHARCOAL. A c 0*93 1*15 1*248 i '43 i '62 A w 0*0365 0*084 0*13 0*206 '35o Cc/Cw 205 208 180 203 197 As the volume of the solution and the amount of charcoal are kept constant, the amounts given in the table are propor- tional to the respective concentrations, C c and C w , in the two phases. The figures show (i) that in very dilute solution the acid is almost completely taken up by charcoal ; (2) that the con- centration in the charcoal increases much less rapidly than the concentration in the aqueous phase. That we are dealing with true equilibria is shown by the fact that the same results are obtained from either side (starting from concentrated or from dilute solutions of the acid). The question now arises as to how these observations are to be interpreted. In the first instance we will consider whether the process is a physical or a chemical one, and if the former, whether it is mainly a surface condensation or whether solid solutions are formed. It appears highly improbable for several reasons that the phenomena are chemical in nature. In the first place the most various substances, including argon and the other in- active gases, which do not, as far as is known, enter into chemical combination, are taken up by charcoal. Further, a definite chemical compound is constant in composition and, if undissociated, its composition is independent of the concentra- tion in the other phase, whereas, as the table shows, the composi- tion of the carbon-acetic acid system varies continuously 326 OUTLINES OF PHYSICAL CHEMISTRY within wide limits. At first sight it would appear possible to explain the results as being due to the formation of a partially dissociated solid compound in equilibrium with its products of dissociation, but it can easily be shown that this assumption also is incompatible with the facts. Applying the law of mass action to such an equilibrium (in the liquid phase) we have (cf. p. 173) [Absorbent] n i [Substance taken up] ^/[Compound] w 8= Const. where the square brackets represent concentrations, and i, ;zaand ^3 represent the number of molecules of the absorbent (charcoal), the substance taken up (acetic acid) and the compound re- spectively taking part in the equilibrium. Further, since the active masses of the charcoal and the compound are constant [Substance taken up] = Constant (in liquid phase) that is, the concentration of the acetic acid in the solution must be constant as long as both solid phases are present. As a matter of fact, the concentration of acetic acid in the solution increases continuously with the total concentration (compare table), so that no second solid phase (no chemical compound) can be present. The formation of a solid dissociating compound from a solid phase and a substance in solution has been investigated by Walker and Appleyard in the case of diphenylamine and picric acid, which combine to form the slightly soluble brown com- pound diphenylamine picrate. 1 Until the concentration of the acid in the aqueous layer reached 0-06 mols per litre the solid diphenylamine (which is practically insoluble in water) remained colourless, on further addition of picric acid the brown diphenylamine picrate began to form, and finally practically all the diphenylamine was converted into picrate, the concentration of the picric acid in the solution remaining all the time practically constant at 0*06 mols per litre. It is evident that 1 Walker and Appleyard, 1896, 69, 1334. COLLOIDAL SOLUTIONS. ADSORPTION 327 the system exactly corresponds with the calcium carbonate calcium oxide carbon dioxide equilibrium already considered (p. 174), except that in the latter case the substance of variable concentration (the carbon dioxide) is in a gaseous and not in a liquid phase. It remains to consider whether the phenomena in question, such as the taking up of acetic acid by charcoal, are due to surface condensation or whether solid solutions are formed. It would seem possible to decide this question at once by observing the rate of establishment of equilibrium, since surface condensation must be a very rapid process, and the formation of a solid solution, whereby (in the case under consideration) one substance has to diffuse into the interior of the other, must be very slow. As a matter of fact the estab- lishment of equilibrium in many cases (but not in all cases, see below) is practically instantaneous, which lends strong support to the surface condensation theory. The strongest evidence in favour of the latter theory, however, is based on a considera- tion of the ratio of the distribution of the substance between the two phases. It has been shown (p. 178) that when a substance distributes itself between two phases the ratio of the distribution is independent of the concentration provided the molecular weight of the solute is the same in both solvents, but if the molecular weight in the solvent A is n times that in the solvent B then /s/C A /C B is constant, which may be written more conveniently thus : C^*/C B = Constant. Now the table on p. 325 shows that for the distribution of acetic acid between water and charcoal the formula holds approximately C C 4 /C W = Constant where C c and C w represent the concentrations in charcoal and in water respectively. Comparing this with the distri- bution formula, C*fQ^ = Constant, we find that i/x = 4 or x = 1/4; that is, if charcoal and water may be regarded as two solvents 328 OUTLINES OF PHYSICAL CHEMISTRY between which the acetic acid is distributed then the molecular weight of the acid in charcoal is 1/4 that in water. Now it was shown by Raoult that acetic acid exists as single molecules in aqueous solution, so that its molecular weight in charcoal, deduced on the assumption that it is present in solid solution, is an impossible one. Analogous results are obtained with other solutes and other absorbing agents and it follows at once that the " solid solution " explanation of the phenomena under consideration is definitely disproved. There is evidence, however, that in some cases solid solution may play a subsidi- ary part in the phenomena. Thus Davis 1 found that when iodine is shaken up with charcoal a very rapid action is followed by a slow action, the latter being presumably due to the slow diffusion of the iodine into the interior of the charcoal. Similarly McBain 2 has shown that when hydrogen which has been in contact with charcoal for a long time is pumped out the greater part of it (that condensed on the surface) can be drawn off immediately, but a small residue (presumably present in solid solution) can only be removed very slowly. It has now been established that the phenomenon under consideration is physical in nature and mainly at least due to surface condensation. In order to distinguish it from such a process as the absorption of gases in liquids, an example of true solution, the process is termed Adsorption, and the substance which is condensed on the surface of the solid phase is said to be adsorbed. Adsorption of Gases. Adsorption Formulae. So far we have been concerned mainly with the adsorption of sub- stances from solution. It is now necessary to deal a little more in detail with the fact already mentioned, that porous substances have a considerable adsorptive power for gases, and that those gases which are most easily liquefied are most largely adsorbed. The nature of the results is well shown by the recent accurate 1 Trans. Chem. Soc., 1907, 91, 1666. 2 Phil. Mag., 1909, 18, 816. COLLOIDAL SOLUTIONS. ADSORPTION 329 work of Homfray l and of Titoff 2 on the adsorption of gases by charcoal. The amount of gas adsorbed is proportional to the adsorbing surface and is the greatei the lower the temperature and the higher the pressure. Titoff found that the adsorption of hydrogen follows Henry's law, so that the formula C A /C B = Constant applies, where C A represents the concentration in the solid phase, C B that in the gas phase. The other gases at low tem- peratures do not follow Henry's law, but the results are repre- sented fairly satisfactorily by a formula of the type C^/*/C B = Constant. The adsorptive power of charcoal for traces of gas, especially at low temperatures, has been used by Dewar to obtain the highest vacua yet reached; the pressures were too low to be capable of measurement. It has been shown above that a formula of the type C A '*/C B = Constant an exponential formula affords a fairly satisfactory representation of the adsorption both of gases and dissolved substances. In the literature it is met with in a slightly different form, which will now be given. Instead of writing C A ^/C B we may put CA/ C* = Constant. When for C A we put x/m, where n represents the amount of sub- stance adsorbed by m grams of adsorbent, we obtain, putting p for C B and i/n for x, the formula x/m = ftp l/n where /3 and n are constant at constant temperature. When i/n = i the adsorption follows Henry's law, but in almost every instance i/n is considerably less than i. This expresses the important fact that adsorption is relatively greatest from dilute solution and falls off rapidly with the concentration (p-325). The Cause of Adsorption Adsorption of gases and liquids occurs more or less at all solid surfaces, a well-known case in point being the adsorption of moisture by glass surfaces, but 1 Proc. Roy Soc., 1910, 84, A, 99. 2 Zeitsch. physikal Chem., 1910, 74, 641. 330 OUTLINES OF PHYSICAL CHEMISTRY it is only when the surface is very large in comparison with the weight of the solid as in the case of porous and finely divided substances that it can readily be measured. We have now to consider why the concentration in the surface layers differs in many cases so greatly from that in the main bulk of the liquid or gas phase. It seems probable at the outset that this must be connected with molecular attraction at the boundary of the phases, in other words with the surface tension (p. 129) and the connection between surface tension and adsorption has been deduced theoretically by Willard Gibbs and by J. J. Thomson. From the general standpoint we must assume that not only increased concentration, but in certain systems a lowering of concentration at the surface, as compared with that in the main bulk of liquid, may occur. Calling an increase of concentration positive adsorption and a diminution negative adsorption, the rule may be expressed as follows : l A dissolved substance is positively adsorbed when it lowers the surface tension^ negatively adsorbed when it raises the surface tension. The first case is met with in most solutions of organic compounds ; the second in solutions of highly ionised inorganic salts. Further Illustrations of Adsorption One very impor- tant process in which adsorption plays a prominent part is the dyeing of fibres such as wool and silk. Whether dyeing is purely an adsorption phenomenon or whether chemical action also plays a part has given rise to a great deal of discussion, and is by no means finally settled. It has recently been shown that the distribution of crystal violet, new magenta and patent blue between wool, silk and cotton on the one hand and water on the other is satisfactorily represented by the adsorption formula, and the value of the exponent */ is approximately the same as when charcoal is used as absorbent, a result which supports the adsorption theory. On the other hand, Knecht showed some years ago that when the basic dye crystal violet 1 Cf. Freundlich, Kapillarchemie., p. 52. COLLOIDAL SOLUTIONS. ADSORPTION 331 (the hydrochloride of an organic base) is shaken up with wool or silk the dye is decomposed, the cation combining with the fibre and the anion (in this case Cl') remaining in the solution. This result was first described as a case of double decomposi- tion between the dye and the fibre, the dye combining with an organic acid in the fibre to form a salt, and ammonia originally associated with the fibre combining with the chlorine to form ammonium chloride. Freundlich and Neumann l have shown, however, that in certain cases at least the chlorine is not left in the solution as a salt, but in the form of hydrochloric acid. The exact form in which the adsorbed dye occurs on the adsorb- ent does not seem to have been properly established the colour appears to indicate that it is present as a salt and not as the free base. The process just described would at first sight appear to be an ordinary chemical change, but further investigation shows that charcoal and even glass pellets split up dyes in an exactly analogous way, the cation being adsorbed and the anion re- maining in solution. It can scarcely be supposed that the charcoal or the glass enter into chemical action with the dyes. Phenomena of an exactly similar nature have already been met with in connection with the precipitation of colloids by electro- lytes (p. 319), and it has been shown that they are connected with the electrical character of the colloidal particles, that ion being most largely adsorbed which carries a charge of opposite sign to that on the colloid. The splitting of basic dyes de- scribed in the present section might be accounted for on similar lines, as also the well-known fact that an "acid" fibre adsorbs more particularly basic dyes and a "basic'' fibre "acid" dyes. The above is a brief outline of the adsorption theory of dyeing, but the process in any particular case is doubtless complicated by other factors, and at present is far from being understood. It has been suggested by Bayliss and others that adsorption 1 Zeitsch. physikal Chem., igog, 67, 538. 332 OUTLINES OF PHYSICAL CHEMISTRY plays an important part in enzyme reactions; the substance acted on is first adsorbed by the colloidal enzyme particles and chemical change follows. The interesting fact that colloids such as gelatine increased the stability of suspension colloids such as silver bromicje or colloidal gold towards electrolytes, may also be accounted for on the basis of adsorption. In the case under consideration it is assumed that the gelatine is ad- sorbed as a thin film on the surface of the particles, so that the latter do not come directly in contact with the electrolyte. It has quite recently been shown that certain dyes, more parti- cularly erythrosine, also exert a protective action on colloidal silver bromide. Substances acting in this way are termed " protective " colloids. CHAPTER XIII THEORIES OF SOLUTION General The nature of solutions, 1 more particularly as regards the connection between their properties and those of the components, has long been one of the most important problems of chemistry. It was early ** recognized that the properties of a solution are very seldom indeed the mean of the properties of the components, as must necessarily be the case if solvent and solute exert no mutual influence. Thus we know that when two liquids are mixed either expansion or contraction may occur, the boiling-point of a mixture may be higher or lower than those of either of its components (p. 88), and a mixture of two liquids may have a high conductivity, although the components in the pure condition are practically non-conductors (p. 259). The most obvious way of accounting for observations of this nature is to assume that they are connected with the formation of chemical compounds between the two components of the solution. As a matter of fact, explanations of the observed phenomena on these lines were formerly in great favour. As water was the substance most largely used as a component of solutions (as solvent), the explanation of the properties of aqueous solutions on the basis of formation of chemical com- pounds between water and the solute was termed the hydrate theory of solution. This theory appeared the more plausible 1 For simplicity, only mixtures of two components will be considered in this chapter. 333 334 OUTLINES OF PHYSICAL CHEMISTRY as a very large number of hydrates compounds of substances, more particularly salts, with water are known in the solid state, thus showing that there is undoubtedly considerable chemical affinity between certain solutes and water. In spite of the plausible nature of the hydrate theory, how- ever, it did not prove very successful in representing the properties of aqueous solutions, and some . facts were soon discovered in apparent contradiction with it. Thus, as already mentioned, Roscoe showed that the composition of the mixture of hydrochloric acid and water with minimum vapour pressure, alters with the pressure, and therefore could not be connected with the formation of a definite chemical compound of acid and water, as had previously been assumed (p. 90). The development of the electrolytic dissociation theory, which has been discussed in the previous chapters, led to a considerable change of view with regard to the influence of the solvent on the properties of aqueous solutions. The pro- perties of the solvent were to some extent relegated to the background, 1 and it was looked upon simply as the medium in which the molecules and the ions of the solvent the really active things moved about freely. The fact that such great advances in knowledge have been made by working along those lines naturally goes far to justify the method of procedure. Within the last few years, however, mainly as a result of the investigation of solutions in solvents other than water, it has come to be recognized that the solvent may play a more direct part in determining the properties of dilute solutions than some chemists were formerly inclined to suppose. Although the main properties of aqueous solutions can be accounted for without express consideration of affinity between solvent and solute, it appears probable that the latter effect must be taken into con- x The properties of the solvent are, of course, all-important in deter- mining whether a substance becomes ionised or not. But it was pot found necessary to take the question of affinity into account directly, and the equations representing ionic equilibria did not contain any term referring directly to the solvent. THEORIES OF SOLUTION 335 sideration in order to account for certain secondary phenomena (and possibly also in connection with ionisation) (p. 344). In the previous chapters the evidence in favour of the electrolytic dissociation theory could not be dealt with as a whole, owing to the fact that it belongs to different branches of the subject. In the present chapter a short summary of the more important lines of evidence bearing on the theory will be given, and then a brief account of the investigation of solutions in solvents other than water. Finally, after dealing with the older hydrate theory of solution, the possible mechanism of electrolytic dissociation will be considered. Evidence in Favour of the Electrolytic Dissociation Theory The evidence in favour of the electrolytic dissociation theory is partly electrical and partly non-electrical. The non- electrical evidence goes to show that there are more particles in dilute solutions of salts, strong acids and bases, than can be accounted for on the basis of their ordinary chemical formulae, and that in dilute solution the positive and negative parts of the molecule behave more or less independently. The electrical evidence goes to show that the particles which result from the splitting up of simple salt molecules are associated with electric charges, either positive or negative. The main points are as follows : (a) If Avogadro's hypothesis applies to dilute solutions, gram-molecular (molar) quantities of different substances, dis- solved in equal volumes of the same solvent, must exert the same osmotic pressure. As a matter of experiment, salts, strong acids and bases exert an osmotic pressure greater than that due to equivalent quantities of organic substances (p. 124). The electrolytic dissociation theory accounts for this on the same lines as the accepted explanation for the abnormally high pressure exerted by ammonium chloride ; it postulates that there are actually more particles present than that calculated according to the ordinary molecular formula. (b] Many of the properties of dilute salt solutions are additive, 336 OUTLINES OF PHYSICAL CHEMISTRY that is, they can be represented as the sum of two independent factors, one due to the positive, the other to the negative part of the molecule. This is true of the density, the heat of formation of salts (p. 148), the velocity of the ions (p. 251), the viscosity, and more particularly of the ordinary chemical reactions for the "base" and "acid" as used in analysis (p. 306). A very striking illustration of the independence of the pro- perties of one of the ions in dilute solution on the nature of the other is the colour of certain salt solutions, investigated by Ostwald. He examined the solutions of a large number oi metallic permanganates, and found that all had exactly the same absorption spectra. This is exactly what is to be expected according to the electrolytic dissociation theory, the effect being exerted by the permanganate ion. Similarly, salts of rosaniline with a large number of acids in very dilute solution gave identical absorption spectra (due to the rosaniline cation) but rosaniline itself, which is very slightly ionised, gave a quite different spectrum. Too much stress should not be laid on this criterion, how- ever, as certain properties, e.g., molecular volumes of organic compounds (p. 61) and the heat of combustion of hydro- carbons (p. 148), are more or less additive, although nothing in the nature of ionisation is here assumed. (c) The magnitudes of the degree of dissociation, calculated on two entirely independent assumptions (i) that the con- ductivity of solutions is due to the ions alone, and not to the non-ionised molecules or to the solvent; (2) that the abnormal osmotic pressures shown by aqueous solutions of electrolytes are due to the presence of more than the calculated number of particles owing to ionisation show excellent agreement (p. 263). (d) The heat of neutralization of molar solutions of all strong monoacidic bases by strong monobasic acids is 13,700 calories, in excellent agreement with the value for the reaction H- + OH' = H 2 O, calculated by van't Hoffs formula from THEORIES OF SOLUTION 337 Kohlrausch's measurements of the change of conductivity of pure water with the temperature (p. 295). (e) The results obtained by four entirely independent methods for the degree of ionisation of water are in striking agreement, in spite of the fact that the assumed ionisation is very minute (p. 294). (/) The formula for the variation of electrical conductivity with dilution, obtained by application of the law of mass action to the assumed equilibrium between ions and non-ionised mole- cules in solution, represents the experimental results in the case of weak electrolytes with the highest accuracy (p. 267). (g) As shown in the next chapter, our present views as to the origin of differences of potential at the junction of two solutions, or at the junction of a metal and a solution of one of its salts, are based on the osmotic and electrolytic dissocia- tion theories, and the good agreement between observed and calculated values goes far to justify the assumptions on which the formulae are based. Many other illustrations of the utility of the electrolytic dissociation theory are mentioned throughout the book. Ionisation in Solvents other than Water 1 In ac- cordance with the mode in which the subject has developed, we have up to the present been mainly concerned with aqueous solutions, and the justification for this order of treatment is that the relationships in aqueous solution are often very simple in character, as shown in detail in the last chapter. The importance of a theory would, however, be much less if it only applied to aqueous solutions, and it is therefore satisfactory that in recent years a very large number of liquids, both organic and inorganic, have been employed as solvents. Although the progress so far made in this branch of know- ledge is not great, the available data appear to ' show that 1 Carrara, Ahrens' Sammlung, 1908, 12, 404. 22 OUTLINES OF PHYSICAL CHEMISTRY the rules which have been found to hold for aqueous solutions also apply to non-aqueous solutions 1 Some solvents, such as ethyl and methyl alcohol, acetic acid, formic acid, hydrocyanic acid and liquefied ammonia, form solu- tions of fairly high conductivity with salts and other substances ; these are termed dissociating solvents (p. 123). Solutions in certain other solvents, such as benzene, chloroform and ether, are practically non-conductors, and the solutes are often present in such solutions in the form of complex molecules. These solvents are therefore often termed associating solvents, but it is not certain whether they actually favour association or polymerization of the solute, or have only a slight effect in simplifying the naturally polymerized solute. It is natural to inquire whether there is any connection between the ionising power of a solvent and any of its other properties. It has been found that as a general rule those solvents with the greatest dissociating power have high dielectric constants (p. 225) (J. J. Thomson, Nernst, 1893). This observation is easily understood when it is remembered that the attraction between contrary electric charges is inversely proportional to the dielectric constant of the medium ; it is evident that the existence of the ions in a free condition must be favoured by diminishing the attraction between the contrary charges. The dielectric constants of a few important solvents (liquids and liquefied gases) at room temperature are given in the table. Solvent. D.C. Solvent. D.C. Hydrocyanic acid 95 Acetone 21 Water . . 81 Pyridine 2O Formic acid 57 Ammonia 16-2 Nitro benzene . 36-5 Sulphur dioxide 137 Methyl alcohol . . 32-5 Chloroform 5' 2 Ethyl alcohol . . 21-5 Benzene 2 '3 1 C/. Walden, Zeitsch. physikal. Chem., 1907, 58, 479. THEORIES OF SOLUTION 339 The data are not usually available for an accurate comparison of the dissociating power of a solvent with its dielectric constant, as the values of //,oo for electrolytes in solvents other than water have been determined in only a few cases. It is important to remember that a comparison of the conductivities of solutions of the same concentration in different solvents is in no sense a measure of the respective ionising powers of the solvents, as the conductivity also depends on the ionic velocity (p. 252). The available data are, however, sufficient to show that although there is parallelism, there is not direct proportionality between dielectric constant and ionising power. There appears also to be some connection between the degree of association of the solvent itself and its ionising power. The examples already given show that water, the alcohols and fatty acids, which are themselves complex, are the best ionising solvents. There are, however, exceptions to this as to all other rules in this section ; liquefied ammonia, though apparently not polymerized, is a good ionising solvent. Briihl has suggested that the ionising power of a solvent depends on what he calls subsidiary valencies (the "free affinity " of Armstrong) ; in other words, the best ionising solvents are those which are unsaturated. It is by no means improbable that the dielectric constant, the degree of poly- merization, and the degree of unsaturation of a solvent are in some way connected. The ionising power of a solvent may be partly of a physical and partly of a chemical nature. The effect of a high dielectric constant would appear to be mainly physical, on the other hand, if the effect of a solvent depends on its unsaturated character, it would most likely be chemical in character. The Old Hydrate Theory of Solution 1 As already men- tioned, attempts have been made to account for the properties of aqueous solutions of electrolytes on the basis of chemical combination between solvent and solute. Among those who 1 Pickering, Watts's Dictionary of Chemistry, Article Arrhenius, Theories of Chemistry (Longmans, 1907), chap. iii. 340 OUTLINES OF PHYSICAL CHEMISTRY have supported this view of solution, the names of Mendeleeff, Pickering, Kahlenberg l and Armstrong 2 may be mentioned. Mendeleeff made a number of measurements of the densities of mixtures of sulphuric acid and water, and drew the con- clusion that the curve representing the relation between density and composition is made up of a number of straight lines meeting each other at sharp angles, the points of discontinuity corresponding with definite hydrates, for example, H 2 SO 4 , H 2 O ; H 2 SO 4 , 2H 2 O ; H 2 SO 4 , 6H 2 O and H 2 SO 4 , i5oH 2 O. Pickering repeated Mendeleeff's experiments, and found no sudden breaks in the density curve, but only changes in direction at certain points. He also drew the conclusion that these points cor- respond with the composition of definite compounds of the acid and water. In this connection it may be recalled that the curve obtained by plotting the electrical conductivity of mixtures of sulphuric acid and water against the composition (p. 259) shows two dis- tinct minima, at 100 per cent, and 84 per cent, of sulphuric acid respectively, corresponding with the compounds H 2 SO 4 (SO 3 , H 2 O) and H 2 SO 4 , H 2 O respectively. As it is a general rule that the electrical conductivity of pure substances is small, there is little reason to doubt that the 84 per cent, solution consists mainly of the monohydrate H 2 SO 4 , H 2 O. The con- tention of Mendeleeff and Pickering, that aqueous solutions of sulphuric acid contain compounds of the components, is thus partially confirmed by the electrical evidence. There is not much reason to doubt the truth of the first postulate of the hydrate theory, that in many cases hydrates are present in aqueous solution. The hydrates are, however, in all probability more or less dissociated in solution, and it will not usually be possible to determine the presence of definite hydrates from the measurement of physical properties. 1 For a summary of Kahlenberg's views on Solution, see Trans. Faraday Soc., 1905, I, 42. 2 Proc. Roy. Soc., 1908, 81 A, 80-95. THEORIES OF SOLUTION 341 It is probable that in general the equilibria are somewhat com- plicated, and are displaced gradually by dilution in accordance with the law of mass action, which accounts for the experimental fact that in general the properties of aqueous solutions alter continuously with composition. Having proved the existence of hydrates in salt solutions in certain cases, Pickering l attempted to account for the properties of aqueous solutions (osmotic pressure, electrical conductivity, etc.) on the basis of association alone, but as his views have not met with much acceptance, a reference to them will be sufficient for our present purpose. Kahlenberg, 2 who has carried out many interesting experiments in solvents other than water, re- gards the electrolytic dissociation theory as unsatisfactory, and considers that the process of solution is one of chemical com- bination between solvent and solute. Armstrong has also attempted to account for the properties of aqueous solutions on the basis of association between solvent and solute. 3 Although, as we have seen, cases are known in which a maximum or minimum or a change in the direction of a curve may correspond more or less completely with the formation of a compound between the two components of a homogeneous solution, this does not by any means always hold. It has already been pointed out that the curve representing the varia- tion of the electrical conductivity of mixtures of sulphuric acid and water with the composition has a maximum at 30 per cent, of acid (p. 2^9). As the pure liquids are practically non- conductors, whilst the mixtures conduct, there must necessarily be a concentration, between o and 100 per cent, acid, at which the conductivity attains a maximum value. This maximum will clearly have no reference to the formation of a chemical compound between sulphuric acid and water, since this would tend to diminish the conductivity. Similar considerations appear to apply for other physical l Loc. cit. z Loc. cit. 3 Loc. cit., also Encyc. Britannica, loth Edition, vol. xxvi., p. 741. 342 OUTLINES OF PHYSICAL CHEMISTRY properties which attain a maximum value for binary mixtures. The curve representing the variation of the viscosity (internal friction) of mixtures of alcohol and water with composition shows a maximum at o for a mixture containing 36 per cent, of alcohol, corresponding with the composition (C 2 H 5 OH) 2 , 9H 2 O, and it has therefore been suggested that the solution consists mainly of this hydrate. At 1 7, however, the mixture of maximum viscosity contains 42 per cent., and at 55 rather more than 50 per cent, of alcohol. The last-mentioned mixture corresponds with the composition (C 2 H 5 OH) 2 , 5H 2 O. If we accept the association view of this phenomenon, it must be assumed that at o the solution contains a hydrate (C 2 H 5 OH) 2 , 9H 2 O, and at 55 a hydrate (C 2 H 5 OH) 2 , 5H 2 O, and that at intermediate temperatures the hydrates with 6, 7 and 8 H 2 O exist which does not appear very probable. Now, Arrhenius has shown that as a general rule the addition of a non-electrolyte raises the viscosity of water. Therefore, if the viscosity of the non-electrolyte is less than, or only slightly exceeds that of water, the curve obtained by plotting viscosity against the composition of the mixture must necessarily attain a maximum at some intermediate point. Why mixtures of two liquids have often a higher viscosity than either of the pure liquids is not known, no general agreement having yet been reached on this and allied questions. 1 Meohanism of Electrolytic Dissociation. Function of the Solvent The fundamental difference between associa- tion theories of solution, as discussed in the last section, and the electrolytic dissociation theory is that the advocates of association entirely reject the postulate of the independent existence of the ions. As, however, the different theories of association unaccompanied by ionisation have so far proved quite inadequate to account quantitatively for the behaviour of aqueous solutions, whilst the electrolytic dissociation theory not only affords a satisfactory quantitative interpretation of the 1 Compare Senter, Proc. Chem. Soc., 1909, 292. For evidence in favour of the association view of this phenomenon, compare Dunstan, Trans. Chem. Society, 1907, 91, 83; Dunstan and Thole, ibid., 1909, 95, THEORIES OF SOLUTION 343 more important phenomena observed in solutions of electrolytes (chap, x.), but has led to discoveries of the most fundamental importance for chemistry, it is not surprising that the electro- lytic dissociation theory has now met with practically universal acceptance. It is very likely that as a result of further investi- gation the theory may require modification in some subsidiary respects, but its general validity appears no longer doubtful. We are now in a position to discuss the possible mechanism of electrolytic dissociation, /. /, the metal sends ions into the solution until the accumulated electrostatic charges prevent further action ; the metal is then negatively and the solution positively charged. (b) If P < /, the positive ions from the solution deposit on 360 OUTLINES OF PHYSICAL CHEMISTRY the metal until the electrostatic charges prevent further action ; the metal is then positively and the solution negatively charged. (c) \f P = /, no change occurs, and there is no difference of potential between metal and solution. As will be shown later, the solution pressures of the different metals are very different. Those of the alkali metals, zinc, iron, etc., are so great that they always exceed the osmotic pressures of their respective solutions- (which cannot be increased beyond a certain point owing to the limited solubility of the salts), and these metals are, therefore, always negatively charged with - Metal -h 4- + + Solution. Solu Metal tion. f Metal - - . Solution. p=p. p-=p. FIG. 38. reference to their solutions. On the other hand, the solution pressure of mercury, silver, copper, etc., is so small that they become positively charged, even in very dilute solutions of their respective salts. Calculation of Electromotive Forces at a Junction Metal/Salt Solution Provided that the changes at the junction of an electrode with a solution are reversible, the E.M.F. at the junction can readily be calculated in terms of the solution pressure, P, of the metal and the osmotic pressure, p, of the solution. This can perhaps be done most simply by calculating the maximum work obtainable when a mol of ELECTROMOTIVE FORCE 361 the electrode metal is brought from the pressure P to the lower pressure /, (i) osmotically, (2) electrically. If a mol of a dissolved substance is brought reversibly from the pressure P to/ the work gained (in this case the osmotic work) is (cf. p. 135) Further, the dissolving of i equivalent of a metal is associated with 96,540 coulombs, and that of a mol of a metal of valency n with 96,540 n coulombs. The work done is the product of the E.M.F. E in volts and the quantity of electricity, 96,540 n coulombs. Equating the osmotic and electrical work, we have n 96,540 E = RTlog e P// RT . P , . or E = - log*-; (i) 96,540^ 6 V In order to obtain E in volts, R must be expressed in electrical units (volt-coulombs). If, at the same time, the change is made to ordinary logarithms (by multiplying by 2*3026) the above equation becomes 2*3026 x 1*99 x 4*183 T P 0*0001983 T P 96,540* gl 7 = ~^~ logl< 7 The numerical values of 2*3026 RT/Fat o, 18, 25 and 30 are as follows : Absolute temperature 273 273 + 18 273 + 25 273 + 30 Value of 2*3026 RT/F o'o54i o'577 '59i 0-0601 At room temperature (15-20) the value of the expression in question is about 0*058, and the general formula becomes which should be remembered. It is clear from the form of the above equation that a tenfold increase or decrease in the osmotic pressure of the ions of the metal will produce a change of E.M.F. of 0*058 volts for a univalent metal, and o'o$8/n volts for a w-valent metal, at room temperature. 362 OUTLINES OF PHYSICAL CHEMISTRY Differences of Potential in a Yoltaic Cell Two such electrodes as have just been described may be combined together to form a voltaic cell. This may be done in many ways, but a convenient arrangement is that for the Daniell cell represented in Fig. 39. in which the solutions are separated by a porous partition, A, which prevents convection, but allows the current to pass. When the poles are placed in the respec- tive solutions, the zinc becomes negatively charged, since P x > p l ; on the other hand, the copper becomes positively charged as/ 2 >P 2 . As already explained, the solution and precipita- tion soon come to a standstill because of the accumulation of electrostatic charges. If, however, the elec- trodes are connected by a wire, the contrary charges neutralize each other through the wire, and in the solution more metal can then be dissolved and de- posited respectively (as there are no longer any opposing forces), the corresponding charges are again neutralized, and so on. The neutralization of charges through a conductor corresponds with the passage of a current. The general question as to the seat of the E.M.F. in such a cell as the Daniell has now to be considered. If the poles of the cell are connected by a wire of metal M, there are no less than five junctions at which there may be contact differences of potential ; two metallic junctions, Zn/M and M/Cu, two metal/ solution junctions, Cu/CuSO 4 and Zn/ZnSO 4 , and one liquid junction, ZnSO 4 /CuSO 4 . The question as to whether there are contact differences of potential at the junction of two metals gave rise to great difference of opinion, and the controversy Zh / X Cu 3d ^f + + ^ mm +~ _. _ _=: -r ~z, ^SO 4 " +- C ~^0 4 FIG. 39. ELECTROMOTIVE FORCE 363 lasted the greater part of last century. It is now generally agreed, however, that if there are such differences they are exceedingly small in comparison with those of the junctions metal/salt solution. The difference of potential at the liquid junction is of much more importance and can be calculated by Nernst's theory (p. 384). It also is small in comparison with those at the liquid/metal junctions, and mav therefore, be left out of account for the present. The distribution of differences of potential in the Daniell cell with open circuit is represented in Fig. 40 (a), the ordi nates Cu f o n-Cu SQ n-Zn FIG. 40. representing the potentials of the different parts of the circuit. The horizontal lines, AB, CD, DE and FG, illustrate the very important fact that the copper, the zinc and the solutions are each of a definite constant potential, and the ordinates, BC and EF, that there are sudden alterations of potential at the junc- tions metal/solution. For simplicity the solutions of zinc sulphate and copper sulphate are represented as being at the same potential, which is only approximately true. It is as- sumed for the present that the difference of potential be- tween copper and N copper sulphate solution is 0-585 volts, the copper being positive, and that the potential difference, Zn/ZnSO 4 , is 0^52 volts, the metal being negative. The 364 OUTLINES OF PHYSICAL CHEMISTRY total difference of potential between zinc and copper on open circuit is thus 0-585 + 0*52 = 1*105 volts. When the circuit is closed by connecting the copper and zinc by a wire of fairly high resistance, R, the distribution of poten- tial in the cell is as shown in Fig. 40 (ft). The sudden changes of potential at the junctions ZnSO 4 /Zn and CuSO 4 /Cu are of the same magnitude as before, but the difference of potential between the zinc and copper, measured by the vertical height, AG, is much less than on open circuit. This is owing to the fall of potential in the cell owing to the resistance of the elec- trolyte, so that the solution in contact with the zinc is at a higher potential than that in contact with the copper, as repre- sented by EDC. If C is the current passing through the cell, and r is the resistance of the electrolyte, the E.M.F. of the cell on closed circuit is given by E = CR + Cr, and CR, the fall of potential in the external wire (represented in the figure by the vertical distance AG), approaches the more nearly to the E.M.F. of the same cell on open circuit the greater R is compared with r (compare p. 355). The E.M.F. of such a combination as the Daniell cell is the algebraic sum of the E.M.F.s at the two junctions, and is represented by the formula Where P x and P 2 are the solution pressures of zinc and copper respectively, p^ represents the osmotic pressure of the zinc ions in the solution, and / 2 that of the copper ions. The values of pi and / 2 are therefore known, but the absolute values of the solution pressures P x and P 2 are unknown. The sign of E 2 is due to the fact that at that junction ions are leaving the solution. In obtaining E as the algebraic sum of the differences of potential E l and E 2 at the two junctions, it is naturally of the utmost importance to take the values of E x and E 2 with their proper sign. Perhaps the best method of avoiding errors in this ELECTROMOTIVE FORCE S 6 5 connection is to consider the tendency of one kind of electricity, say positive electricity, to pass round the circuit. In going round the circuit in the Daniell cell, starting with the zinc, the different junctions are met with in the order Zn | ZnSO 4 | CuSO 4 | Cu 0-52 0-585 > 1*105 and this is a very convenient method of representing the Daniell or any other cell. Now at the junction Zn/ZnSO 4 positive electricity tends to pass from zinc to solution at a potential (pressure) of 0*52 volts, as indicated by the arrow. Further, as the osmotic pres- sure of Cu" ions in copper sulphate solution is greater than the solution pressure of copper, positive electricity tends to pass across the junction CuSO 4 /Cu, in the direction of the arrow at an E.M.F. of 0-585 volts. It is clear that the forces at the two poles are in the same direction, and therefore positive electricity tends to pass through the solution in the direction indicated by the lower arrow at a total E.M.F. of 0*520 + 0-585 = 1-105 volts. Further illustrations are given at a later stage. Influence of Change of Concentration of Salt Solution on the E.M.F. of a Cell The general equation just given may be written in a slightly different form by substituting for the pressures the corresponding concentrations. Considering first the solution pressure, P lf of the zinc, it is theoretically possible to choose a Zn" ion concentration, C lf such that its osmotic pressure will just balance the solution pressure of the metal ; this may be substituted for P 1 in the general equation. Similarly, for p v the osmotic pressure of the zinc ions in the solution, we may substitute the corresponding concentration, c^ Dealing in the same way with the copper side of the cell, the equation for the Daniell cell (or any other cell of similar type) becomes 366 OUTLINES OF PHYSICAL CHEMISTRY C C v^i i V-/r In this form the general equation may be employed to in- vestigate the question as to how the E.M.F. of the cell is affected by varying the concentration of the salt solutions. For the zinc side, since C x is greater than c lt it is clear that the quotient Cj/^, and therefore E lf is increased by diminish- ing c lt the concentration of the Zn" ions. For the copper side, however, as C 2 is less than c% (p. 342), the quotient C 2 /^, therefore E 2 , will evidently be diminished by diminishing the copper sulphate concentration. The general rule with re- gard to the influence of change of ionic concentration on the E.M.F. of a cell may be expressed as follows : Diminishing th& concentration of a solution from which ions are separating lowers, and diminishing the concentration of a solution into which new ions are going increases, the E.M.F. of a cell. It is evident from general principles that the effect must be as described ; in the first case, the tendency to the separation of ions is lessened, and the E.M.F. falls ; in the second case, the entrance of new ions is facilitated, and the E.M.F. increases. If the concentration of the Or* ions in the solution is pro- gressively diminished, a point must be reached at which the solution pressure of the metal is just balanced by the osmotic pressure of the Cu- ions. If the concentration is still further diminished, the tendency for copper - to pass into solution will steadily increase, and ultimately may become greater than the tendency of zinc to pass into solution. It should therefore be theoretically possible to reverse the direction of the current in the Daniell cell by sufficiently diminishing the Cu" ion con- centration, and this state of affairs can be realised experimentally by adding potassium cyanide to the copper sulphate solution. A further important deduction can also be drawn from the general equation. As c and c^ stand for the concentration of the positive ions in the solution, the E.M.F. of the cell should be independent of the nature of the negative ion, pro- ELECTROMOTIVE FORCE 367 vided that the salts are equally ionised. This consequence of the theory is completely borne out by experiment. For twenty- one different thallium salts, in N/5o solution, the difference of potential between metal and solution varied only from 0*7040 to 0-7055 volts, the slight variations being readily accounted for by differences in the degree of ionisationr. Concentration Cells We have now to consider what are termed " concentration cells," cells in which the E.M.F. de- pends essentially on differences of concentration. In some respects, concentration cells are simpler than those of the Daniell type, which have so far been considered. Concentration cells may be divided into two main classes (a) Those in which the solutions (and therefore the active ions) are of different concentrations. (b) Those in which the electrode materials yielding the ions are of different concentrations. (a) Concentration Cells with Solutions of Different Concen- trations As a type of the elements in question, we will con- sider a cell in which silver electrodes dip in solutions of silver nitrate of different concentrations, c l and c The arrange- ment for the practical determination of the total E.M.F. of such a combination is shown in Fig. 41, where A and B repre- sent the cells containing the silver nitrate solutions and the vessel C contains an indifferent electrolyte. As this form of cell is largely employed in measurements of E.M.F., it may be well to describe it fully. It consists of a glass tube 3-4 cm. wide, with a straight side-tube D on one side and a bent side- tube E on the other, the latter being employed for making con- nection with the indifferent electrolyte in C as shown. Into the lower end of a glass tube, F, is cemented a thick rod of silver covered with the finely-divided metal by electrolysis, and the glass tube is held by a cork closing the cell. The cell is filled with a solution of silver nitrate of definite strength through the bent tube by suction through the straight side-tube, D, which is then closed by a clip. The other " half-cell," B, is prepared 368 OUTLINES OF PHYSICAL CHEMISTRY in exactly the same way, but contains a solution of silver nitrate of different concentration. The ends of the bent tubes are then dipped into an indifferent electrolyte in the vessel, C, as shown, and the total E.M.F. of the combination determined by the potentiometer method in the usual way, connection with the silver electrodes being made by wires passing down the interior of the glass tubes. In this case, the general equation for an electrolytic cell, simplifies to E = 0- (0 FIG. 41. since C, the solution pressure of the metal, is the same on both sides, and is therefore eliminated. A cell of the type Ag I AgNO 3 dil AgNO 3 conc Ag works in such a way that silver is deposited from the more concentrated solution, in which the osmotic pressure is higher, and is dissolved at the pole in contact with the weaker solution, which offers less resistance to the entrance of Ag 4 ions. The ELECTROMOTIVE FORCE 369 change, therefore, proceeds in such a way that the differences of concentration tend to equalize, and when the solutions have reached the same concentration, the current stops. Positive electricity therefore passes in the element from the weak to the strong solution, as indicated by the arrow, and in the connecting wire from the strong to the weak solution ; the electrode in contact with the strong solution becomes positively charged, the other electrode negatively charged. The equation shows that the E.M.F. of such a concentra- tion cell depends only on the respective concentrations of the positive ions in the two solutions and their valency, and not on the nature of the electrodes or on the nature of the anions, and the experimental results are in full accord with this deduction. Otherwise expressed, the E.M.F. of any element made up of a univalent metal M dipping in solutions of one of its salts of different concentration is of the same absolute value as that of the silver concentration cell, provided that the solutions are of corresponding concentration, and ionised to the same extent. Further, if the solutions are dilute, and electrolytic dissociation therefore fairly complete, the ratio of the ionic concentrations in different dilutions will be approximately the same as the ratio of the concentrations themselves. Thus, in the example under consideration, the ratio c^c^ for i/ioo molar, and i/iooo molar solutions, will be approximately 10 : i ; log^/^ is therefore i, and the value of E for the cell Ag I AgN0 3 | AgN0 3 I Ag j m/iooo j m/ioo \ is 0*05 S/n = 0*058 volts, since n, the valency of the ions con- cerned, is unity. If, however, the solutions are more concentrated, the fact that ionisation is incomplete must be taken into account in calculating the E.M.F. of a cell. Suppose, for instance, it is required to calculate the E.M.F. of the cell Ag I AgNO 3 m/ioo \ AgNO 3 tn/io \ Ag. 24 370 OUTLINES OF PHYSICAL CHEMISTRY N/io silver nitrate solution is ionised to the extent of 82 per cent, at 18, whence c^ = 0*082, and N/ioo silver nitrate to the extent of 94 per cent., whence q = 0*0094. We have therefore c^c^ = 0*082/0*0094 = 872, and E = 0*054 volts, in excellent agreement with the experimental value. Strictly speaking, it is not justifiable in cells of this type to neglect the contact difference of potential between the two solutions, which may amount to a considerable fraction of the total E.M.F. The accurate formula for the calculation of the E.M.F. of cells of this type is given in a succeeding section (p. 384). If, however, both solutions contain an indifferent electro- lyte in equivalent concentration great in comparison with those of the active salt, the difference of potential at the liquid junction becomes negligible, and the above formula (i) holds accurately (cf. p. 383). It is evident from the formula that the E.M.F. of a con- centration cell cannot be greatly altered by increasing the con- centration on one side, owing to the limited solubility of the salts used as electrolytes. On the other hand, the E.M.F. may be greatly altered by diminishing the ionic concentra- tion on one side. Conversely, when a cell is made up with a solution of silver nitrate of known Ag* ion concentration, t lt and one of unknown concentration, c , and the E.M.F. of the cell is measured, c can readily be calculated. This principle has been applied more particularly for the determination of very small ion concentrations, and may be illustrated by the determination of the Ag* ion concentration in a saturated solution of silver iodide. When the concentration on one side is very small, it is usual to add some salt, with or without a common ion, to eliminate the potential difference at the liquid junction, and also to increase the conductivity in the cell, so as to render the measurements more accurate. In this case potassium nitrate may conveniently be used. The observed E.M.F. of the cell Ag | KNO 3 + Agl | AgNO 8 o'ooim + KNO 3 1 Ag ELECTROMOTIVE FORCE 371 is 0*22 volts. Since c^ = 0*001, we have E = 0-22 = 0-058 Iog 10 (o -oo i /<:<,), whence c = 1*6 x io~ 8 . In other words, a litre of a saturated solution of silver iodide contains i'6 x io~ 8 mol of silver iodide, in excellent agreement with the value, 1-5 x io~ 8 mol, obtained from conductivity measurements (p. 301). (b) Cells with Different Concentrations of the Elec- trode Materials (Substances Producing Ions) Not only can concentration cells be obtained by employing different con- centrations of an electrolyte, but also by using different con- centrations of metals or other electrode materials yielding ions. The concentration of metals can for our present purpose be most satisfactorily varied by employing their solutions in mercury, the so-called amalgams. For example, a concentra- tion cell can readily be built up as follows : Zinc amalgam conc./zinc sulphate solution/ zinc amalgam dilute which differs from the cells of the first type in that the osmotic pressure of the zinc ions in contact with the two poles is the same, but the concentration, and therefore the solution pressure of the metal on the two sides, is different. The E.M.F. of a cell of this type is represented by the general formula (p. 361) Since the same solution (in this case zinc sulphate) is in contact with both electrodes, p =/ 2 , and the formula becomes On the assumption that Pj and P 2 , the solution pressure of the zinc in the concentrated and dilute amalgams respectively, are proportional to the respective concentrations, we obtain EJ 372 OUTLINES OF PHYSICAL CHEMISTRY which is exactly the same form' of equation as that for cells with different electrolyte concentrations. As the solution pressure of the zinc is higher in the con- centrated amalgam, it passes into solution from the latter and is deposited in the less concentrated amalgam, so that the con- centrations tend to become equal. It follows that positive electricity passes in the cell from the concentrated to the dilute amalgam, as shown by the arrow. As an illustration, the E.M.F. of a cell for which Cj = 0*14 mol and C 2 = 0*00214 mol of zinc per litre of amalgam at 23 may be calculated. If it be assumed that zinc is unimolecular when dissolved in mercury, n = 2, and -TV o'oooioSi x 296. 0*14 E = - Iog 10 = 0-053 volts, in excellent agreement with the observed value, 0-052 volts. So far, the possible effect of mercury on the potential has been disregarded, and this is justified by the excellent agreement between observed and calculated values for the E.M.F. on the assumption that mercury simply acts as an indifferent solvent. The explanation is that for a mixture of two metals it is the metal with the higher solution pressure that goes into solution, and mercury can consequently be used as solvent in potential measurements for any metal which is "less noble," /.*., which has a higher solution pressure than mercury itself. As indicated above, the E.M.F. of a metal dissolved in mer- cury depends on the concentration. The difference of potential between a saturated solution of a metal in mercury and an aqueous solution of one of its salts is the same as that between the salt solution and the pure metal, and even for dilute amal- gams the E.M.F. is not very different from that of the pure metal, as the example shows. On the other hand, the potential of a metal in chemical combination with a more noble metal may be quite different from that of the pure metal. The energy relations in concentration cells in which very dilute solutions are employed are remarkable. In the silver ELECTROMOTIVE FORCE 373 nitrate concentration cell described above, the change con- sisted simply in bringing Ag ions from the pressure /j to the lower pressure / 2 - When a perfect gas expands from the pressure / x to / 2 , no internal work is done, and this is the more nearly the case for ordinary gases the lower the pressures. In an exactly corresponding way no internal work will be done when a salt is further diluted in sufficiently dilute solution ; in other words, the heat of dilution will be zero. This means that the change of chemical energy' (Q in the Helmholtz formula), also termed the heat of reaction, is zero, so that the electrical energy obtained from a concentration cell with suffi- ciently dilute solutions does not come from a chemical change at all, but entirely from the surroundings. Under these circum- stances, as Q is zero, the Helmholtz formula simplifies to F T T J?T Electrodes of the First and Second Kind. The Calomel Electrode So far only electrodes which are reversible with regard to the positive ion have been considered; these are termed electrodes of the first kind. In an exactly similar way it is possible to construct electrodes which are reversible with regard to the negative ion these are termed electrodes of the second kind. They are prepared by immersing a metal in a saturated solution of one of its difficultly soluble salts, which solution also contains a salt with the same anion as the in- soluble salt. The E.M.F. of the electrode depends only on the concentration of the anion, since the concentration of all the other substances is constant. The most important electrode of this type is the calomel electrode, which consists of mercury in contact with solid mercurous chloride and a saturated solution of the latter salt in potassium chloride solu- tion as electrolyte. The calomel electrode is reversible with regard to Cl' ions, just as the Cu/CuSO 4 electrode is reversible with regard to Cu- ions. If positive electricity passes from 374 OUTLINES OF PHYSICAL CHEMISTRY metal to solution, the mercury combines with Cl' ions and calomel is formed; if passed in the reverse direction chlorine goes into solution and solid calomel disappears. The electrode, therefore, acts like a plate of solid chlorine, which gives up or absorbs the element depending on the direction of the current. As the tendency of Cl' ions to enter or leave the solution depends on the concentration of Cl' ions already present, the difference of potential between mercury and the solution must depend on the concentration of the potassium chloride solution used, as already pointed out. A normal solution is mostly largely employed. The calomel electrode is largely used as a normal electrode by means of which the E.M.F.s of other electrodes may be compared ; its chief advantage for this purpose is that it can readily be reproduced with an accuracy of about i millivolt. A convenient form of the electrode is shown in Fig. 42. A vessel of the type already described in connec- tion with concentra- tion cells (p. 347) may conveniently be used. A layer of dry mercury is first placed in the bottom of the FIG. 42. vessel, then a paste made by rubbing in a mortar mercury and calomel with some of the potassium chloride solution, and the vessel is then filled up with ^-potassium chloride solution ELECTROMOTIVE FORCE 375 which has previously been saturated with calomel by shaking with excess of the latter. Connection with the mercury may conveniently be made by means of a platinum wire sealed at the bottom into a glass tube A, the latter passing up through the rubber stopper closing the vessel. In making measure- ments, the bent side-tube, C, must also be filled with the potassium chloride solution. This is done by suction at the straight side-tube, B, which is then closed by a clip. For measuring the potential of another electrode by means of the calomel electrode, the arrangement already shown in Fig. 41 is used. Neglecting for the present the differences of potential at the liquid junctions, the E.M.F. of the combination in question is the algebraic sum of the differences of potential at the two metal/solution junctions. It follows that if the single potential difference between mercury and solution is known, the single potential difference at the other electrode can readily be cal- culated. Unfortunately no single potential difference is known with certainty (see next section), and it is, therefore, necessary to refer them to an arbitrary standard. Two such standards are in general use, (a) the so-called " absolute " standard ; (S) the hydrogen standard. As regards the first standard, Ostwald as- sumes that the potential difference between mercury and the solution in the normal calomel electrode is 0-560 volts at 18, the mercury being positive, and differences of potential referred to this standard are termed " absolute potentials," e c (see next section). On the other hand, Nernst refers E.M.F.s to the hydrogen standard, c h the difference of potential between a platinum electrode saturated with hydrogen and a solution of an acid normal with regard to H- ions being put equal to zero. The "absolute" potentials, referred to the calomel electrode, have a theoretical basis, and there is reason to suppose that the real, but at present unknown, single potential differences are not very different from the " absolute " potentials. Inde- pendently of this, however, the use of the calomel electrode in actual measurements is justified by the fact that it can be re- 376 OUTLINES OF PHYSICAL CHEMISTRY produced with a high degree of accuracy. The use of the hydrogen electrode as standard is purely arbitrary, as it is not pretended that the difference of potential between electrode and solution is actually zero, but the reference of potential differences to this standard has certain advantages. It is, in fact, usual to make the actual measurements with the calomel electrode, and then to refer them to the hydrogen standard, on the basis that when the hydrogen electrode is taken as zero the E.M.F. of the normal calomel electrode is + 0*283 volts; that of the electrode with N/ioKCl + 0-336 volts, at 18. In order to illustrate the use of the calomel electrode for potential measurements, the separate determination of the dif- ferences of potential metal/solution for the two parts of the Daniell cell will be considered. When the zinc electrode is combined with the calomel electrode, as shown in Fig. 41, to form the cell Zn i -080 the E.M.F. of the combination, as shown by potentiometer measurements, is 1-080 volts, the zinc being negative with regard to mercury, so that positive electricity flows in the cell from zinc to mercury, as indicated by the lower arrow. In order to obtain the potential difference Zn/ZnSO 4 , we proceed as follows (p. 365). It is known that mercury in contact with a solution of calomel becomes positively charged, and that for the calomel electrode the tendency for positive electricity to pass across the junction towards the mercury is 0*560 volts. The tendency for positive electricity to pass round the circuit is equivalent to 1-080 volts, hence the E.M.F. at the Zn/ZnSO 4 junction must act in the direction shown by the upper left-hancj -ZnSO 4 KC1 (in vessel C) Hg 2 Cl 2 in KC1 0*520 0-560 ELECTROMOTIVE FORCE 377 arrow, and is 1*080 -0*5 60 = '5 20 volts. In other words, the E.M.F. at the junction Zn/ZnSO 4 is 0-520 volts, the zinc being negatively charged. Similarly, the observed E.M.F. of the cell Cu | -CuS0 4 | KC1 | Hg 2 Cl 2 in -KCl | Hg < > 0-585 0-560 0*025 is 0-025 volts, the copper being positive with regard to mercury, hence positive electricity flows from mercury to copper in the cell, as indicated by the lower arrow. As far as the calomel junction is concerned, the tendency for positive electricity to flow round the circuit is equivalent to 0-560 volts towards the right, as indicated by the arrow. Hence in order that for the whole cell the tendency of positive electricity may be to flow towards the left at a potential of 0-025 v l ts tne E.M.F. at the Cu/CuSO 4 junction must act in the opposite direction to that at the calomel junction and exceed it by 0-025 volts. The E.M.F. at the junction Cu/CuSO 4 is therefore 0-585 volts and positive electricity flows from solution to copper, as indicated by the arrow. The total E.M.F. of the cell Zn/ZnSO 4 /CuSO 4 /Cu is, there- fore, -0-520 + ( 0-585)= 1*105 volts, which agrees with the value obtained by direct measurement (p. 34^). It is evident from the above that although the single potential differences at the junctions depend upon the value of the potential assumed for the standard, the E.M.F. of the complete cell does not depend upon the E.M.F. of the standard, which is eliminated. If referred to the hydrogen electrode as standard, the poten- tial difference Zn//rZnSO 4 is 0*520 + ( - 0-283) = ~~ '83 volts, and that for Cu/?rCuSO 4 is + 0-585 + ( - 0*283) = + 0-302 volts, the E.M.F. of the Daniell cell being as before j= (-0-803) + ( - 0-302) = 1*105 volts, 378 OUTLINES OF PHYSICAL CHEMISTRY As reference electrodes for alkaline solutions, the mercuric ox- ide electrodes Hg/HgO in .NaOH and Hg/HgO in /ioNaOH are most convenient. The same kind of vessel may be used as for the calomel electrode. The potentials, which become constant after 2-3 days, are for the normal electrode Eh = + 0-114 volt and for the N/io electrode + 0-169 volt at 18. As reference electrode for acid solutions the hydrogen electrode (p. 375) or the mercurous sulphate electrode Hg/Hg 2 SO 4 in .H 2 SO 4 may be used. For the latte e A = + 0-689 volt at 1 8. Single Potential Differences. The Capillary Electro- meter. When mercury and sulphuric acid are in contact in a capillary tube, and the arrangement is connected with a source of E.M.F. in such a way that the mercury is in contact with the negative pole and the acid with the positive pole, the area of the surface of separation between acid and mercury tends to diminish. The following out of this observation of Lippman's has led to an approximate estimate of the absolute differences of potential at metal/solution junctions. When mercury and sulphuric acid have been in contact for some time, it is probable that there is a constant difference of potential between them, brought about in a rather complicated way. We have already learnt that well-defined differences of potential are established when a metal is in contact with a solution of one of its salts of definite concentration, and that is probably the state of affairs in the present case. We may suppose that some of the mercury dissolves in the sulphuric acid to form mercurous sulphate, and that the solution im- mediately in contact with the mercury is saturated with regard to the salt. As, however, the osmotic pressure of solutions of mercury salts is in general greater than the solution pressure of mercury, H g 2 " ions deposit on the mercury and the latter becomes positively charged with regard to the solution. The two kinds of electricity attract each other, and we will assume with Helmholtz that the effect of this attraction is that there is a layer of positive electricity near the surface of the mercury ELECTROMOTIVE FORCE 379 holding a corresponding layer of negative electricity near the surface of the acid (" Helmholtz double layer ") (cf. Fig. 38). Now there will be* a certain surface-tension at the junction mercury /solution in the capillary tube, and, as is well known, the effect of surface tension is to make the areas of the surfaces in contact as small as possible. This tendency will, however, be counteracted by the electric layers; the positive charges will repel each other and tend to enlarge the surface, and the same is true of the negative charges. The effect of the difference of potential is, therefore, to diminish the surface tension. The fact that a contrary E.M.F. applied to the junction tends to diminish the surface of separation between acid and mercury will now be readily understood. The con- trary E.M.F. diminishes the difference of potential between acid and mercury, part of the force diminishing the surface tension is removed, and the latter attains more nearly its true value when undisturbed by electrical forces. When the con- trary E.M.F. is gradually increased, the surface tension increases at first, attains a maximum value, beyond which it gradually diminishes. It is plausible to suppose that the surface tension increases as the difference of potential between mercury and acid gets slnaller and smaller, that it attains its maximum value when the contact E.M.F. at the junction is just neutralized by the contrary E.M.F., and that it again diminishes as the latter is further increased and the surfaces become charged with electricity of opposite sign to the original charges. This at once gives us a method of determining single differences of potential. It is only necessary to note when the surface tension attains its maximum value ; under these circumstances the applied E.M.F. is clearly equal to the single difference of potential at the junction mercury/solution and the problem as to the value of a single potential difference is solved. In this way Ostwald estimated the E.M.F. of the normal calomel electrode at 0*560 volts. Unfortunately the matter is not quite so simple as the above 380 OUTLINES OF PHYSICAL CHEMISTRY considerations would lead us to suppose, and it is fairly certain that the absolute potentials arrived at in this way may differ to some extent from the true values. It has'already been pointed out that two standards are in use, and that the use of the calomel electrode for measuring differences of potential has certain practical advantages. Before considering another method which has been suggested for measuring single differences of potential, it should be mentioned that the phenomena just described have been utilized in the construction of an electrometer the so-called capillary electrometer which, as already mentioned (p. 356) can be used as a null instrument in E.M.F. measurements by the compensation method. A convenient form of the capillary electrometer is represented in Fig. 43. A tube C, 4*5 mm. internal diameter and a bulb-tube A are connected by a vertical capillary tube B 0-5 mm. in- ternal diameter. So much mercury is poured into C that it stands at a con- venient height in the capillary tube. A quantity of mercury is also placed in A and the latter and the capillary are then filled up with dilute sulphuric acid. As indicated in the figure the two quantities of mercury can be connected with the positive and negative poles of a source of E.M.F. when required. The wire D connected with the mercury in the bulb-tube is sealed i n a gl ass tu be so as not to come in contact with the sulphuric acid. When the apparatus is so arranged that the mercury and acid are in equilibrium at a point in the capillary tube and the two quantities of mercury are then connected with a source of E.M.F. the potential at the junction in the capillary tube will alter owing to alteration in the concentration of mer- Qurous salt produced by the current. The surface tension be- FIG- 43- ELECTROMOTIVE FORCE 381 tween acid and mercury must therefore also change (p. 379) and also the position of the junction in the capillary, since the position of the meniscus depends to some extent on the surface tension between mercury and acid. The use of the apparatus as an electrometer will now be evident. It is best so to arrange matters that the mercury at the narrow surface is connected with the negative pole of the external source of E.M.F. through a tapping key, and the junction is observed through a small microscope. If an external E.M.F. is applied, the surface will move when the key is momentarily depressed, and for small differences of potential (up to 0*01 volt) the movement of the meniscus is proportional to the applied E.M.F., so that the name electrometer is justified. When the applied E.M.F. is zero, no movement of the meniscus occurs on making contact, and the electrometer may therefore be used as a null instrument. When not in use, the electrometer should be connected up with a cell of E.M.F. not exceeding i volt. An alternative very instructive method of determining single potential differences, the theory of which is due mainly to Nernst and the practical realization to Palmaer, will now be de- scribed. When mercury in a fine stream is allowed to flow into an electrolyte containing a definite concentration of mercurous salt (e.g., mercurous chloride), Hg 2 " ions from the solution deposit on the drops as they enter (the osmotic pressure of Hg 2 "ionsin the solution being greater than the solution pres- sure of the mercury), the drops thus become positively charged, and further become surrounded with a layer of the liberated Cl' ions. When the drops reach the bottom of the vessel containing the electrolyte, the positive ions are given up and reunite with the Cl' ions to form more calomel. The net result of this process is that the solution gets poorer in calomel where the drops enter, and richer where they unite with the mercury. A concentration cell is thus formed, and it is evident that positive electricity must flow from the weak to the strong solution, that is, from top to bottom of the vessel, a deduction which is borne out by experiment. 382 OUTLINES OF PHYSICAL CHEMISTRY Now it must be possible to reduce the concentration of Hg 2 " ions to such a point that the osmotic pressure of the Hg 2 " ions is just equal to the solution pressure of the mercury ; there is then no deposition of Hg 2 " ions on the entering drops, and no current flows. Conversely ', when no current results when mercury is dropped into an electrolyte containing Hg^- ions, the difference of potential between mercury and the solution must be zero. If the Hg 2 - ion concentration is still further reduced, the solution pressure of the mercury is greater than its osmotic pressure in the solution, and the current flows in the opposite direction. The Hg 2 " ion concentration was reduced by adding potassium cyanide till the point of no current and therefore zero difference of potential was reached. The solution in equilibrium with mercury under these conditions may be termed the null solu- tion. If then a cell is built up of the type Hg | null solution | solution of salt of metal M | M o ^ -> H 2 ; when it goes in the contrary direction gaseous hydrogen becomes ionised according to the converse equation, H 2 -> 2H\ A hydrogen concentration cell is obtained when two hy- drogen electrodes, containing the gas at different pressures, are combined in the usual way. Such cells correspond exactly with those made up with amalgams of different concentrations. The direction of the current is such that the pressures on the two sides tend to become equal, so that hydrogen becomes ionised at the high pressure sJ4e and is discharged as gas at the low pressure side. 25 386 OUTLINES OF PHYSICAL CHEMISTRY In calculating the E.M.F.'s of such cells by the general formula (p. 371) it has to be renumbered that, since the hydrogen molecule contains two atoms the work gained in bringing a mol of the gas reversibly from the pressure P l to the lower pressure P 2 is RT log e PJ/P.J whilst if the same change is carried out electrically, H 2 + 2F~ > 2H 4 , the energy concerned is 2F coulombs. Hence, since 2F = RT log e PJP 2 the E.M.F. of the cell is T7 RT 1 P l E= JprlOg.gJ, The same formula applies to gas cells in which chlorine and other divalent gases are used (see also p. 398). On the other hand, since 4F coulombs are associated with the solution of i mol of oxygen (O 2 + 2H 2 O - 4F^4OH') the E.M.F. of an oxygen concentration cell is v RT , P, E = -p !og p 1 . 4r P2 Another type of hydrogen concentration cell is obtained when the gas concentration in the electrodes is constant and the H' concentration in contact with the two electrodes is different. An interesting cell of this type is built up as follows: H 2 (Pt) | N/io alkali | N/ioacid | H 2 (Pt) Since the equilibrium H + OH'2H 2 O always holds, there must be a minute concentration of H' even in alkaline solution and therefore the above represents a hydrogen concentration cell. From the E.M.F. of the above cell which, after ap- plying a correction for the contact difference of potential, amounts to o 6951 volt at 18, the product of the ionic concentration for water, [H-] [OH'] = k can be calculated as follows. From the general equation E = 0-0577 Iog 10 cjc^ we have 0-6951 = 0-0577 Iog 10 ^ 2 f lt the H- concentration in N/io acid at 1 8, is 0*0888 hence ELECTROMOTIVE FORCE 387 and 2 , the H- concentration in N/io alkali = 0-0888 x lo" 12 ' 045 . The OH/ concentration in the same solution, allowing for in- complete dissociation, is 0*0892. Therefore [H-] x [OH'] = 0-0888 x 10 - 12 ' 045 x 0-0892 = 0-7 x 10 ~ 14 at 1 8, which is in ex client agreement with the value found by other methods (p. 294). Cells in which the electrodes are in contact with different gases, for example, the hydrogen-oxygen cell, are referred to below. Potential Series of the Elements During the considera- tion of the Daniell cell (p. 360), it was pointed out that metals differ greatly with regard to their solution pressures. Zinc, for example, has a very high solution pressure, whilst that of copper is very small. The difference of potential between a metal and a solution of one of its salts at room temperature is represented by the formula T , 0-058 , P t = _1_ log,.-, and if/, the osmotic pressure of the positive ions of the salt, is the same for all the electrodes, say that represented by a solu- tion containing a gram-ion per litre, it is evident that the value of E is proportional to the solution pressure of the metal. As regards the standard to which the E.M.F.s are to be referred, the hydrogen standard has in this case certain advantages. The potential of metals with regard to normal-ionic solutions of their salts is therefore obtained by measuring the E.M.F. of cells of the type H 2 (Pt) | H- | normal ionic solution of the metallic salt | metal, the difference of potential H 2 (Pt) | #H- being taken as zero. The E.M.F. of the combination H 2 (Pt) | H- | ;*-ZnSO 4 | Zn 0-770 388 OUTLINES OF PHYSICAL CHEMISTRY measured with the potentiometer in the usual way, is 0-770 volts, the hydrogen being positive with regard to the zinc. The value of E Zn804 _ Z n is therefore + 0770 volts, the poten- tial difference at the other junction being zero by definition, and positive electricity goes in the cell in the direction indicated by the arrow, that is, the solution tension of zinc is greater than that ofhydrogen> so that the former displaces the latter (indirectly) from solution. On the other hand, the E.M.F. of the cell H 2 (Pt) | nH' | CuSO 4 | Cu is 0*329 volts, copper being positive ; positive electricity goes in the solution in the direction represented by the arrow. Hydro- gen therefore goes into solution and copper is deposited, so that the solution pressure of hydrogen is greater than that of copper. The numbers obtained as above indicated, that is the dif- ference of potential between a metal and a normal-ionic solution of one of its salts (solutions which contain a gram of the corres- ponding ion per litre) are termed the normal potentials or electro- lytic potentials of the metals in question and are usually indicated by the symbol e . In a similar way the normal potentials of electrodes which yield negative ions (such as oxygen, chlorine, and bromine) may be measured. The following table contains the normal potentials e oh for a large number of elements referred to the hydrogen electrode as standard. The normal potentials referred to the normal calomel electrode, e^ (its potential being taken as zero), are obtained from the normal hydrogen potentials by means of the formula e oh = *. + 0-283 volt. The numbers for chlorine, bromide and iodine, are comparable with the others, and are obtained in a somewhat similar way. The value for chlorine, for example, may be obtained by measuring the E.M.F. of a cell of the type. ELECTROMOTIVE FORCE 389 H 2 (Pt) | n ' H | n * Cl | Cl 2 (Pt), the right-hand electrode being reversible for chlorine just as the left-hand one is reversible for hydrogen (see below). Normal Potentials, e oh . Na Mg Al Mn Zn Fe Cd - 2-7 - 1*48 - 1-28 - 1-07 - 0-770 - 0-46 - 0-42 Tl Co Ni Sn Pb K 2 Cu - 0-32 - 0*3 - 0-25 - 0*19 - 0-12 o + 0-329 Hg/Hg 2 - Hg/Hg- Ag Pt Au O I Br Cl F 0-775 '^35 '8 '86 i'o8 0-393 0*63 1-09 1*40 2'o By means of this table, the E.M.F. of a cell made up of two metals in contact with normal solutions of their salts can at once be calculated. As the following schemes show, a zinc- nickel element has the E.M.F. 0-770 - 0*25 = 0*520 volts, and a zinc-silver element the E.M.F. 0*770 - ( - 0-80) = 1*570 volts. Zn I nZn" I Ni" I Ni 0-770 0-25 Zn | nZn" \ #Ag- | Ag 0*770 o'8o 0*520 v. positive electricity flowing in the respective cells, in the direc- tions indicated by the lower arrows. The student should have no difficulty in understanding these schemes in the light of the considerations advanced on p. 365. Both in the case of zinc and of nickel the solution pressure of the metal is greater than the osmotic pressure of the metallic ions in normal solution, and, therefore, when arranged to form a cell, the tendency for posi- tive electricity to pass round the circuit is in the opposite direc- tion at the two junctions. Positive electricity, therefore, flows in the direction in which the acting force is the greater, and the total E.M.F. is the difference of the forces at the two junctions. 390 OUTLINES OF PHYSICAL CHEMISTRY In the zinc-silver cell, on the other hand, the forces act in the same direction, and the total E.M.F. is therefore the sum of the forces at the junctions. According to Nernst's formula, and in agreement with the convention now widely used that the potential difference has the positive sign if the electrode is positively charged with respect to the solution and the negative sign if the electrode is negatively charged, the normal potential is represented by the formula : RT, '- - inr"*^ since c, the concentration of the ions, in the above measurements is unity. Therefore the general formula repre- senting the P.D. between an electrode and an electrolyte of the ionic concentration c is when the electrode gives positive ions, and nF when the electrode gives negative ions. In order to illustrate the use of these formulae we may cal- culate the P.D. at each electrode and the total E.M.F. of the cell Ag | AgCl sat. sol. | Ni SO 4 o-i molar | Ni at 25, assuming that the P.D. at the liquid contact is eliminated ( and that the nickel salt is 60 per cent ionised. [ for nickel - 0-25 volts ; for silver o'8o volts.] The formula is as follows : RT ' n 2 F n 1 for nickel is 2 and Cj is 0-06; n 2 for silver is i and c 2 is 1-25 x 10 ~ 5 gram-ions per litre at 25. Hence E= - 0*25 + 0-029 Iog 10 (0-06)- 078- 0-058 log 10 (i-25 x'icr 5 ) - 0-25 - 0-035 ~ ' 8 + 0-289 = - 0-796 ELECTROMOTIVE FORCE 391 The total E.M.F. of the cell is - 0796 volts; the P.O. at the silver electrode is + o^n volts, and at the nickel electrode - 0*25 - '035 = - 0*285 volts. In order to avoid errors of sign, it is well to check results such as the above from the point of view of general principles. Since diminishing the concentration of a solution from which ions are separating lowers, and diminishing the concentration of a solution into which new ions are going increases the E.M.F. at a junction (p. 366) it is evident that the effect on the E.M.F. of alteration of the concentrations of the solutions must be as shown above. From the above considerations it would appear that metals which stand higher than hydrogen in the tension series can liberate hydrogen from acids anfl that,the numbers in the table afford an approximate measure of the energy of the change On the other hand, hydrogen at atmospheric pressure should displace the metals which stand below it in the tension series. This has been shown to hold in some cases at least with hydrogen occluded in platinized platinum electrodes, the plat- inum presumably acting as a catalyst for reactions which under ordinary conditions are extremely slow. Finally each metal should be able to displace from combination any metal below it in the tension series, the difference of potential between the metals being a measure of the free energy of the change. On the whole these conclusions are borne out by the experi- mental results except in so far as the phenomenon of over- voltage comes into play. This subject is briefly discussed in a later section (p. 403). Cells with Different Gases The simplest example of these cells is the hydrogen-chlorine cell, already referred to. One-half of the cell consists of a hydrogen electrode in acid, the other of a similar electrode saturated with chlorine, and the two electrodes are combined as represented in Fig. 41, the intermediate vessel containing acid of the same strength as that in the cell. The chemical change which takes place in the cell 392 OUTLINES OF PHYSICAL CHEMISTRY is the combination of hydrogen and chlorine to form hydro- chloric acid. Representing the cell as usual H 2 (Pt) | H- | C1' I Cl 2 (Pt), 1-40 it is clear that positive electricity flows in the cell from hydrogen to chlorine in the direction represented by the arrow, the chlorine becoming the positive and the hydrogen the negative pole. The E.M.F. of the cell in normal acid at the ordinary temperature is about i '40 volts. The most important cell of this type is the hydrogen-oxygen or Grove's cell, the two poles being saturated with hydrogen and oxygen respectively. Wh$n connection is made the gases gradually disappear, hydrogen becoming ionized at one pole and oxygen uniting with water to form hydro xyl ions at the other pole. The cell may therefore be represented by the following scheme (acid, alkali or salt) 1-23 and positive electricity flows through the cell from hydrogen to oxygen as represented by the arrow, so that hydrogen is the negative pole and oxygen the positive pole. The hydrogen electrode is reversible with regard to hydrogen, as follows : H 2 ^2H*, the reaction taking place at the oxygen electrode is as follows : H 2 O + iO 2 ^2OH'. When employed as indicated above, the change is that represented by the two upper arrows and 2F passes through the wire ; when, on the other hand, 2F is sent through the cell in the opposite direction, the changes at the two poles are represented by the two lower arrows. If absolutely indifferent electrodes were used for absorbing the gases, and the changes at the electrodes were fully rever- ELECTROMOTIVE FORCE . 393 sible, the calculated E.M.F. of the cell is 1-23 volts. 1 The values actually observed are smaller, probably owing to the formation of an oxide of platinum, which has an oxygen potential different from that of free oxygen. Theoretically, only pure water is necessary as electrolyte, but, in order to increase the conductivity, dilute acid or alkali or a dilute salt solution is employed as electrolyte. The E.M.F. of the cell is independent of the nature of the electro- lyte since the product [H-][OH'] is the same in acid, alkaline, or neutral salt solution, but this is not the case for the single potential differences at the electrodes. Oxidation-Reduction Cells The gas cell just described is a typical oxidation-reduction cell, as when working hydrogen is being oxidized at the negative pole and oxygen reduced at the positive pole. As may be anticipated, corresponding cells can be con- structed in which instead of hydrogen another reducing agent is used, and instead of gaseous oxygen another oxidizing agent. Indifferent metals, such as platinum or iridium, are used as electrodes in all cases. We will first consider a cell built up of a hydrogen electrode on one side and a platinized platinum electrode dipping in a solution of a ferrous and a ferric salt on the other. When the two electrodes are connected up, a current flows in the cell from the hydrogen to the other electrode. Hence at the hydrogen electrode gaseous hydrogen is going into solution as hydrogen ions according to the equation H 2 + 2F = 2H*, 2 and at the other electrode Fe"* ions are being reduced to Fe** ions according to the equation 2Fe*** - 2F = 2Fe**, the charges neutralizing each other through the wire and thus producing 1 Corresponding with the free energy of formation of water from its elements. The calculation is rather complicated. (Compare Nernst and von Wartenberg, Zeitsch. physikal. Chem., 1906, 56, 544.) a aF or 2 x 96,540 coulombs converts a mol of hydrogen to H- ions. 394 OUTLINES OF PHYSICAL CHEMISTRY a current. When the same quantity of electricity is passed through the cell in the opposite direction, Fe" ions are con- verted to Fe ions, and hydrogen gas is liberated at the other pole ; the cell therefore works reversibly, and the measurement of the E.M.F. gives a measure of the free energy or affinity of the reaction. The total change is, of course, expressed by the equation 2Fe + H 2 = 2Fe" + 2H\ Other oxidizing agents can be measured in the same way against the hydrogen electrode, and from the results a table of various solutions, arranged in the order of their oxidizing potentials, can be obtained. Some of the values obtained in this way may be given SnCl 2 in HC1 0-23 volts FeCl a in HC1 0-98 volts NH 2 OH in HC1 0-38 volts KMnO 4 in H 2 SO 4 i -50 volts The above are only meant .to indicate the order of the results, as the accurate values depend greatly on the concentration and composition of the solutions. The four solutions mentioned, even stannous chloride, in acid solution exert an oxidizing action on gaseous hydrogen, and therefore the direction of the current is the same as in the ferric chloride cell. As might be anticipated, potassium per- manganate has the highest oxidation potential. When, on the other hand, a platinum electrode dipping into a solution of stannous chloride in potassium hydroxide is con- nected with a hydrogen electrode so as to form a cell Sn" in H 2 (Pt) (Pt) 0-560 hydrogen ions are discharged and the stannous salt becomes oxidized, positive electricity, therefore, flowing in the cell in the direction of the arrow. The change which takes place in the cell may be represented by the equation 2li- + Sn" =Sn-"- + H 2 , the hydrogen acting as the oxidizing agent. In this case we ELECTROMOTIVE FORCE 395 may say that the stannous chloride solution has a certain reduc- tion potential. The above considerations are sufficient to show that the terms " oxidizing agent " and " reducing agent " are relative and not absolute ; whether a substance acts as an oxidizing or a reducing agent depends on the substance with which it is brought in contact. The hydrogen electrode may be replaced by a platinum electrode dipping in a solution of a reducing agent, an oxida- tion-reduction cell containing only liquids being obtained. One well-known cell of this type consists of platinum electrodes dipping in solutions of ferric chloride and stannous chloride respectively. The changes at the electrodes may be represented by the equations (j) 2Fe- - 2F = 2Fe- (2) Sn" + 2F = Sn and the total change as follows 2Fe- + Sn" = 2Fe" + Sn It is now easy to understand what at first sight appears very puzzling, that a ferric salt can oxidize a stannous salt at a dis- tance, the solutions being in separate cells and possibly con- nected by an indifferent solution. The above equations show that the essential feature of the phenomenon is the transference of two positive charges from the iron to the tin ions through the wire. As a definite potential may be ascribed to every substance acting as an oxidizing or reducing agent, it is clear that the E.M.F. of an oxidation-reduction cell may be represented as the algebraic sum of the differences of potential at the two junc- tions. When a strong oxidizing solution is combined with a still stronger oxidizing solution to form a cell, the former will be oxidized at the expense of the latter, but the E.M.F. of the cell will be small, as the solutions are acting against each other. The further apart two solutions are in the oxidation-reduction potential series, the greater will be the E.M.F. of the cell formed by their combination. 396 OUTLINES OF PHYSICAL CHEMISTRY We are now in a position to give a clear definition of oxida- tion and reduction in dilute salt solutions. An increase in the number of positive charges or a diminution in the number of negative charges on an ion denotes oxidation ; decrease in the number of positive charges or increase in the number of negative charges on an ion denotes reduction. The usual definition of oxidation as consisting in an addition of oxygen to a compound or the abstraction of hydrogen from it, is clearly inapplicable to salt solutions, but the older definition retains its value for changes in which organic compounds are concerned, and for solid compounds ; these have so far been very little investigated from an electro-chemical standpoint. According to the above definition, all reactions which take place electromotively are oxidation - reduction reactions, oxidation taking place at one electrode and reduction at the other. In the Daniell cell, for instance, oxidation takes place at the cathode, Zn + 2F-Zn", and reduction at the cathode Cu" - 2F = Cu. It follows that the displacement of one metal by another is to be regarded as an oxidation-reduction process. Elements which can only give positively charged ions, e.g. the typical metals, can only act as reducing agents, whilst elements such as chlorine, which only yield negatively charged ions, invariably exert an oxidizing action. Solutions, on the other hand, may behave according to the conditions either as oxidizing or reducing agents, since one or the other ion may react. Cupric bromide solution, for instance, acts as an oxidizing agent towards zinc and as a reducing agent towards copper. Moreover, a single ion, e.g. ferrous ion, Fe" may act either as an oxidizing or as a reducing agent since it can be changed into uncharged Fe or into Fe m * f . Electromotive Force and Chemical Equilibrium. In the previous section, we have considered oxidation-reduction cells from the qualitative standpo : nt only. Just as in the case of the Daniell cell, which indeed is a special type of oxidation- ELECTROMOTIVE FORCE 397 reduction cell, the E.M.F. at an electrode depends upon the concentration of all the ions taking part in the change. Thus the E.M.F. at a platinized platinum electrode immersed in a solution of a ferric salt is only definite when a certain proportion of Fe" ions are also present, and the E.M.F. depends on the concentrations of both ferric and ferrous salt. The general equation representing the dependence of the E.M.F. of such cells on the concentrations of the substances taking part in the reaction will now be given. The reversible reaction n 1 A l + n 2 A 2 + . . . ^iij'Aj' + n 2 'A 2 ' ... (p. 159), when it proceeds in one direction in an electrolytic cell, may be represented by the equation njAj 4- n 2 A 2 + . . . + nF-Mi/A/ + n/A 2 ' + . . . which indicates that n 1 mols of Aj and n 2 mols of A 2 . . . are converted into n/ mols of A/ and n 2 ' mols of A 2 ' by taking up n faradays. The maximum work obtainable when the substances on one side of the equation at definite concentrations are transformed isothermally and reversibly into the substances on the other side of the equation also in definite concentrations may be derived by a non-electrical method or by carrying out the reaction in a galvanic cell. In the former case the maximum work may be stated in the form where the square brackets represent concentrations and K represents the equilibrium constant. When the process is carried out in a galvanic cell the maximum work obtained is A = nFE (p. 352) hence When both the initial substances and the final products are in unit concentration the maximum work obtainable non- electrically is A = RT log e K 398 OUTLINES OF PHYSICAL CHEMISTRY and in a galvanic cell nFe , where e is the normal potential Hence the general equation representing the dependence ol the E.M.F. of the cell on the concentrations of the reacting substances is E = e - ?I 10R [A 1 /]>V t A >'. nF ge [A,]", [A 2 ]" 2 The concentrations of the more highly oxidized substances (i.e. those formed by taking up positive charges) occur in the denominator. For the change Fe- + the above expression has the form For the chlorine electrode 2CV + 2F^C1 2 RT = <- log. LCIT/[C1 2 ]. As regards the permanganate electrode, for which the equation MnO 4 ' + 8H- 5F^ Mn~ + 4H 2 O represents the probable chemical change, the expression for the E.M.F. is as follows : RT . [Mnl- [H 2 O] 4 K = _ _ IOP- I . . J _ t _ ? _ =L. 5F ge [Mn0 4 ]' [H-] 8 It is clear from the above equations that the effect on the E.M.F. of the cell of systematic variation in the concentrations of the reacting substances throw light on the nature of the chemical change taking place in the cell and also on the number of faradays associated with the change in question. Electrolysis and Polarization If an external E.M.F. of i volt is applied to two platinum electrodes dipping in a con. centrated solution of hydrochloric acid, it will be found that the large current which at first passes when connection is made rapidly diminishes and finally falls practically to zero. The ex- planation of this behaviour is that while the current is passing hydrogen accumulates on the cathode and chlorine on the ELECTROMOTIVE FORCE 399 anode, thus setting up an E.M.F. which acts against the E.M.F. applied to the poles of the cell. This phenomenon is termed polarization. In the above case the gases go on accumulat- ing in the electrodes till the back E.M.F., which we will term e t is equal to the applied E.M.F., when the current ceases. If, however, an E.M.F. of 1*5 volts is applied at the electrodes, a continuous current passes through the solution and it is evident that in this case the back E.M.F. e has not attained the value of i '5 volts. The explanation is evident when it is remem- bered that the E.M.F. of a cell in which platinum electrodes are charged with hydrogen and chlorine respectively at atmo- spheric pressure is 1-40 volts (p. 392). When an E.M.F of 1*5 volts is applied, the electrodes become charged up tc atmospheric pressure, but no higher, the excess of the gases escaping into the atmosphere. It follows that e cannot under ordinary circumstances attain a higher value than i -40 volts, so that electrolysis proceeds at an E.M.F. of E - e 0*10 volts. The E.M.F. which must just be exceeded in order that a continuous current may pass through an electrolyte is termed the " decomposition potential" of the electrolyte, and it is clear from the above example that the decomposition potential is equal to the E.M.F. of a cell in which the products of electrolysis are the combining substances. As the E.M.F. of such a cell is the algebraic sum of the differences of potential at the electrodes, it is clear that the decomposition potential is also the sum of two factors, namely, the sum of the potentials required to discharge the anion and cation respectively. The decomposition potential of an electrolyte may be deter- mined in two ways. According to the first method, the external E.M.F. applied to the electrodes is gradually raised and the point noted at which there is a sudden increase in the current. The value of the current, C, is determined by the equation E - e = CR, where R is the resistance of the circuit, and will obviously 400 OUTLINES OF PHYSICAL CHEMISTRY increase rapidly as soon as E is greater than e. The second method is to charge the electrodes up to atmospheric pressure by using an E.M.F. greater than e t then the external circuit is broken and the E.M.F. of polarization measured at once. This method depends upon the fact already indicated, that the de- composition potential is that E.M.F. which is just sufficient to overcome the E.M.F. of polarization. As has just been pointed out, the potential required to dis- charge an ion such as Zn" must just exceed the difference of potential at the junction Zn/Zn", and is, therefore, the same as the potential of the metal in volts in the tension series (p. 389). Further, the E.M.F. required to decompose an electrolyte is clearly the sum of the separate differences of potential required to discharge the anion and cation respectively, and is, there- fore, obtained by addiner the values for the two ions in the tension series. The matter becomes clearer when we consider that the potential difference between an element and its ions may conveniently be regarded as a measure of the affinity of the element for electricity. Thus the affinity of zinc for positive electricity is equivalent to 0*770 volts, and that of chlorine for negative electricity to 1*40 volts. To convert zinc ions to metallic zinc we must, therefore, apply a contrary E.M.F. which just exceeds the affinity of zinc for positive electricity, in other words, the decomposition potential of zinc ions is 0770 volts. On this basis, the decomposition potential of zinc chloride should be 0770 + 1-40 = 2-170 volts, of hydrochloric acid 1-40 volts, and of copper chloride ( - 0-329 + 1-40) = 1-071 volts respectively. This is fully confirmed by the experimental determinations of Le Blanc, who obtained the following values : ZnCl 2 = 2-15 volts, HC1 = 1-31 volts, CuCl 2 = 1*05 volts, an agreement within the limits of experimental error. Separation of Ions (particularly Metals) by Electro- lysis The results just mentioned are well illustrated by the phenomena observed when a mixture of electrolytes is electro- lysed at different values of the applied E.M.F. The foregoing ELECTROMOTIVE FORCE 401 considerations show that on gradually raising the E.M.F. that chemical change takes place most readily for which the least difference of potential is required, and this may be taken advantage of for the electrolytic separation of metals which are discharged at different potentials. Suppose, for example, a mixture of hydrochloric acid, zinc and copper chlorides is subjected to electrolysis. Below i volt practically no change will occur, but at n volts, a little above the decomposition potential for copper chloride, copper will be deposited on the cathode. When it has been almost completely removed, and the potential is raised to 1-4 volts, hydrogen will be liberated at the cathode. Finally, the attempt may be made to remove zinc by raising the external E.M.F. above 2*2 volts, but this cannot be effected in acid solution, as there is a large excess of hydrogen ions, which are more easily discharged than zinc. In an exactly corresponding way, almost all the bromine may be electrolytically separated from a solution containing zinc chloride and zinc bromide before the chlorine appears. It is, therefore, clear that it is the value of the E.M.F., and not the strength of the current, which is of primary importance for the separation of metals, and in recent years methods based on this principle have become of great commercial importance. Besides the value of the applied E.M.F., the concentration of the ions in contact with the cathode is of great importance, as the decomposition potential necessarily depends on the ionic concentration, and hence great attention is now paid to the efficient stirring of the electrolyte. 1 The Electrolysis of Water. Overyoltage (Super- tension) at Electrodes. When aqueous solutions of many salts and strong acids and bases are electrolysed with smooth platinum electrodes only hydrogen and oxygen are liberated as products of electrolysis and the decomposition potential is in 1 The electrolytic separation of metals on this principle is described in recent papers by Sand (Journal of the Chemical Society, 1907, 91, 373, iQo8, 93, 1572), and others 26 4 o2 OUTLINES OF PHYSICAL CHEMISTRY all cases about i '66 volts. It was formerly supposed that one or both of these gases were formed by the action of the primary products of electrolysis on the solvent, but this does not account for the fact that the decomposition potential is in general the same for different acids and bases. It is now accepted, for reasons given below, that the gases are products of the primary decomposition of water. If such is the case, and the decomposition of water proceeds reversibly at the electrodes, we would expect the decomposi- tion potential to be about 1*2 volts, in agreement with the E.M.F. of the hydrogen-oxygen cell, whereas it is considerably higher. When, however, platinized platinum electrodes are used and the current is plotted against the applied E.M.F., the latter being gradually increased, it is found that there is a sudden increase in the current at 1*1 volts (so that water can be continuously decomposed at the latter potential), but a much more rapid increase at i -66 volts. Two possible explanations of these remarkable facts might be suggested. Nernst was formerly of opinion that at the lower potential H' and O" ions are being discharged the current being veiy small because of the exceedingly minute concentration of the O" ions. The more rapid decomposition at 1*66 volts is due to the discharge of H* and OH' ions the latter combining to form water and oxygen according to the equation 4.OH -> 2H 2 O + O2. Another mode of explaining the results is that the decom- position potential depends on the nature and condition of the electrode material ; at many electrodes the potential must be raised above that theoretically required for reversible decom- position in order to reach the point of decomposition. Thus assuming that the decomposition of N/i sulphuric acid takes place reversibly at a platinum cathode, the following values for the cathodic decomposition potential with other metals were obtained: Pd + 0-26, Pt o, Fe - 0-03, Cu - 0-19, Al - 0*27, Pb - 0*36, Hg - 0*44. Thus hydrogen is eliminated more easily at a palladium than at a platinum electrode, per- ELECTROMOTIVE FORCE 403 haps owing to the formation of an alloy with the former metal ; in all other cases a greater or less excess of E.M.F. is required in order to liberate the gas. Overvoltage phenomena also oc- cur- at the anode when oxygen is being liberated, but in this case the order of the metals is not the same as with hydrogen. The magnitude of the overvoltage increases considerably with increase of current-density. There is no doubt as to the great, importance of overvoltage phenomena, although they are not ye} fully understood. They appear to depend, in part at least, on supersaturation with the gas. Thus when hydrogen is liberated at a platinized platinum anode, the latter dissolves a large amount of the gas and facili- tates its escape in bubbles, thus bringing about equilibrium between the gas in solution and in the gas space. On the other hand smooth platinum, and such metals as lead and mercury, have very little solvent power for hydrogen, and a much higher pressure is required in order to force in sufficient of the gas to admit of the formation of bubbles (Nernst). Ac- cording to Forster, the liberated substance forms some com- pound with the electrode material, and 'the supertension is determined by the concentration of the gas thus dissolved in some form in the electrode. By making use of the high concentration of hydrogen obtainable at electrodes showing considerable supertension, reductions not readily effected by other methods can be performed. Supertension phenomena have an important bearing on the dissolving of metals in acids. Pure zinc should liberate hydro- gen from acids at a potential of 0770 volts but the superten- sion is so great as almost to reach this value and the reaction therefore proceeds very slowly. The overvoltage at impure zinc is much less and therefore the metal dissolves much more readily in acids. In the latter case local differences of potential doubtless also play a part. The main evidence in favour of the view that water under- 404 OUTLINES OF PHYSICAL CHEMISTRY goes primary decomposition during electrolysis is that the de- composition potential is largely independent of the electrolyte, whether acid, base or salt ; and further, that of the possible changes which can take place at the electrodes the decomposi- tion of water is usually that which can take place at the lowest potential (compare previous section). In the case of hydro- chloric acid the relationships are more complicated. In con- centrated solution the decomposition potential is lower than that of water (p. 400) and the main products are hydrogen and chlorine; with progressive dilution the decomposition potential rises and ultimately a mixture of oxygen and chlorine is liber- ated at the anode. The decomposition potential curve of sulphuric acid shows two further points of rapid increase of current, at 1-95 and 2-6 volts respectively. It seems probable that the former value is connected with the discharge of SO/' and the latter with the discharge of HSO/ ions. Electrolysis and Polarization (continued). The E.M.F. required to bring about decomposition of an electrolyte is not determined solely by the magnitude of the polarization due to the products of electrolysis. The current also causes concen- tration changes at the electrodes and these changes always act in opposition to the E.M.F. driving current through the cell. This effect is known as concentration polarization and is mini- mised by stirring the electrolyte. Any substance which tends to diminish the polarization in a cell is termed a depolarizer ; It may act as a catalyst in ac- celerating the changes at the electrodes, e.g., platinized platinum in the liberation of hydrogen, or it may alter the change taking place at the electrodes to one that takes place more easily, e.g., the use of potassium dichromate in the so- called Bichromate cell. The " insoluble " salt in an electrode of the second kind acts as a depolarizer. Recent investigations have shown that polarization occurs in ELECTROMOTIVE FORCE 405 many cases where it would not be anticipated, and this fact has raised the question as to the exact nature of the changes taking place at the electrodes during electrolysis. When, for in- stance, a current is passed through the cell Cu | CuSO 4 | Cu it would be anticipated according to the accepted views re- garding electrolysis that Cu" ions would be discharged at the cathode as metallic copper, that SO 4 " ions after discharge at the anode would immediately attach the latter forming copper sulphate. As a matter of fact Le Blanc l has shown that under these circumstances considerable polarization occurs both at anode and cathode, so that the changes taking place at the poles can scarcely be as simple as those just assumed. A still more striking case occurs in the electrolysis of solid silver salts between silver electrodes. With silver sulphate, for in- stance, a polarization E.M.F. of 0*312 volts was observed two minutes after breaking the circuit and at - 80 an E.M.F. of no less than 1*562 volts one minute after breaking the circuit. 2 The cause of these remarkable observations is still by no means understood. Accumulators As is well known, accumulators are em- ployed for the storage of electrical energy. An accumulator is a reversible element ; when a current is passed through it in one direction the electrodes become polarized, and when the polar- izing E.M.F. is removed and the poles of the accumulator are connected by a wire, the products of electrolysis recombine with production of a current and the cell slowly returns to its original condition. It will be clear from the above that the Grove's gas cell is a typical accumulator or secondary element; when a current is passed through it in one direction the electrodes become charged with hydrogen and oxygen, and these gases can be 1 M. Le Blanc, Abhandlungen der Bunsen-Gesellschaft, No. 3, 1910. 2 Haber and Zawidzki, Zeitsch. physikal. Chem., 1911, 78, 228. Com- pare Annual Reports Chemical Society for 1912, p. 19. 406 OUTLINES OF PHYSICAL CHEMISTRY made to recombine with production of a current. From a technical point of view, however, a satisfactory accumulator must retain its strength unaltered for a long time when the poles are not connected, and must be easily transported. A gas accumulator would be in many respects un suited for commercial purposes. The apparatus most largely used for the storage of electricity is the lead accumulator, the electrodes of which in the un- charged condition contain a large amount of lead sulphate (obtained by the action of sulphuric acid on the porous lead of which the electrodes largely consist at first) and dip in dilute sulphuric acid. The accumulator is charge by sending an electric current through it. At the cathode, the lead sulphate is reduced by the hydrogen ions (or rather by the discharged hydrogen) to metallic lead according to the equation PbSO 4 + 2H- - 2 F = Pb + 2H- + SO 4 " or more simply, PbSO 4 - 2F = Pb + SO 4 " On the other hand, the SO 4 " ions wander towards the anode and react with it according to the equation PbSO 4 + SO 4 " + 2H.O + 2F = PbO 2 + 4H- + 2SO 4 " so that the anode and cathode consist mainly of lead peroxide and metallic lead respectively. On connecting up to obtain a current (discharging), SO 4 " ions are discharged at the new anode (the lead pole), and reconvert it to lead sulphate, according to the equation Pb + S0 4 " + 2 F = PbS0 4 , and simultaneously H* ions are discharged at the new cathode (the peroxide pole), the peroxide being reduced to the oxide, and acted on by sulphuric acid to reform the sulphate, according to the equation PbO 2 + 2H- + H^SO 4 - 2F = PbSO 4 + 2H./). ELECTROMOTIVE FORCE 40? The chemical changes taking place on charging and discharging are summarized in the equation Pb + PbO 2 + 2H 2 SO 4 ^ 2PbSO 4 + 2H 2 O ; the upper arrow represents discharging, and the lower arrow charging. The E.M.F. of the lead accumulator is about 2 volts. It is not strictly reversible, but under ordinary conditions of working about 90 per cent, of the energy supplied and stored up in it can again be obtained in the form of work. The only other accumulator of commercial importance is that developed more particularly by Edison and his co-workers, and known as the Edison accumulator. In the charged condition the positive plate consists of hydrated nickelic oxide, Ni 2 3 , x H 2 and the negative plate of finely divided iron, the electro- lyte being about 4 N alkali. On discharging the nickelic oxide is reduced to nickelous hydroxide Ni(OH) 2 and the iron is oxidized to ferrous hydroxide Fe(OH) 2 . According to Forster the changes taking place on charging and discharging are re- presented approximately by the equations : Fe + Ni 2 O 3J i-2H 2 O + i -8H 2 O^Fe(OH) 2 + Ni(OH) 2 . Both the anode and cathode consist of steel flames provided with a large number of pockets (made of nickel-plated steel) in which the active electrode materials are packed. The potential during discharge is about 1*34 volts, and, as the above equation shows, is independent (in practice only very slightly dependent) on the alkali concentration. One advantage possessed by the Edison accumulator is its comparative lightness. The Electron Theory l In the previous chapters we have learnt that certain atoms (or groups of atoms) can become associated with definite quantities of electricity, and that certain other atoms can take up twice as much, three times as much, and so on. No atom is associated with less positive electricity J Nernst, Theoretical Chemistry, chap. ix. ; Rutherford, Radio-Activity; Ramsay, Presidential Address, Trans. Chem, Soc. t 1908, 93, 774. 4 o8 OUTLINES OF PHYSICAL CHEMISTRY than a hydrogen atom, and we may therefore state that a hydrogen atom unites with unit quantity of electricity to form an ion. A barium ion has twice as much positive electricity, and a ferric ion three times as much positive electricity as a hydrogen ion. Further, since quantities of hydrogen and chlorine ions in the proportion of their atomic weights are electrically equivalent, it follows that Cl' (and other univalent negative ions) contain unit quantity of negative electricity. This increase by steps in the amount of electricity associated with atoms at once recalls the law of multiple proportions, and it appears plausible to ascribe an atomistic structure to electricity ; in other words, to postulate the existence of positive and negative electrical particles, which under ordinary cir- cumstances are associated with matter. On this view, the number of dots or dashes ascribed to positive and negative ions respectively indicates the number of electrical particles (positive or negative) with which the atoms become associated to form ions. These views 1 (Helmholtz, 1882) have received powerful support during the last few years from the results of experi- ments on the passage of electricity through vacuum tubes, the so-called Hittorf s or Crookes' tubes. When a current at very high potential is sent through a highly evacuated tube, rays from the cathode the so-called cathode rays stream across the tube with great velocity, and it -has been shown that these rays consist of negative electricity. The speed of the particles depends on the E.M.F. between the poles of the tube, but at a difference of potential of 10,000 volts is about one-fifth of the velocity of light. The mass of these particles is about i/i ooo of that of the hydrogen atom. They are usually termed negative electrons. More recently, it has been dis- covered that the ft rays given off from disintegrating radium at a speed approaching that of light also consist of negative electrons. 1 Helmhgltz, Faraday Lecture, Trans. Chctn. Soc., 1883, ELECTROMOTIVE FORCE 409 As negative electrons have thus been found to exist separate from matter, it is natural to expect that free positive electrons may also be isolated. So far, however, this has not been found possible, and opinions differ somewhat as to the reason. Nernst, following Helmholtz, considers that there is no ground for doubting the existence of positive electrons ; the reason why it has not yet been found possible to isolate them is due to their great affinity for matter. Further, Nernst and others assume that positive and negative electrons unite to form neutral atoms or neutrons^ and that these neutrons constitute the ether which is assumed to pervade all space. Other investigators regard a positive ion as an atom minus one or more negative electrons ; the loss of a negative electron would leave the previously neutral atom positively charged. 1 From observations on the effect of a magnetic field on the cathode discharge, it has been calculated that the actual charge carried by a univalent ion (positive or negative) is about 4 x 10 ~ 10 electrostatic units. The application of the electron theory to ordinary chemical changes yields interesting results. For simplicity we will assume the existence of positive electrons, and designate them by the symbol , negative electrons by the symbol 0. When hydro- gen arid chlorine unite to form hydrochloric acid, we assume that under ordinary conditions the valency of the hydrogen is satisfied by that of the chlorine. We may, however, dis- place a chlorine atom by a positive electron, and thus obtain the saturated chemical compound H or H ; in an exactly similar way, the hydrogen may be displaced by a negative electron, forming the saturated compound C10. In the same way, a dilute solution of copper sulphate contains the / / saturated compounds Cu(^ or Cu - and SO 4 <^ or SO 4 ". The electrons, therefore, behave exactly as univalent atoms, 1 Ramsay, loc. cit. 4 io OUTLINES OF PHYSICAL CHEMISTRY the positive electrons enter into combination with positive elements such as H, K, Na, Ba, etc., the negative electrons enter into combination with negative elements or groups, such as Cl, Br, I, NO 3 , SO 4 . Nothing is known as to the constitution of a non-ionised salt molecule in solution. The formula for non-ionised sodium chloride may perhaps be Na Cl, the molecule being held together at least partly by electrical forces. Just as there are great differences in the affinity of the elements for each other, so the elements have very different affinity for electrons. Zinc and the other metals have a great affinity for positive electrons, the so-called non-metallic ele- ments have in many cases considerable affinity for negative electrons. The order of the elements in the tension series may be regarded as the order of their affinity for electricity. On this view the potential required to discharge the ions is simply the equal and opposite E.M.F. required to overcome the attraction of the element and the electron (p. 375). Practical Illustrations. Dependence of Direction of Current in Cell on Concentration of Electrolyte It has already been pointed out (p. 346) that the current in a Daniell cell may be reversed in direction by enormously reducing the Cu- ion con- centration by the addition of potassium cyanide. The two chief methods for diminishing ionic concentration are (i) the forma- tion of complex ions (as in the above instance) ; (2) the forma- tion of insoluble salts. When a cell of the type Cd CdS0 4 dilute KNO 3 | CuSO 4 I Cu dilute is set up, and the poles are connected through an electroscope, it will be found that positive electricity passes in the cell in the direction of the arrow. If some ammonium sulphide solution is then added to the copper sulphate solution, "insoluble" copper sulphide is formed, and the concentration of the Cu" ELECTROMOTIVE FORCE 411 ions is reduced to such an extent that the current flows in the reverse direction. If the Daniell cell Zn ZnSO 4 | KNO 3 I CuSO 4 Cu dilute I I dilute is built up in the same way, it will not be found possible to re- verse the current by the addition of ammonium sulphide, owing to the greater solution pressure of the zinc as compared with cadmium ; but if potassium cyanide is added, the current changes in direction, owing to the fact that the Cu" ion con- centration in a strong solution of potassium cyanide (in which the copper is mainly present in the complex anion Cu(CN) 4 ") is considerably less than in a solution of copper sulphide. The following experiments, which are described in consider- able detail in the course of the chapter, should if possible be performed by the student. For further details text-books on practical physical chemistry should be consulted. (a) Preparation of a standard cadmium cell (p. 357). (b) Measurement of the E. M . F. of a cell by the compensation method (p. 355). (c) Preparation and use of a calomel "half-cell " (p. 375). (d) Preparation and use of a capillary electrometer (p. 380). (e) Measurement of the E.M.F. of a concentration cell (p. 368). (/) Measurement of the E.M.F. of the hydrogen-oxygen cell (p. 392). (g) Determination of the solubility of a difficultly soluble salt, -K'. . (2) When the solutions are mixed, the volume becomes v -4- v l and the pro- portion of H' ions o H- a'. For the acid HA we now have (I - a)(v + V') Dividing equation (3) by equation (i) we obtain (o + a')v _ a + a' __ v + ' v' ' ~~ (v + v')a whence v a _ a or -- v v v PROBLEMS AND QUESTIONS 415 Now al v and a'fv' are the respective concentrations of H' ions in the isohydric solutions of the acids, and have now been shown to be equal in other words, the condition for isohydry is that the concentration of the common ion in the two solutions before mixing must be the same. (5) Measurement of Chemical Affinity. We have seen that there are two principal methods of measuring chemical affinity (T) by means of E.M.F. measurements in a galvanic cell (p. 351) and (2) by measurements of the position of tquilibrium in the system under definite conditions. The first method has already been fully described. A proof of the for- mula used in the equilibrium method and one or two examples will now be given. It will be sufficient for our present purpose to derive the affinity formula for a reaction in which gases only are concerned; the same formula applies to reactions in heterogeneous systems. A vessel contains hydrogen, oxygen, and water vapour of the respec- tive concentrations Cn 2 , Co 2 , and Cn 2 o at the constant temperature T. It is assumed that one of the walls of the vessel is permeable for hydro- gen only, another for oxygen only, and a third for water vapour only, and that the walls can be displaced without friction. Outside each of these walls is the particular gas for which it is permeable, at the same tempera- ture and concentration as the corresponding gas inside, and the amounts both outside and inside are so great that no appreciable change in con- centration is caused by the passage of a mol of gas into or out of the vessel. The wall permeable for hydrogen is now moved inwards so that 2 mols of hydrogen are removed from the vessel, and similarly, by moving in- wards the wall permeable for oxygen, i mol of the latter gas is brought outside. In these processes no work is done, as no alterations of pressure are set up. The hydrogen and oxygen are now allowed to expand rever- sibly at constant temperature T until they attain any desired smaller concentrations C'u 2 and Co 2 The work done by a mol of a perfect gas in expanding from the volume v to v l is A = RT log e vjv = RT log e C/C' and therefore (assuming that both hydrogen and oxygen behave as perfect gases) the total work gained in the above processes is f The 2 mols of hydrogen (concentration Cn 2 ) and the mol of oxygen (concentration Co 2 ) are now combined to form 2 mols of water vapour of concentration CH 2 0> the latter concentration being so chosen that the water vapour is in equilibrium with hydrogen and oxygen of the respec- tive concentrations Cn 2 and Co 2 . No work is done in this combination, which is carried out under equilibrium conditions. Finally the 2 mols of water vapour of concentration Cn 2 o are brought isothermally and rever- sibly to the initial concentration Cn 2 o and added to the contents of the vessel through the wall permeable for the vapour. In the latter process the work gained is The result of these processes is that in the interior of the vessel 2 mols of hydrogen of the concentration Cn 2 an d * m ol of oxygen of the concentra- tion Co 2 have disappeared and a mols of water vapour of the concentration 416 OUTLINES OF PHYSICAL CHEMISTRY Cfl 2 o have been formed without any alteration of temperature or concen- tration inside the system. The total work gained is A = A, + A 2 = 2 RT log e ^ + RT log, -^ + 2 RT lo ge Cn 2 Co 2 which is a measure of the affinity of hydrogen and oxygen at the tempera- ture and concentration in question. The above equation may be written in the form Now A depends only on the initial and final states of the system and is therefore independent of the arbitrarily chosen concentrations C'n 2 and Co 2 to which the gases were brought after removal from the vessel. It follows that the expression ... 2 - = constant = K, in other words, Cli 2 Co 2 whatever be the concentrations Cn 2 and Co 2 , the concentration Cn 2 o of water vapour in equilibrium with Cn 2 and Co 2 is such that the above equation holds. We have here a thermodynamical proof of the law of mass action, first established by Guldberg and Waage from kinetic considerations. The affinity of hydrogen to oxygen is therefore represented by the formula A = RT log e K - RT log e Il2 and can be obtained for any concentration C of the reacting substances when the equilibrium constant of the action has been determined. It can easily be shown that a formula of this type applies both to homogeneous and heterogeneous reactions. The general formula is as follows (p. 297) : A -RT log. K-RT log. t*'.]'' [*.'*- [AJ, [AJ-V- which, when the initial substances and the products are in unit concen- tration, simplifies to A = RT log K, For the combination of hydrogen and iodine the general formula becomes A=Rriog.K-RT 1 og. [ ^ f L_. At the temperature of boiling sulphur (T = 273 + 445 = 718) K = = 50. 0-02 The work obtained by the combination of i mol of iodine and i mol of hydrogen, each at unit concentration, to 2 mols of hydrogen iodide, also at unit concentration, is therefore A = 1-985 x 718 x 2-303 Iog 10 5o = + 5575 calories. We have here a case where the affinity of a reaction and the heat of reaction are of opposite sign - the latter is about - 6000 cal. The general formula will now be used to calculate the chemical affinity of a heterogeneous reaction, namely, the maximum work obtain- able in the combination of i mol of carbon dioxide with calcium oxide at PROBLEMS AND QUESTIONS 417 a definite temperature to form calcium carbonate. It is usual to denote the affinity of a gas as that shown towards the solid substances at atmo- spheric pressure. We proceed to calculate the affinity of carbon dioxide for calcium oxide at 671 C. = 944 abs., the equilibrium pressure at this temperature being 13-5 mm. In this case (p. 174) [CaC0 3 ] _^_ ~ [CaO] [COJ /cos, and A = - RT log e p. therefore A = - 1-985 x 944 x 2-303 Iog 10 13-5/760 = 7540 calories. The value of A obtained is the same whether concentrations or partial pressures are used for calculations in which gases are concerned. In the above calculation the pressure of the atmosphere is taken as unit. (6) Deduction of the Formula Connecting Displacement of Equilibrium with Change of Temperature. Van't Hoff's formula (p. 166) which is usually written in the form <*(log a K) _ - Q dT " RT a can easily be deduced from the expression A - Q = T(dA./dT) for the second law of thermodynamics (p. 151) and the affinity formula A = RT log e K given in the last section. From the latter formula we obtain by differentiation and whence dT RT a 1. A certain quantity of a gas measures 100 c.c. at 25 and 700 mm. pressure. What pressure will be required to change the volume to 50 c.c. at - 10 C. ? Ans. 1236 mm. 2. What volume is occupied by (a) i gram of nitrogen, (b) i gram of carbon dioxide at 20 and a pressure of 72 cm. of mercury ? Ans. (a) 906-3 c.c. ; (b) 576-8 c.c. 3. An open vessel is heated till one-third of the air it contains at 20 is expelled. What is the temperature of the vessel ? Ans. 117-6 C. 4. If 0-5 grams of a gas measure 65 c.c. at 10 and 500 mm. pressure, what is its molecular weight ? Ans. 271-5. 5. If i gram of nitrogen, i gram of oxygen and 0-2 gram of hydrogen are mixed in a volume of 2-24 litres at o, calculate the respective partial pressures of the gases in the mixture, in grams per sq. cm. Ans. 369, 323, and 1025 grams /cm. 2 6. The density tot benzyl alcohol, C 6 H r ,CH 2 OH, at its boiling-point is 1*145. Compare the observed and calculated values of the molecular volume (p. 61). Ans. Obs. 123-7. Cal c. 128-8. 7. The density of a solution containing 4*1375 grams of iodine in 100 grams of nitrobenzene is 1*2389 at 18, the density of the solvent at the same temperature being 1-20547. From these data calculate the molecu- lar solution volume of iodine. Ans. 67*2 c.c. 8. The density of formic acid at 20 is 1*2205 and n D at the same tem- perature is 1*3717. Calculate the molecular refractivity of formic acid by 27 A - Q = T = RT log, K + 418 OUTLINES OF PHYSICAL CHEMISTRY the Lorentz formula and compare it with the value calculated from the atomic refractivities (cf. p. 65). Ans. Obs. 8-56. Calc. 8-35. g. The value of no for a mixture of formic acid and water containing 62*7 per cent, of the latter was found to be 1*3625 at 19*5, and the density at the same temperature 1*1462. Calculate the refraction constant by the Lorentz formula and compare it with, that calculated on the assumption that the components exert their effects independently. [D 19 for water 0-9984 ND = i*3333-] Ans. Obs. 0-1937. Calc. 0-1936. 10. Find the relationship between the solubility, s, of a gas and its absorption coefficient, a, in a liquid at t (cf. p. 83). Ans. 5/a = (273 + *)/273. 11. Calculate the gas constant, R, in litre-atmospheres from the obser- vation that a solution containing 34*2 grams of cane sugar in i litre of water has an osmotic pressure of 2*522 atmospheres at 20. Ans. 0-0860. 12. The osmotic pressure of a 2 per cent, solution of acetone in water is equal to 590 cm. of mercury at 10. What is the molecular weight of acetone? Ans. 60 (found), 58-0 (theor.). 13. What is the molecular concentration of an aqueous solution of urea which at 20 exerts an osmotic pressure of 4*6 atmospheres ? Ans. 0-19 molar. 14. The vapour pressure of ether (mol. wt. 74) is lowered from 38-30 cm. to 36-01 cm. by the addition of 11*346 grams of turpentine to 100 grams of ether. Calculate the molecular weight of turpentine. Ans. 132 (theor. 138). 15. The vapour pressure of water at 50 is 92 mm. How much urea (mol. wt. 60) must be added to 100 grams of water to reduce the vapour pressure by 5 mm. ? Ans. 18-1 grams. 16. A current of dry air was passed in succession through a bulb con- taining a solution of 30 cane sugar in 160 grams of water, through a bulb, at the same temperature, containing water, and finally through a tube containing concentrated sulphuric acid. The loss of weight in the water bulb was 0-0315 grams and the gain in weight in the sulphuric acid bulb 3-02 grams. Calculate the molecular weight of cane sugar in the solution. Ans. 339. 17. The addition of 1*065 grams of iodine to 30-14 grams of ether raises the boiling-point of the latter by 0-296. What is the molecular weight of iodine in ether ? Ans. 251. 18. The vapour pressure of ether at o is 183-4 mm., at 20 433*3 mm. Calculate the latent heat of vaporisation per mol. of ether at 10. Ans. 6840 cal. 19. The vapour pressure of water over a mixture of CuSO 4 , 5H 2 O and CuSO 4 , 3H.X) is 2-933 mm. at 13-95 and 21-701 mm. at 39*7. Calculate the heat given out when i mol. of water combines with CuSO 4 , 3H 2 O to form CuSO 4 , 5H ? O. Ans. - 13,730 cal. 20. 0-3 grams of camphor, C 10 H 16 O, added to 25*2 grams of chloroform raise the boiling-point of the solvent by 0-299. Calculate the molecular elevation constant for chloroform. Ans. 38-2. 21. From the data in the previous question calculate the heat of vapo- risation of chloroform (boiling-point 61). Ans. 6931 cal. 22. 1-2 grams of a substance dissolved in 24-5 grams of water (K =s PROBLEMS AND QUESTIONS 419 18-5) caused a depression of the freezing-point of 1*05. Find the mole- cular weight of the substance. Ans. 86. 23. Beckmann found that 0*0458 grams of benzoic acid in 15 grams oi nitrobenzene (K = 80) caused a depression of the freezing-point of 0-099. What conclusion can be drawn from this observation as to the molecular condition of benzoic acid in nitro benzene ? Ans. Acid is associated. 24. At 343 the vapour pressure of ammonium bromide is 195 mm. and at 356 it is 289 mm. Calculate the heat of vaporisation of ammonium bromide, assuming dissociation complete. Ans. 45,000 cal. 25. From formula (i) p. 137, deduce the expression and hence calculate the osmotic pressure of an ethereal solution the boil- ing-point of which is 35*2. (Boiling-point of ether, 34*8 ; latent heat of vaporisation per gram 84-5 cal. Ans. 6*5 atmos. 26. At 21 the surface tension, 7, of diethyl sulphate in 28-28 dynes/cm. 2 and at 62*6 7 is 24*00 dynes/cm. 2 Find the value of c, the temperature coefficient of the molecular surface energy (D 21 = 1*0748 ; D 62 * 6 = 1*0278). Ans. 2*17. 27. For rronochlorhydrin 7 at 17 is 47*61 dynes/cm. 2 (D = 1-3254) and at 57*8 4372 dynes/cm. 2 (D = 1*2883). What conclusions can be drawn from these data as to the molecular complexity of the liquid ? Ans. c = 1*44, liquid is associated. 28. Calculate the heats of formation of ethane, ethylene and acety. lene respectively from their elements at 17 (a) at constant pressure, (b) al constant volume from the following data. Heats of combustion : ethane 370,440 cal., ethylene 333,350 cal., acetylene 310,100 cal. Heats of formation : carbon dioxide 94,300 cal., liquid water 68,400 cal., all at constant pressure. Ans. Ethane: C.P. 23,360 cal., C.V. 22,200 cal. Ethylene: C.P. - 7950 cal., C.V. - 8530 cal. Acetylene : C.P. - 53,100 cal., C.V. - 53,100 cal. 29. Find the heat of formation of anhydrous aluminium chloride from the following data (Thomsen). 2A1 + 6HClAq = 2 AlCl 3 Aq + 3H 2 + 239,760 cal. H 2 + C1 2 = 2HC1 + 44,000 cal. HC1 + Aq = HClAq + 17,315 cal. A1C1 3 + Aq = AlCl 3 Aq + 76,845 cal. Ans. 321,960 cal. (for A1 2 C1 6 ). 30. The heat of solution of anhydrous strontium chloride is 11,000 cal., that of the hexahydrate - 7300 cal. What is the heat of hydra- tion of the anhydrous salt to hexahydrate. Ans. 18,300 cal. 31. The specific heats of diamond and graphite in the neighbourhood of 10 (o-i7) are 0*1128 and 0-1604 calories per gram respectively. The heats of combustion are 94,310 and 94,810 calories per 12 grams respec- tively. Find the heat evolved in the transformation of graphite to diamond at o C. Ans ; 490 cal. 32. In the synthesis of nitric acid and. of ammonia the primary reac- tions are N 2 + O 2 ;-;>2NO - 43,200 cal. 24,000 cal. 4 2o OUTLINES OF PHYSICAL CHEMISTRY Discuss fully the effect of temperature and pressure on these reactions and refer, for illustration, to the manufacturing processes : why is it that in these processes an elevated temperature is used, although one reaction is endothermic and the other exothermic ? At 2000 abs. K = [NO]/[N 3 ]*[O 2 ]i = 0-0153. Assuming the heat of reaction independent of temperature, calculate the equilibrium constant at 2500 abs. (Birmingham Univ.) 33. The vapour density of phosphorus pentachloride referred to air as unity was found to be 5-08 at 182, 4-00 at 250, and 3-65 at 300, calcu- late the degrees of dissociation at these temperatures. Ans. 41-7 per cent. ; 80 per cent. ; 97-3 per cent. 34. From the following data for the equilibrium N 2 O 4 ^2NO 2 at 49-7 calculate the degree of dissociation at each pressure and show, by finding the dissociation constant, that the law of mass action applies : Pressure in mm. Hg 26-80 93'75 182-69 261/37 497*75 Density (air = i) 1-663 1-788 1*894 i*993 2 * I 44 The vapour density of N 2 O 4 is 3*179 (air = i). Ans. 0-93 ; 0-789 ; 0-69 ; 0*63 ; 0-493. 35. Bodenstein found that the degree of dissociation of carbonyl chloride, according to the equation COC1 2 ^> CO + C1 2 , is 67 per cent, at 503, 80 per cent, at 553, and 91 per cent, at 603. From these results calculate the heat of dissociation of carbonyl chloride. Ans. 19,210 cal. from 5O3-553 ; 22,880 cal. from 553-6o3. 36. The ratio of distribution of aniline between benzene and water is io-i : i. When a litre of aniline hydrochloride solution, containing 0-0997 mols. of the salt, was shaken with 59 c.c. of benzene at 25 it was found that 50 c.c. of benzene had taken up 0-0648 grams of aniline. Find the amount of hydrolysis of aniline hydrochloride in the solution and calculate the dissociation-constant of aniline as a base (cf. p. 291). Ans. i'56 per cent., 4*6 x 10 10 . 37. When heated in aqueous solution at 52-4 the concentration of sodium bromoacetate in solution was n-o, 9-4, 7-9 and 6-9 at times o, 26, 52 and 74 hours respectively from the commencement of the reaction, the decomposition being ultimately complete. Find the order of the reaction and calculate the times required to complete (a) one-third, (b) two-thirds of the change. Ans. Unimolecular. 65-2 hours, 177 hours. 38. In an experiment on the rate of reaction between sodium thiosul- phate and ethyl bromoacetate (cf. p. 232) 50 c.c. of the reaction mixture required the following amounts of O-QIIO N iodine at the times from the commencement of the reaction indicated in the table. t (min.) o 5 10 15 25 40 ^ cc.s. iodine solution 37-25 24-7 18-75 15-3 ir6 8*85 4-4 Show that the reaction is of the second order and find the velocity constant for concentrations of i mol. per litre. Ans. 14-6. 39. From the electrolysis of hydrochloric acid in a cell with a cadmium anode the following results were obtained : change in concen- tration of chlorine at anode and cathode respectively + 0*00545 gram silver deposited in voltameter connected in series with the cell 0*0986 gram. Calculate the transport numbers of hydrogen and chlorine (Cl = 35-46; Ag = 107*9). Ans. H = 0*832; Cl =a o'i68. PROBLEMS AND QUESTIONS 421 40. The transport number of the cation in potassium chloride was found to be 0-497 and \ M = 130-1. What is the absolute velocity of K' in cm. per second, under unit potential gradient ? Ans. 0*00067 cm. /sec. 41. At 18 the velocity of migration of the Ag- ion is 0*00057 cm./sec. and of the NO 3 ion 0-00063 cm./sec. What is the value of p^ for silver nitrate at 18 ? Ans. jt ^ = 115-8. 42. Find the degree of ionisation of lactic acid at different dilutions and. calculate the ionisation constant from the following data, valid for 25: v (litres) 64 128 256 512 oo pv 34-3 47-4 64-2 87-6 381 Ans. 0-000138. 43. If the velocity coefficient for catalysis by N/4 acetic acid is 0-00075 what will be the coefficient when the solution is also N/4O with respect to sodium acetate, assuming that the latter is dissociated to the extent of 86 per cent. ? Ans. 0-000075. 44. If an amount of base insufficient for complete saturation is added to an equimolecular mixture of acetic and glycollic acid, in what propor- tion will the salts be formed? (Dissociation constants at 25. Acetic acid 0-000018, glycollic acid o'ooois.) Ans. i : 2*9. 45. A N/io solution of sodium acetate is ionised to the extent of 80 per cent, at 18. What is the osmotic pressure of the solution at this temperature ? Ans. 4*28 atmos. 46. Sodium chloride in 0*2 molar solution is dissociated to the extent of 80 per cent, at 18. What will be the concentration of a urea solution which is isotonic with the salt solution ? Ans. 21-6 grams per litre. 47. Calculate the E. M. F. of an oxyhydrogen cell from the facts that 2H 3 + O 2 = 2H 3 O + 2 x 68,400 cal. and that the temperature coefficient of the E. M. F. of the cell is - 0-00085 volts at room temperature (17). Ans. 1*23 volts. 48. Find the E. M. F. at each electrode and the total E. M. F. of the cell Fe I FeSO 4 o-iN | CuSO 4 o-oi N | Cu at 25, assuming that the iron salt is 40 per cent, ionised and the copper salt 60 per cent, ionised at the dilutions in question, and that the P. D. at the liquid contact is eliminated. [Use the general formula on p. 390.] Ans. Fe electrode - 0*46 - 0*041 = - 0-501 volts. Cu + 0-329 - 0-064 = + 0-265 volts. Total E. M. F. of cell - 0-776 volts. 49. Discuss the influence of temperature and pressure on the equilibrium 2SO 2 + O 2 ^2SO 3 + 45,200 cal. and show how the change of the equilibrium constant with temperature can be calculated. (University Coll., London.) 50. Give an account of the different methods, static and dynamic, which have been used for determining the relative chemical affinities of acids in dilute aqueous solution. (University Coll., London.) 51. Explain the action of the Daniell battery (copper in copper sul- phate, zinc in zinc sulphate) (a) on the hypothesis of the dual nature of electricity + and - , (b) on the hypothesis that negative electricity consists of electrons. Draw two diagrams, one to illustrate each method of re- presentation. (University Coll., London.) 422 OUTLINES OF PHYSICAL CHEMISTRY 52. Criticise the various theories which have been advanced to explain the mechanism of electrolytic conauction. 53. Criticise Berthelot's principle of maximum work. 54. What do you understand by the solubility product ? Discuss the question of the simultaneous solubility of two salts possessing a common ion. (St. Andrews Univ.) 55. Explain carefully why the ratio of the specific heats of a gas de- pends on the number of atoms in the molecule. Briefly describe the method by which for physico-chemical purposes this ratio is determined. (Sheffield Univ.) 56. Define the terms " absorption coefficient," " critical solution tem- perature," " solid solution " and " eutectic alloy " giving examples. (Sheffield Univ.) 57. " Every chemical reaction is reversible." Discuss the statement carefully so as to reveal the extent to which it is true, quoting examples. (Sheffield Univ.) 58. Write a brief account of the developments in electro-chemistry associated with the names of Daniell, Faraday, Hittorf and Arrhenius. (Sheffield Univ.) 59. How would you determine, either directly or indirectly, the critical temperature, pressure and volume (or density) of a pure substance. (Dublin Univ.) 60. Discuss the conditions on which the possibility of completely separating a mixture of two miscible liquids by fractional distillation de- pends. (St. Andrews Univ.) 61. Discuss the associating and dissociating properties of solvents. (St. Andrews Univ.) 62. Describe some experiments in support of the view that ions migrate during electrolysis. How are the transport numbers of ions determined ? (St. Andrews Univ.) 63. Describe the preparation and properties of some colloidal solutions. What is the present view as to the nature of such solutions ? (St. Andrews Univ.) 64. Explain why (a) a higher potential is necessary to electrolyse a decinormal solution of hydrochloric acid than is necessary for a normal solution, (b) why an E.M.F. is usually set up at the surface of contact of dilute and concentrated solutions of the same electrolyte, (c) why magnesium displaces hydrogen slowly from water but rapidly from hydrochloric acid. (St. Andrews Univ.) 65. Describe an experiment to illustrate the migration of ions during electrolysis. How would- you show that the cation and anion in a solu- tion of copper sulphate move with different velocities, and how would you determine the relative velocities ? (Birmingham Univ.) 66. State the phase rule and explain the terms involved. Apply the rule to explain the fact that the extent of dissociation of calcium carbonate depends only on the temperature. (Sheffield Univ.) 67. What class of substance have in solution molecules of larger size than that calculated from the formula, and how does the phenomenon depend on (a) the constitution of the solute, (b) the nature of the solvent. (Sheffield Univ.) APPENDIX. EQUIVALENT CONDUCTIVITY AT 18. TABLE la. Normal Concentr'n. KC1. NaCl. KNO 3 . AgN0 3 . NaC 2 H 3 2 . JK.SO, Na 2 C0 3 . BaCl 2 . 0*0001 129-5 109*7 1247 "5*5 76-8 133 '5 _ 120-5 0-0002 129*1 109*2 124*3 115-2 76*4 1327 119-8 0*0005 128-3 108-5 123-6 "4'S 75-8 130-8 118*3 O'OOI 127-6 107-8 122-9 114-0 75 '2 129*0 II2'O n6'9 0*002 126*6 1067 I22"O 113-0 74*3 126-3 108*5 115*0 0-005 124-6 104-8 I2O*I III'O 72-4 121-9 102-5 111*3 O'OI 122-5 I02'8 Il8*I 108-7 70*2 117*4 96*2 1077 0*02 120*0 100*2 115*2 105*6 67*9 111*8 89-5 IO3"3 0*05 115*9 95 '9 IIO'O lOO'I 64*2 102-5 80*3 96*8 O'l iii*9 92*5 104*4 947 6rx 95*9 72*9 92-2 0'2 1077 88*2 98-6 88-1 57 'i 88*9 65-6 867 '5 102*3 80-9 897 77*8 49*4 787 54'5 77*6 I 98*2 74'4 80-4 67*8 41*2 71*8 45 '5 70-3 92*6 64*8 69*4 55-8 30*0 34'5 60-3 TABLE U. Normal Concentr'n. CuS0 4 . KOH. NaOH. NH 4 OH. HC1. HN0 3 . H 2 S0 4 . HC 2 H 3 2 . O'OOOI II3'3 _ __ 66 _ _ __ 107 0*0002 in*i 53 80 0-0005 106*8 38-0 368 57 O'OOI zoi'6 234 208 28-0 377 375 361 41 O'OO2 93 '4 233 206 20 '6 376 374 351 30*2 0*005 81*5 230 203 13*2 373 37i 33 20*0 0*01 72*2 228 200 9*6 370 368 308 I4-3 0-02 63-0 225 197 7'i 367 364 286 io"4 0*05 5 J *4 219 190 4'6 360 357 253 6*48 O'l 45 'o 213 183 3'3 35i 35 225 4*60 0-2 39-2 206 178 2'3 342 340 214 3 '24 o*5 30*8 197 172 *'35 327 324 205 2*01 i 25-8 184 160 0-89 301 310 198 I-32 2 20'I 160*8 I3I-4 '53 2 254 258 183 0*80 From Kohlrausch and Holborn, Leitvermo*en der Elektrolyte. 423 4 2 4 OUTLINES OF PHYSICAL CHEMISTRY IONIC MOBILITIES (VELOCITIES) IN AQUEOUS SOLUTION AT 18. TABLE Ila. Normal Concentr'n. K. Na. Li. NH 4 . Ag. Ba. *Sr. *Ca. *Mg. $Zn. O'OOOO 65-3 44*4 35*5 64-2 557 57*3 54 'o 53' 49 47 '5 0*0001 647 43 '8 34 '9 6 3 -6 55'4 55'o 517 50-6 47 45*i 0'0002 64-4 43'6 347 63-4 55' 1 54'3 Si 'o 50*0 46 44 '5 o'ooo5 64 'I 43'3 34'4 6 3 -o 54*9 53'3 50-0 48-9 45 43 '5 O'OOI 637 42-9 34'0 627 547 52-2 48-9 47-8 43 42-3 0'CO2 63-2 42-4 33*5 62-2 54 '2 57 47 '4 46-4 42 40-9 0*005 62-3 41-4 32-6 6l'2 53 '2 48*2 44*9- 43*9 40 38-4 O'OI 6i'3 40-5 31-6 60-2 5i'9 457 42-4 41-4 37 35*9 0*02 60 'o 39 '2 3' 3 59 'o 5' 427 39'4 38-3 34 32-9 0-03 59 '2 38-3 2 9'4 58-1 48-6 40-5 37'2 36-1 1 32 307 0*05 57 '9 37 'o 28*2 56-8 46-6 377 34 '4 33 '4 29 27-9 O'l 55'8 35'o 26-1 54'8 43 '3 33'8 30-S 29-4 25 24-0 TABLE Normal Concentr'n. H. Cl. 1 NO S . C10 3 . C 2 H 3 3 . JS0 4 . |C 2 4 . C0 3 . OH. O'OOOO 3i8 65-9 667 60-8 56-2 337 697 6 3 _ 174 O'OOOI 318 65-3 66-1 60 '2 55'5 33'i 67*2 61 172 0'0002 316 6 5 -i 65-9 60 'o 55'2 33'o 66-6 60 172 0*0005 315 64-8 65-5 59 '6 54*6 32-8 6SH 59 171 O'OOI 3M 64-4 65-1 59*3 54 'i 32-6 64^0 58 69 171 0-002 313 63'9 64-6 58-8 53'4 3 2< 4 62 '3 56 66 170 0-005 3" 63-0 637 57-8 52'4 31-6 59'2 54 60 168 0*01 310 62 'o 627 56-8 Si'3 30-8 56-i 5i 55 167 0'02 307 607 6i'5 55-6 497 29 '8 52'3 48 5 165 0*03 305 59'8 60-6 547 48-4 29*0 497 46 47 163 0'05 302 58-6 59*3 53'4 46-4 28 'o 46-1 43 43 161 O'l 296 56-5 57 '3 5i '4 43'2 26-4 41-9 39 38 157 from Kohlrausch and Holborn, Leitvermogen der Elektrolyte. APPENDIX TRANSPORT NUMBERS OF ANIONS. TABLE III. n = gram equivalents per litre. 425 n =3 O'OI. 0-02. 0-05. O*I. O*2. 0-5- i. 2. KC1 1 KBr KI f NH 4 ClJ 0*506 0-507 0-507 0-508 0-509 o'S^ O'.5i4 0-5I5 NaCl 0*614 0*617 0*620 0-626 0-637 0-642 KNO, 0-497 0-496 0-492 0-487 0*479 NaN0 3 0-615 0*614 O"6l2 0*611 0-608 AgN0 3 KC 2 H 3 O 2 0-528 0-528 0-528 0-528 o'33 0-527 o*33 0-519 0-33 0*501 0*331 0-476 0-332 KOH 0735 0-736 0-738 0*740 NaOH o'8i 0-82 0-82 0-82 0-825 HC1 0-172 0*172 0-172 0*173 0*176 0-185 iBaC! 2 0*56 0^65 o'575 0*585 o*595 0-615 0*640 0-657 ICaCL iK 2 C0 3 0-58 0'59 o'6i o*39 0*64 0-40 0-66 0-41 0-675 0-435 0-686 o'434 0700 0-413 |Na 2 C0 3 0*52 o-53 o'53 o*54 0-548 0-542 |MgS0 4 o"6o 0-64 0-66 0*70 0-74 076 *CuSO 4 . 0-62 0-626 0-632 0-643 0-668 0-696 0720 IH^O, ~~ ~ 0-193 0-191 0-188 0-182 0-174 o'i68 POTENTIAL SERIES OF THE ELEMENTS. 1 TABLE IV. The numbers in the following table give the potentials of the substances in question in contact with normal ionic solutions of their salts, referred to three different standards, The numbers under * oh are referred to the potential of the hydrogen electrode as o - o volis, those under e oc are referred to the normal calomel electrode as zero, and those under e c to the calomel electrode = + 0-560 volts. *oh g " Absolute oh. oc. " Absolute Potentials." Potentials." Manganese -1-07 -1*36 0*80 Hg/Hg 2 " 0775 0-492 1-052 Zinc - 0*770 -0-493 Hg/Hg" 0*835 0-552 1*112 Iron -0*46 -0-74 -0-18 Silver 25 0-798 1*075 Cadmium 0*42 -0*703 -0-143 Platinum . 0-86 0-58 I-I4 Thallium 0*32 - 0*603 - 0-043 Gold i -08 0*80 Cobalt -0*30 -0-58 0-02 Fluorine 2*0 i*7 2-26 Nickel -0*25 + 0*03 Oxygen 2 1-2(1-66) 0*9 1-46 Lead 0*119 0*402 + 0*158 Chlorine^ 1*400 I'I2O 1-68 Hydrogen + 000 -0*283 + 0-277 Bromine 5-25 1-095 0*812 1*372 Copper + 0-329 + 0*046 + 0-606 Iodine J 0*628 0-345 0*905 1 From Le Blanc, Lehrbuch der Elektrochemie. 2 Cf. p. 400. These values apply to a solution of normal H" concentration. In order to liberate oxygen from a solution of normal OH' concentration 0*8 volts less are re- quired, and to liberate hydrogen from the same- solution 0*8 volts more are required than in the case of a normal solution of acid. INDEX. ABNORMAL molecular weights in solu- tion, 123. vapour densities, 40-42. "Absolute" potentials, 375, 378. Absorption oflight, 69-73. spectra and chemical constitution, 73- Accumulators, 405. Acetic acid, adsorption of, 325. atomic volume of, 61. density of vapour, 41. dissociation of, 267. Acids, catalytic action of, 205, 219, 272. effect of substitution on strength of, 304. strength of, 269-274. Active mass, 156. of solids, 173. Additive properties, 62, 251, 335. Adsorption, 324. and enzyme action, 332. and surface tension, 330. by charcoal, 324. formulae, 328. theories of, 324-328. Affinity, chemical, 148, 154, 271, 415. constant, 157, 273, 275. Amalgams, cells with, 351. Amlcrons, 318. Ammonium chloride, dissociation of, 42, 219. hydrosulphide, dissociation of, 176. Amphoteric electrolytes, 307. Argon, position in periodic table, 23. Associated solvents, ionising power of, 339- Associating solvents, 123. Association in gases, 41. in solution, 124, 338-342. Atomic heat, 21. hypothesis, 5. Atomic refractions, values of, 65. volumes, 60. weights, determination of, 8-15. standard for, 17. table of, 19. Attraction, molecular, 34, 58. Available energy, 104, 150, 352. Avidity of acids, 269-274. Avogadro's hypothesis, 10, 36. deduction of, from kinetic theory of gases, 32. valid for solutions, 103, 109. BASES, catalytic action of, 220. strength of, 274-276, 292. Beckmann's methods, 116, 120. Benzoic acid, distribution between solvents, 178, 198. Beryllium (glucinum), atomic weight of, 10, ii. Bimolecular reactions, 207, 230. Binary mixtures of liquids, 84-91. distillation of, 87. vapour pressure of, 87. Blood, catalysis by, 202, 229. Boiling-point, elevation of, 114, 118. Boron, atomic heat of, 12. Brownian movement, 318. CADMIUM standard cell, 356. Calomel electrode, 373. Calorimeter, 146, 147, 153. Capillary electrometer, 380. Cane sugar, hydrolysis of, 205. Carbon, atomic heat of, 12. dioxide, critical phenomena of, 49. Catalysis, 217-224. mechanism of, 222. technical importance of, 219. Cathode rays, 399. Chemical affinity, 148, 154, 271. Chemical equilibrium" and E.M.F., 396. 427 428 OUTLINES OF PHYSICAL CHEMISTRY Chemical equilibrium and pressure, 169. and temperature, 166, 169. Clark cell, 358. Coagulation of colloids, 320. adsorption theory of, 323. Colligative properties, 62. Colloidal particles, charged, 319. size of, 318, 323. platinum, 220, 232, 316. solutions, 313. coagulation of, 319. filtration of, 323. optical properties ot, 317. preparation of, 315. Colloids, 313. diffusion of, 313. electrical properties of, 319. irreversible, 323. precipitation by electrolytes, 319. reversible, 323. Combining proportions, law of, 4. volumes of gases, law of, 9, Combustion, heat of, 145. Complexions, 281, 303, 310. Components, definition of, 181. Concentration cells, 367-373. Conductivity, electrical, effect of tem- perature on, 263. equivalent, 251. of pure substances, 258. measurement of, 254-258. molecular, 249, 257, 265. specific, 235, 249. Conservation of energy, law of, 140. of mass, law of, 3. Constant boiling mixtures, 89. Constitutive properties, 62. Continuity of gaseous and liquid states, Copper sulphate, hydrates of, 174. Corresponding states, law of, 56. temperatures, 57. Critical constants, 51, 56. phenomena, 49-58, 69. solution temperature, 86. temperature, determination of, 77. Carbohydrates, 188. Crystallisation interval, 192. Crystalloids, 313. "Cyclic" processes, 133, 136. DANIELL cell, 348, 362, 366. reversal of current in, 366, 401 . Decomposition potential of electrolytes, 399- Deliquescence, 175. Density of gases and vapours, 36, 43. determination of, 37, 41, 48. Dialysed iron, 315. Dialysis, 315. Dielectric constant, 225, 338. and ionisation, 338. Diffusion of gases, 33. in solution, 108. and osmotic pressure, 98, io3. Dispersed system, 315. Dispersion, 315. Dissociating solvents, 123. Dissociation constant, 266, 273, 275. electrolytic, 260-263, 335-337. degree of, 261. evidence for, 335'337. mechanism of, 342. of water, 283, 293. of salt hydrates, 174. in gases, 42, 125, 163. solution, 125, 260-263 thermal, 163. Distillation of binary mixtures, 87, 9*, steam, 90. Distribution coefficient, 95, 178, 197, 327- Dulong and Petit's law, n. Dyeing, adsorption theory of, 330-331. EDISON accumulator, 407. Efflorescence, 175. Electro -affinity, 410. Electrode, calomel, 373. hydrogen, 376, 385. mercuric oxide, 378. Electrodes, normal, 375, 376. Electrolysis, 236-238, 393. of water, 401. separation of metals, etc., by, 395. Electrolytes, strong, 279-282. Electrolytic dissociation. See Dis- sociation, electrolytic. Electrometer, capillary, 380. Electromotive force and chemical equilibrium, 396. Electromotive force and concentration of solutions, 365. measurement of, 354. standards of, 356. Electrons, 407. and light adsorption, 72. INDEX 429 Electrons and valency, 409. Elements, i. disintegration of, 2. periodic classification of, 20. potential series of, 386. table of, 21. Emulsoids, 322. Enantiotropic substances, 197. Endothermic and exothermic com- pounds, 144. Energy, available, 104, 150, 332. chemical, 140, 351-354- conservation of, 140. free, 104, 150, 352. internal, of gases, 46. intrinsic, 143. kinds of, 139. Enzyme action and adsorption, 332. reactions, 221. reversibility of, 222. Equilibrium, effect of pressure on, 169. of temperature on, 166-170. false, 218. in gaseous systems, 161-164. in electrolytes, 266-312. in non-electrolytes, 164-166. kinetic nature of, 158, 160, 241. Equivalents, chemical, 8, 15, 237. electrochemical, 237. Ester equilibrium, 156, 164. Esters, hydrolysis of, 206. sapouification of, 207, 275. Eutectic point, 187, 191. Exothermic and endothermic com- pounds, 144. Expansion of gases, work done in, 27. FARADAY'S laws, 237. Ferric chloride, hydrates of, 194. Filtration of colloidal solutions, 323. Fluidity, 74. Formation of compounds, heat of, 143. Freedom, degrees of, 179, 182. Freezing-point, lowering of, 119-121, 194. Friction, internal. See Viscosity. GAS cells, 364. constant, R, 26, 102. laws, 25-26. deduction of, 31-33. deviations from, 28, 33-35. Gases, 25-48. adsorption of, 328. Gases, behaviour of, on compression, 51. kinetic theory of, 29-35, 46. liquefaction of, 58. solubility of, in liquids, 82. specific heat of, 43-48. Gay-Lussac's law of gaseous volumes, 9- of expansion of gases, 25. Gel (hydrogel), 323. Gladstone-Dale formula, 64. Grotthus' hypothesis, 264. HAEMOGLOBIN, osmotic pressure of, 316. Heat of combustion, 145. additive character of, 148. of ionisation, 285, 295, 344. of solution, 146, 153. Helium, liquefaction of, 59. critical constants of, 51. Helmholtz formula, 351-354, 373- views on valency, 399. Henry's law, 82, 95, 178. Hess's law, 125. Heterogeneous equilibrium, 172-199. Hydrate theory, 333, 339. Hydrated ions, 346. Hydrates, dissociation of, 174. in solution, 340. Hydration in solution, 345-347. Hydrogel, 323. Hydrogen, adsorption of, 329. electrode, 375, 385. iodide, decomposition of, 159, 161. Hydrogen-oxygen cell, 392. peroxide, decomposition of, 202, 229. Hydrogen sulphide, dissociation of, 167. INDICATORS, theory of, 296, 309. Intermediate compounds in catalysis, 223. Ionic and non-ionic reactions, 307. Ionisation and chemical activity, 311. degree of, 261, 281. energy relations in, 343. heat of, 285, 295, 344. mechanism of, 342, 345. role of solvent in, 314, 338, 342- 345- Ionising power of solvents, 338, 339. and free affinity, 339. Ions, 236. .430 OUTLINES OF PHYSICAL CHEMISTRY Ions, complex, 281, 303. 310, migration of, 236, 243-249. . reactivity of, 306, 311. velocity or mobility of, 252-254. Irreversible electro-chemical processes, 354-. Isoelectnc point, 320. Isohydric solutions, 277, 414. Isomorphism, 13, 14. Isosmotic solutions, 105. Isotonic coefficients, 106. solutions, 105. JOULE-THOMSON effect, 58. KINETIC energy, 32, 46, 140. and temperature, 32, 319, of gas molecules, 46. theory of gases, 29-35, 46. Kohlrausch's law, 251. LEAD accumulator, 405. Le Chatelier's theorem, 169. Light, absorption of, 69-73. Liquefaction of gases, 58. Liquids, molecular weight of, 125. miscibility of, 84, 95. properties of, 49-79. Lorenz-Lorentz formula, 64. MASS action, law of, 155-160, 173. and strong electrolytes, 279- 283. in heterogeneous systems 172. proof of, 160. Maxima and minima on curves, 76, 88, 339-342- " Maximum work and chemical af- finity, 150. Medium, influence of, on reaction velocity, 224. Metastable phases, 184. Microns, 318. Migration of the ions, 236, 243-249. Miscibility of liquids, 84. Mixed crystals, 13, 95, 190, 192. Molecular attraction, 34, 58. surface energy, 125. volume, 60, 78. in solution, 62. weight of colloids, 316. abnormal, 40, 123. of dissolved substances, 109- 125. Molecular weight of gases, 36-43. n c- of liquids, 125-127. Molecules, velocity of gaseous, 33. Monotropic substances, 197. Morse and Frazer's measurements of osmotic pressure, 104. Movement, Brownian, 318. Multiple proportions, law of, 4. NATURAL law, definition of terms, 6, 7 Neumann's law, 13. " Neutal salt action," 84. Neutralization as ionic reaction, 284. heat of, 148, 283-285, 336. Neutrons, 409. Normal electrodes, 374, 375. potentials, 388. OCTAVES, law of, 20. Optical activity, 66-69, 229. van't Hoff-Le Bel theory of, 67. Order of a reaction, 213. Osmotic pressure, 97-109. and diffusion, 98, 108. and elevation of boiling-point, 109, 138. and gas pressure, 102, 103. and lowering of freezing-point, 109, 136. and lowering of vapour pres- sure, 109, 131. measurement of, 99, 105. m^c anism of, 106. of colloids, 316. Ostwald's dilution law, 266, 307, Overvoltage, 401. Oxidation, definition of, 396. Oxidation-reduction cells, 393. Ozone-oxygen equilibrium, 168. PARTIAL pressures, law of, 81. Periodic law, 23. system, 20-24. table, 21. Phase, definition of term, 17?. rule, 179. Phosphorus pentachlori 'e, dissociation of, 163. Plasmolysis, 105. Polarisation, concentration, 404. electrolytic, 350, 355, 398, 404. of light, 66. Potential differences at liquid junctions, 382. INDEX 43 1 otential differences, origin of, 362. single, 375, 379, 381. series of the elements, 387. Potentials, "absolute," 375, 378. normal, 388. Protective colloids, 332. Prout's hypothesis, 17. QUADRUPLE point, 196. R, value of, for gases, 27. for solutes, 102. Radium, 2, 379. Raoult's formula, 112. Reaction, order of, 213. Reactions, consecutive, 216. counter, 216. side, 215. Reduction, definition of, 395. Refraction formulae, 64. Refractivity, 63-66. Reversibility in cells, 354. Reversible reactions, 151, 156 222. Rotatory power, 66, 229. magnetic, 69. SALT solutions, solubility of gases in, 84. Semi-permeable membranes, 81, 97, 105, 107, 130. Silicic acid, colloidal, 315, 323. Sodium sulphate, solubility of, 93. Sol (hydrosol), 323. Solubilities, determination of small, 300-302, 370. Solubility, coefficient of, 83. curves, 86, 93, 196. effect of temp?r. 261, 347- of liquids, 73-77, 322. measurement of, 75. absolute values of, 76. of binary mixtures of, liquids, 76, 342. WATER, catalytic action of, 219, 220, 2 33- decomposition by, 285-293. dissociation constant of, 283, 293, 387- electrolysis of, 401-404. equilibrium between phases, 179. ionisation of, 283, 293. PRINTED IN GREAT BRITAIN AT THE UNIVERSITY PRESS. ABERDEEN THIS BOOK IS DUE ON THE LAST DATE STAMPED BELOW AN INITIAL FINE OF 25 CENTS WILL BE ASSESSED FOR FAILURE TO RETURN THIS BOOK ON THE DATE DUE. THE PENALTY WILL INCREASE TO SO CENTS ON THE FOURTH DAY AND TO $1.OO ON THE SEVENTH DAY OVERDUE. ID I U / THE UNIVERSITY OF CALIFORNIA LIBRARY