Glass. Book. . \Hr 3V V4^W THE SOIL, CONSIDERED A8 A SEPARATE AND DISTINCT DEPARTMENT OF NATURE, ROBERT. SERRELL.WOOD, Corresponding Member of the National Institut: WASHINGTON, MARCH, 1850. The most palpable source of nutrition to all created beings was sup- posed by the ancients to possess the attributes of vitality; it was there- fore an amiable weakness on their part to personify the Earfh, and to hold her in peculiar veneration. Modern science has banished this beau- tiful sentiment from its stern philosophy, but it can never invalidate the fact that there are certain ingredients of the soil (whatever be their origin) which claim intermediate rank between matter in such states of comoi nation as the chemist can produce by synthesis, and the lowest specimens of vege'able organisms : neither has it yet successfully proved that the same elements in other shape than the organic salts of humus contribute with equal efficiency to the luxuriance of vegetation, although there is evidence in volcanic and other localities to show, that an excess of either free carbonic acid gas, or ammonia, or water, even when the other minerals present suffice for the wants of plants, is injurious to the highest degree. A greater proportion than at present of those gases and vapours in the atmosphere, and consequently in the soil, may have favored the earliest denizens of our globe : those tribes have now nearly passed awa)% or their constitution has been modified with modifications of cli- mate, &c. A just appreciation of fossil organic remains has elicited a probable truth, that function and organization proceed through both kingdoms of nature by parallel lines of advancement, observable since the difl^erent periods of the world at which they respectively commenced their fxist- ence. It would seem as if some general law, harmonizing with the earth's progress in its physical capacity, governed the succession of these products, an idea which is further supported by their gradujj,l develop- ment at the present day from the germinal to a perfect state. We should also bear in mind the remarkable fact, that animals and vegetables are blended together so as to render any attempt to define their distinguish- ing properties utterly futile. Vegeto-animals have been fully recognised by naturalists ; and we are next led to inquire whether the soil, forming a connection between organized and unorganized matter, partakes of a ve^eJo-minerdl character in the highest acceptation of the term. The animal department, although indebted for its growth and prime condition to azotized aliment approximating more or less in its nature the tissues themselves, borrows, from vegetables especially, hydro-car- bonaceous substances of a less complex composition, a portion of which is converted into fat, another portion is directly oxidized and excreted, while a third is presumed, in the case of the lowest animals, to be con- vertible by means of ammonia into gelatine, &c., their integuments cor- responding with those of plants as surfaces ab-;orbent of nourishment, sufficiently at least to establish a close relation between both races in this lespect as well as in their both inhaling oxygen.* Again, the vege- table department in its highest range, although dependant upon rich mould or organic manures for its most efficient support, (as man and some other animals are upon flesh,) draws from the atmosphere elements convertible into cellulose, &c., indicating the claims of animals upon vegetables, of vegetables upon the soil, and, as I shall endeavor to show, the ultimate dependance of the soil upon the atmosphere. Nature evi- dently proposes more than one resource for the maintenance of her crea- tures ; and unity of design, which pervades the works of creation, would suggest that, although the soil receives its most unequivocal accessions from the debris of plants, it nevertheless allows the crude materials of air to circulate within its pores, and to form more notable combinations. Animals, vegetables, and the soil are constituted in large proportion of particles, which have possessed, but which no longer retain, the usual characteristics of life— particles, be it observed, which threaten to resolve themselves into simpler forms, unless the tendency to disintegration be •The oxidation of the hydrocarburets is generally believed lo liberate caloric in living bodies as a primaty result, but I respectfullv maintaii-i that it, in the first instance, cause, the surrender of electricity which was previously combined ; heat cou^equen.ly becomes a sec.mdary effect, ol an : altered consistency or composition m sohds or fluids, whereby ,l,eir specfic capacity for cal.r.c ( is affected. The temperature of animals is exaggerated by physical exenion, whieh cau-es the . contract on of muscles and a more rapid circulation of the blood. A large portion of the.r food .3 already combined with oxygen in the propor.ion to form water ; no heat is theref„re evolved from this source, ind the separation oFfree water from their surfaces m the shape of vapour produces a reduction (if temperature perhaps equivalent to the heat generated by the conversion ot venou. into arterial blood. The slow reactions between highly constituted substances may be identical in a chemical point of view with ordinary cases of combustion, but the results very different ; the amount of heat liberated being proportionate to the gr-ater or less competency of cotiductmg media to carry off the electricity set free, or of ether contiguous molecules in the circulation or elsewhere to appropriate that imponderable by forming new combinauons. And here I may be permitted to add, that if the solution of a simple metal in the voltaic apparatus liberates a force which, on being conducted by a special arrangement of wire around an enclosed bar of iron mag- netizes it, a Ionian the resolution of more complex particles, such as those contained in the ani- mal circulation, might be supposed capable of contracting (magnetizing) a muscle enclosed with- in a network of conducting ne.vous filaments. A ganglion is the voltaic apparatus, certain con- stituents of the blood electrolytes, the motor and sensitive nerves conducting media, and the mns- cie, which is insulated by cellular matter and ligament, a magnet. 1 he contraction of a muscle or a congeries of muscles would not necessarily diminish the volume of their mass, because their re- duction of size only tends to enlarge the capacity of the surrounding cellular pubstance ; tree m- grees is therefore aliowc d to the blood between the fibres, and coneequently greater efficiency produced in the parts. 3 counteracted by a force of an opposite kind. The soil possesses no evi- dence of organization either in mass or in detail ; but organization may mark grades of development without being indispensable to characterize living matter. Nothing can be more indefinite than even the essential properties of life. Can physiologists determine at wliat precise moment the vital principle is surrendered by a piece of muscle cut from the leg of a healthy animal 1 The separation of a part merely shortens its term of existence by destroying perhaps the faculty of self-preservation or re- production. Where then shall we find the first link in the self-supporting chain of vital products? Are we to consider the vesicles or cells which the microscope discovers almost everywhere on the earth's surface as ex- hibiting the simplest manil'estations of life, or may we refer its rudiments to the corpuscles of blood, or to certain constituents of sap ? I propose to regard the soil as a creature sui generis, sustaining living bodies whilst it is itself sustained by them. Its proportions are limited by the means of increment placed at its disposal. If the natural history of soil be studied, we find that although it may in- crease enormously under certain conditions, and although its term of maturity may be prolonged to an apparently indefinite extent, its ulti- mate dissolution, in whole or in part, is a matter of as much certainty as the lapse of ages. Organized bodies, however, display their power of increase more particularly in their progeny, which represent the pa- rent in an enlarged individuality. The soil, likewise constituted, as I shall presently endeavor to show, of many individuals of different char- acter, is' capable of propagating \\s kind by a quasi-fissiparous process — that is to say, a portion of veritable mould being isolated from the main body and placed in a favorable situation, exerts a quickening influence upon surrounding matter of elemental identity: mould, consequently, either enlarges in bulk itself, or gives bulk to vegetables, just as vegeta- bles, daring their growth, either enlarge in bulk themselvs, or give bulk to animals which leed upon them. It maybe further urged, as a gene- ral proposition, that animals, plants, and the soil, increase and multiply in co-ordinate ratios, and that, with the continued addition of light, a much greater mass of matter will be engaged in the enjoyment of more exalted faculties, either in an organized or semi-organized shape. Aboriginal soil, then, may be attributed to the rays of the sun co-ope- rating with physical changes of certain universally diflused substances, which I shall presently mention — changes of form, consistency, and po- sition, capable of impressing the heterogeneous residue with new affini- ties. We, however, regard, as chiejii/ rnstrnmental, at the present day, in the generation ol" humus de nouo from carbonic acid and water, the forces liberated by already existing humus, or by materials of higher ^rade in the act of decomposition — forces identical with those emitted from the luminous worlds around us. Commencing with the lowest grade of progressive developments, we submit for consideration : first, whether ulmin and other semi-organized subst mces were not originally, and are not still, produced from carbonic acid and water at the expense of ammonia which becomes decom- posed in the ground by means of oxygen, nitrogen being liberated upon the same terms which vegetables prescribe for themselves during an an- alogous process of transformation.* Secondly, whether the disintegra- tion of those hydrocarburets which are formed in vegetables from ulmin, such as starch, gums, oils, &c., does not promote the ibrmation of various azotized proximate principles, when ammonia, sulphur, phosphorus, and some few other minerals, are present. Lastly, whether the dissolution of these proteine and allied compounds into less complex forms, or into their ultimate elements, does not generate cellulose, &c. The idea on which we particularly insist is, the reluctance on the part of bodies, whether organized or unorganized, to allow their constitutional forces to exhaust themselves by their component materials becoming resolved into simpler combinations, as long as contiguous matter evinces the dis- position of assuming an identical character or an equivalent complexi- ty of constitution. For this reason, the snme forces which enter into the constitution of vegetables are apparently transmitted from one gene- ration to another. But, on the other hand, it must be confessed that, were it not for the incessant appropriations of the luminous element by the surface materials of our globe, no iurther progress in the quantity or quality of chemico-vital phenomena could be anticipated. It would likewise be unreasonable to expect the occurrence of these spontaneous formations of soil, where the want of indi>pensable f)re- requisites prohibits what would be an ordinary train of events in more favored regions. The fixed alkalies and alknloi cls, in moderate quantity, might expedite the process, and yet the same bases, or ammonia, or water, in excess, effectually prevent it. To consider them as tending to break up, under all circumstances, rather than to superinduce more complex relations of matter, would be to adopt an error equivalent with considering oxygen an element of universal destruction. Viewed solely as an accumulation of dead or etiete materials, the ground presents a melancholy picture of desolation, l)ut as a thing of life it offers eminent support to the doctrine of development. As soon as a fit habitation was prepared for land-animals and plants, they each in the fulness of time entered on their career. There is an aptitude in this arrangement, and no less probable is it that the first and simplest forms of living matter derived their forces from existing substances of lower degree in complexity, and that the light of heaven co-operated then, as it dees now, in the glorious consummation. Water-plants flour- ished long before dry land appeared ; these must have subsisted upon gases and salts dissolved in the ocean, and their debris became the source of much primeval soil. This admission by no means militates against the proposition that semi-organized compounds, constituting humus, may also be formed in Nature's laboratory by a direct union of the elements concerned, the most obvious cause of a primary character being the reduction of ammonia, or its transtbrmation, into water and nitrogen, by means of oxygen. Whether other compounds be formed in the soil, such as nitrates, which are due to progressive as well as retrograde re- • It niny be oliserved that the gaseous effluvia (excretions proper) respired by the leaves of planis, are (or the most part simple elements, as oxyuen and nitrosren, which, on assuming the Oeritoiin condition, ijivt up the electiiciiy previously binding them with solids in tie closest chemi- cal relations ; their loss of this force redounds to the benefit of plants by the consequent fixation of cerhor? actions, must depend upon dynamic contingencies. Holding these pre- mises in mind, we are led to inquire whether the decomposition of semi- organized compounds did not liberate the necessary forces and introduce the lowest types of vegetable organisms, under conditions of the world more favorable than at present, and which we can scarcely now appre- ciate.* These in turn becoming decomposed, and surrendering their forces, may have forwarded new combinations of vegetable matter, until we reach a period of the earth's history teeming with vital phenomena familiar to us. Germs, like nuclei of lesser note, may be identical, or nearly so, in their ultimate or proximate elements, and yet differ in the proportions of their combined imponderables. On this hypothesis the variety of vegetables and even animals is divested somewhat of mystery ; the ele- ments of nutrition being the same, the congenital forces which direct the earliest vital movements in each particular genus or species deter- mine their subsequent figure and organization. Af er making due allowance for climate and the immediate effects of solar irradiation upon the digestive powers of plants, we attach no little importance to the shape in which their food is presented to the roots. It is asserted by the modern school of Agricultural Chemists, that the or- ganic food of plants is exclusively carbonic acid and ammonia dissolved in water, and, of course, the force of life is esteemed the chief cause of all organic changes of a progressive character. With us, on the con- trary, it is contended, that the substances aforesaid could not possibly be melamorphosed into higher compounds except by the addition of light, or of forces identical with light, derived from organized and semi-orga- nized materiel in the act of decomposition. It is well known, that no manure is more acceptable to vegetables than their own decaying leaves, or the debris of a higher class of plants; the explanatioh now offered for this fact by authoi's entitled to our utmost respect, is, as stated above, very simjjle ; but unfortunately it leaves the solution of ulterior pheno- mena hopeless. To attribute the more abstruse transmutations to a force of life is tantamount to an abandonment of principles applicable to all * These conditions have reference to tbrmer bipolar movements of our e inh, not of an extra- vagant, but of an exaggerated iiind. I intend, on some future occasi m, to submit reasons for the belief th;it the sun is the immeciate cause of the dmrnal rotation of planets within the solar sys- tem, and of their annual changes of position and presentation. To be more explicit: if solar rays be compounded, ;is I shall araue, of repellent and attractive forces neutralized by their com- bination ill light, and ihey be decomposed on the surfacte of the ear h, (this surlace being a mixed one of solids, liquids, and aeriform tiuids ) we can understand how more of the calorific rays tnay be detained on the peripheral or outer portion of oui planet, and exert an influence there, while the electric rays, for the most pan, pass on to ihe innermost surface ot ihe solid crust, causing ad- ditional layers to be precipitated from the central fluid mass. A tempo ary loss of equilibrium llnis occasioned bt'lween the opposite sides of the ^^phere, produces a centrifugal tendency in the comparatively enlarged proximal surface, and a centripetal tendency in the d'stal surface, which becomes, each section of it for the instant, comparaiively smaller than its antipod. We further surmii-e that the earth has reached its present rate of movement and extfnt of bipolar oscillation after considerable diminution of intensity in the North and Soutii hemispheres respectively, at difl^erent epochs; that the approaches to a more perlect equiiibrium^and consequent alleraii(uis of climate from this cause, have been so gradual within the historic period as to liave escaped the no- tice of observers in this field of science. I am notacquainted with any more plausible explanation of the undoubted changes of level in the ocean since the commencement of the tertiary era, as evi- denced by phenomena of universal extent. 6 physical changes for the production of which chemists are unable to con- trol or concentrate the usual forces of matter. Practical agriculturists will ke^iiai^ij0f