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 THE LIBRARY 
 
 OF 
 
 THE UNIVERSITY 
 OF CALIFORNIA 
 
'LORADO SCIENTIFIC SOCIETY. 
 
 'ORT OF THE EXECUTIVE COMMITTEE OF THE 
 COLORADO SCIENTIFIC SOCIETY FOR 
 THE YEAR 1911. 
 
 tEPORT OF THE TREASURER OF THE COLORADO 
 
 SCIENTIFIC SOCIETY FOR THE YEAR ENDING 
 
 DECEMBER 16TH, 1911. 
 
 THE WATER SUPPLY OF COLORADO. 
 
 | 
 
 By CHARLES W. COMSTOCK. 
 
 A CRITICAL DISCUSSION OF THE PRINCIPLES OF 
 THE RICHARDS PULSATOR CLASSIFIER 
 
 By LEWIS B. SKINNER. 
 
 DENVER, 
 
 PUBLISHED BY THE SOCIETY 
 APRIL, 1912. 
 
BANCROFT 
 UBHAftY 
 
 
 
 ' 
 
 L^ <sP CrrPo-* ' 
 
 REPORT OF THE EXECUTIVE COMMITTEE OF THE 
 
 COLORADO SCIENTIFIC SOCIETY FOR 
 
 THE YEAR 1911. 
 
 Denver, Colorado, December 16th, 1911. 
 By the Secretary. 
 
 During the past year the proceedings of your Society 
 show that nine regular meetings were held, with an average 
 attendance of 26-2/3, and that nine papers were presented 
 and read. The papers read, with their titles and authors, 
 were as follows : 
 
 "A Discussion of Rock Streams with Special Reference 
 to the Rock Streams of Veta Peak, Colorado," by Dr. Horace 
 B. Patton. 
 
 "Description of a Tin Deposit in Texas," by Dr. Regis 
 Chauvenet. 
 
 "Genesis of Ore Deposits," by Mr. George J. Bancroft. 
 
 "A Recent Trip to Honduras," by Mr. Rensselaer H. Toll. 
 
 "Asbestos Deposits of Casper Mountain, Wyoming," by 
 Mr. Henry C. Beeler. 
 
 "The 105th Meridian and the Mile High Level, in Denver," 
 by Dr. Herbert A. Howe. 
 
 "Eskimo Dogs, Their Origin, and an Example of Rever- 
 sion," by Mr. J. D. Figgins. 
 
 "The Occurrence and Origin of Nitrates in Colorado Soils ; 
 Some of Their Effects and What They Suggest," by Dr. Wil- 
 liam P. Headden. 
 
 "Screenless Sizer," by Mr. James M. McClave. 
 
 There were nine papers published this year, the same 
 number having been published last year. 
 
 The lowest attendance at any meeting was 14 in Septem- 
 ber, while the highest was 37 in April. The average atten- 
 dance for the nine meetings was 26-2/3. In 1910 the lowest 
 attendance at any meeting was 23 in December, and the high- 
 est was 108 in April, the average being 40.3. 
 
 . 
 
ii REPORT OF THE EXECUTIVE COMMITTEE 
 
 During the year 24 members have been elected. The loss 
 has been 21; 6 by death and 15 by resignation, leaving a net 
 gain of 3. Those lost by death were as follows : Mr. Robert 
 Forrester, who died December 20th, 1910; Mr. John E. Chap- 
 son, who died January 20th, 1911; Mr. Samuel F. Emmons, 
 who died March 28th, 1911; Mr. James B. Grant, who died 
 November 1st, 1911; Mr. Charles B. Kountze, who died No- 
 vember 17th, 1911; and Judge Carlton M. Bliss, who died 
 November 27th, 1911. 
 
 Of the present total membership of 252, 154 reside in 
 Denver; 46 outside of Denver, in Colorado; 41 outside of 
 Colorado, in the United States, and 11 in foreign lands. The 
 roll consists of 4 life members, 9 honorary fellows, 13 fellows, 
 173 members, 38 associates, and 15 who have not as yet been 
 graded. 
 
 The Executive Committee held 5 regular meetings, with 
 an average attendance of 6-1/5, besides several informal meet- 
 ings. 
 
 There have been 6 exchanges added during the past year, 
 viz. : American Brass Founders' Association, Australian Min- 
 ing and Engineering Review, Colorado School of Mines, Eco- 
 nomic Geology, Carnegie Library of Pittsburgh, and the Pat- 
 ent Office Library of London. 
 
 The number of visitors to the museum and library during 
 the past year was 1,321, the number last year being 1,336. 
 
 Books added to the library during 1911 were as follows: 
 
 By Purchase 
 
 American Society of Mechanical Engineers, Volumes 29, 
 30 and 31. 
 
 By Gift 
 
 Annual Report of the Smithsonian Institution for 1909. 
 
 Annual Report of the United States National Museum for 
 1910. 
 
 Twenty-seventh Annual Report of the Bureau of Ameri- 
 can Ethnology for 1905 and 1906. 
 
REPORT OF THE EXECUTIVE COMMITTEE iii 
 
 Twenty-fourth Annual Report of the Interstate Commerce 
 Commission for 1910. 
 
 Biennial Report of the State Historical and Natural His- 
 tory Society of Colorado for 1909 and 1910. 
 
 Bureau of American Ethnology, Bulletin Number 40, 
 Part 1 ; also Bulletin Numbers 43, 44, 50 and 51. 
 
 Colorado Geological Survey Bulletin, Numbers 1 and 2, 
 presented by Mr. W. F. R. Mills. 
 
 Congressional Records Index to Volume 41, Parts 1-5; 
 also Volume 42, Parts 1, 3, 7 and 8. 
 
 Geological Survey of Ohio, Fourth Series, Bulletin Num- 
 bers 2, 12 and 13. 
 
 Geological Survey of Iowa, Volume 20, and Annual Report 
 for 1909. 
 
 Library of Congress Report for 1910. 
 
 Mineral Resources for 1909, Parts 1 and 2. 
 
 Oklahoma Geological Survey, Bulletin Numbers 2, 5 
 and 8. 
 
 Proceedings of the Iowa Academy of Science for 1910, 
 Volume 17. 
 
 Proceedings of the United States National Museum, Vol- 
 umes 30, 39 and 40. 
 
 Records of the Geological Survey of New South Wales, 
 Volume 9, Part 1. 
 
 The Mineralogy of Pennsylvania, presented by Mr. John 
 Eyerman. 
 
 The Railway Library for 1910. 
 
 Wisconsin Geological and Natural History Survey, Bul- 
 letin Numbers 21 and 22 ; also Scientific Series Num- 
 bers 6 and 7. 
 
 During the past year the Society has been organized into 
 5 sections, viz.: 
 
 1 Technical Chemistry and Metallurgy. Secretary, Mr. 
 H. 0. Bosworth. 
 
 2 Economic Geology and Mining Engineering. Secre- 
 tary, Mr. S. A. lonides. 
 
iV REPORT OF THE EXECUTIVE COMMITTEE 
 
 3 Mechanical and Electrical Engineering. Secretary, 
 Mr. H. S. Sands. 
 
 4 Irrigation and Civil Engineering. Secretary, Mr. F. 
 W. Bosco. 
 
 5 Pure Science. Secretary, Mr. G. M. Butler. 
 
 These Sections have held meetings during the year as 
 follows : 
 
 April 8th Section 1 held its first regular meeting, at 
 which Mr. Lewis B. Skinner presided. He gave the address 
 of the evening on "The Practical Versus the Theoretical Man/' 
 
 April 21st Section 2 held its first regular meeting, Mr. 
 S. A. lonides presiding. Mr. George J. Bancroft read a paper 
 on "The Superficial Appearance and Alteration of Ore De- 
 posits.'* 
 
 September 9th Section 1 held its second regular meet- 
 ing, Prof. Herman Fleck acting as chairman. The chair read 
 a paper which had been prepared for this meeting by Mr. 
 F. L. Clerc on "The Utilization of the Zinc Carbonates and 
 Silicates of Leadville, Colorado." 
 
 November 18th Section 1 held its third regular meeting, 
 Mr. Howard C. Parmelee presiding. Dr. Bain read a paper en- 
 titled "Methods of Ore Treatment." 
 
 November 25th Section 5 held its first regular meeting, 
 Mr. George E. Collins acting as chairman. The following 
 papers were read: "Recent Developments in Physics," by 
 Prof. L. F. Miller; "Recent Developments in Chemistry," by 
 Dr. J. B. Ekeley, and "Recent Developments in Geology," by 
 Prof. G. M. Butler. 
 
 In addition to these, under the auspices of this Society 
 and the State School of Mines, meetings have been held at 
 Idaho Springs, Leadville, Telluride and Ouray, for the purpose 
 of stimulating the mining industry of the state by "Practical 
 Talks" by well known scientific engineers to the miners, 
 mine and mill operators of these towns. These meetings have 
 met with much encouragement from the mining communities 
 
REPORT OF THE EXECUTIVE COMMITTEE v 
 
 and the expectation of good results along the line of more eco- 
 nomic management of mines and mills is well warranted. 
 
 With the. view of broadening the usefulness of this So- 
 ciety and obtaining a fuller measure of benefit of the scien- 
 tific labor of the community, in the spring of this year, sec- 
 tions were organized. It was considered that these sections 
 would allow for specialization under one organization, which 
 would result in economy in many ways; affording a common 
 meeting place for members, devoting special attention to dif- 
 ferent branches of scientific investigation, a better frater- 
 nizing of these specialists, a more beneficial interchange of 
 ideas and a greater promotion of useful knowledge. These 
 sections are just now getting into working order, and there 
 is every reason to expect the most satisfactory results from the 
 experiment. 
 
 On account of threats of increased rental at our former 
 headquarters at 1510 Court Place, it was considered advisable 
 by the Executive Committee to make a change, and after 
 much painstaking labor by the committee appointed for the 
 purpose, the present quarters for our library and meeting 
 rooms were obtained at a rental of $50 per month, which in- 
 cludes light and janitor services. Our museum, which occu- 
 pies a large floor space, with the kindly consent of the school 
 authorities, was placed in the North Side High School Build- 
 ing, where it is open to the public and will, in addition, serve 
 as a stimulus to the students of the geological classes of that 
 school. 
 
 The assistant secretary, Miss Riddle, has rendered good 
 and efficient service, especially to the secretary and treasurer, 
 and for her zeal and ever loyal interest to the welfare of the 
 Society I wish to express, on behalf of all its members, our 
 grateful appreciation. 
 
 DR. WILLIAM A. JOHNSTON, 
 
 Secretary. 
 
REPORT OF THE TREASURER OF THE COLORADO 
 
 SCIENTIFIC SOCIETY FOR THE YEAR ENDING 
 
 DECEMBER 16TH, 1911. 
 
 418 Boston Building, Denver, Colo., Dec. 16th, 1911. 
 
 RECEIPTS. 
 
 Balance from statement of 1910... $ 351.11 
 
 Annual dues - 1,805.00 
 
 Rent - 455.00 
 
 Annual dinner 189.00 
 
 Sale of Proceedings 25.00 
 
 Life memberships 300.00 
 
 Cancelled fire insurance 16.80 
 
 Miscellaneous .. 10.30 
 
 $3,152.21 $3,152.21 
 DISBURSEMENTS. 
 
 Rent $1,100.00 
 
 Printing Proceedings 384165 
 
 Printing Notices, Ballots and Stationery.. 233.75 
 
 Lighting 28.95 
 
 Illustrating lectures 41.70 
 
 Postage and Envelopes 133.68 
 
 Fire insurance 86.20 
 
 Salary of assistant secretary 580.00 
 
 Petty cash 73.55 
 
 Periodicals, books and binding 39.00 
 
 Library furnishings and repairs 29.70 
 
 Exchange .75 
 
 Annual dinner 261.45 
 
 Moving to present quarters. 99.10 
 
 Engraving resolutions 6.00 
 
 Miscellaneous . 18.50 
 
 $3,116.98 $3,116.98 
 Cash on hand 35.23 
 
 $3,152.21 
 
REPORT OF THE TREASURER yii 
 
 This report shows a total collection of $2,801.10 as against 
 $2,819.00 in 1910, a falling off of $17.90. The total disburse- 
 ments as shown, were $3,116.98 as against $2,861.53 for 1910, 
 an increase of $255.45. 
 
 In analyzing and comparing the expenditures with those 
 of the previous year, you will find the comparison as follows : 
 
 DECREASE. 
 
 Rent account $100.00 
 
 Printing of Proceedings 80.55 
 
 Periodicals, books and binding 26.05 
 
 Exchange 1.20 
 
 Annual dinner 24.35 
 
 Miscellaneous .. 51.00 
 
 $283.15 
 INCREASE. 
 
 Printing Notices, Ballots, Circulars, etc.... $ 90.05 
 
 Lighting 6.20 
 
 Postage and envelopes 10.80 
 
 Insurance 17.40 
 
 Salary of assistant secretary 270.00 
 
 Petty cash 18.55 
 
 Library repairs and furnishings 12.80 
 
 Illustrating lectures 7.70 
 
 Moving 99.10 
 
 Engraving resolutions 6.00 
 
 $538.60 
 $283.15 
 
 $255.45 
 
 The chief items of increase fall on cost of printing notices, 
 ballots and stationery, which is due largely to the extra no- 
 tices and circulars sent out in connection with organizing of 
 
Viii REPORT OF THE TREASURER 
 
 the "Sections." The other two important items are the in- 
 crease in the salary of the assistant secretary, and the cost of 
 moving. Respectfully submitted, 
 
 J. W. RICHARDS, 
 
 Attest : Treasurer. 
 
 RICHARD A. PARKER, 
 
 Chairman. J- Auditing Committee. 
 FRANK E. SHEPARD. 
 
 December 18th, 1911. 
 
PROCEEDINGS OP THE COLORADO SCIENTIFIC SOCIETY. 
 VOL. X, pp: 123-130. 
 
 THE WATER SUPPLY OF COLORADO. 
 
 By CHARLES W. COMSTOCK. 
 
 Address of the Retiring President read at the meeting of the Society, December 16, 1911. 
 
 There is a well established custom among societies de- 
 voted to the advancement of learning, in accordance with which 
 the retiring presiding officer outlines a field wherein his con- 
 freres may labor with advantage for the discovery of prin- 
 ciples and the accumulation of facts which are needed in the 
 work-a-day world. Thus, while the papers and discussions of 
 the year are contributions toward the solution of problems 
 previously presented, the function of the address at the annual 
 meeting is to state another problem which has been forced to 
 the front amid the changing conditions and which demands 
 our attention. 
 
 Conforming to this custom, which I think an admirable 
 one, I have chosen to discuss a subject which has occupied 
 most of my attention for a number of years just past, viz.: 
 "The Water Supply of Colorado." 
 
 At the risk of being thought elementary, I must revert to 
 first principles and consider the source of all water, i. e., pre- 
 cipitation from the atmosphere. Rain or snow falls and im- 
 mediately divides itself among a number of channels. A por- 
 tion is again evaporated directly from the surface of the 
 ground or from the snow surface. Another portion sinks into 
 the ground, is absorbed by vegetation, and either becomes a 
 part of the plant itself, or is evaporated from its foliage. Still 
 another part finds its way into the ground far enough to be 
 beyond the reach of atmospheric influences and becomes part 
 of the great body of ground water. This third portion itself 
 
124 THE WATER SUPPLY OF COLORADO 
 
 may be subdivided into two, one becoming part of what is 
 ordinarily known as "ground water/' and the other joining the 
 deeper subterranean flow. Finally, a fourth portion runs off 
 the surface of the ground and finds its way into the channels 
 of surface streams. 
 
 All of this water, except that absorbed by vegetation, or 
 evaporated, may under proper conditions, become available for 
 use. The subterranean flow supplies artesian wells, of which 
 there are many in Colorado, particularly in the San Luis Val- 
 ley. 
 
 The ground water is in sufficient quantity in some parts 
 of the state to irrigate small tracts of land. The surface flow, 
 although probably only a small fraction of the total precipita- 
 tion, is relied upon to supply nearly all our demands for domes- 
 tic, agricultural and industrial purposes. 
 
 The division of the water among these various modes of 
 distribution varies widely with the geology, the topography and 
 the climate of the region in which the water flows, as well as 
 with the distribution in time of the precipitation itself. 
 
 To cite extreme cases : In the heart of the mountain ranges 
 where there is little soil, where the rocks are bare and the 
 slopes steep, where the altitude is high and the rocks generally 
 of a crystalline character, nearly all the water which falls 
 divides itself into two classes the first, covered by evapora- 
 tion, and the last covered by surface run-off. Although tem- 
 peratures are generally low in such localities, the winds blow 
 almost constantly, frequently with great violence, and the ten- 
 sion of the aqueous vapor in the atmosphere is very low. These 
 two conditions do more to increase evaporation than a high 
 temperature. Vegetation is scant .or entirely absent, and, 
 therefore, plays no part in the distribution of the water. There 
 is little or no soil, and the rocks are crystalline and compact. 
 Therefore, the quantity absorbed is relatively insignificant. On 
 the other hand, the slopes are steep and water runs very 
 rapidly to the natural drainage lines of the country. 
 
 Per contra, in the open prairie, such as forms the east- 
 ern forty per cent, of this state, all the conditions are changed. 
 
COMSTOCK] THE WATER SUPPLY OF COLORADO 125 
 
 The topographical relief is small and the slopes are slight. 
 There is a considerable quantity of vegetation, even on our 
 most barren plains. The soil and sub-soil are deep and often 
 very porous. Even the rocks themselves which underlie the 
 soil, or which outcrop in places, are sedimentary and capable of 
 absorbing large quantities of water. The temperatures are 
 higher, but the winds, as a rule, less constant, and the tension 
 of aqueous vapor generally greater. 
 
 We here find one condition which makes for greater evap- 
 oration than in the mountains, and two which tend to decrease 
 it. The net result we do not know. The water falling on por- 
 ous and absorbent soil with gradual slopes does not run off 
 readily, but is absorbed in large quantities. The precipitation 
 itself comes mostly in the form of rain in the warmer portions 
 of the year, whereas in the mountains it is chiefly in the form 
 of snow during the fall and winter months. The vegetation 
 directly absorbs some water and facilitates the evaporation of 
 more. 
 
 Thus we find that while in the mountains very little water 
 is absorbed by soil or rocks, on the plains a great deal is dis- 
 posed of in this way. The quantity evaporated on the plains, 
 as compared with the mountains, is unknown, but is known to 
 be very great, and some is absorbed by vegetation, which is 
 not the case at extremely high altitudes. 
 
 The general result is that the run-off from the plains 
 areas to the channels of the natural streams is insignificant, 
 except on those rare occasions of very great precipitation 
 within a short time. This distinction is so marked in what is 
 known as the "arid" or "semi-arid" region that the drainage 
 area of a stream is quite commonly divided into two portions 
 which are known respectively as "contributing" and "non- 
 contributing" areas. 
 
 To be enabled to make the best use of the water which 
 falls to our lot, we should know with accuracy the total quan- 
 tity supplied and the proportion of it which is disposed of in 
 these various ways, under the great variety of conditions 
 which exist in the state. 
 
126 THE WATER SUPPLY OF COLORADO 
 
 Three of the elements mentioned are capable of direct 
 measurement, viz. : 
 
 Precipitation ; 
 
 Surface run-off; 
 
 Evaporation. 
 
 Some work has also been done in attempts to measure the 
 absorption by and percolation through various soils. The re- 
 sults so far, however, have not been such as to warrant any 
 generalizations. 
 
 What do we know about precipitation in Colorado ? 
 
 The Monthly Weather Review, for September, 1911, an 
 official publication of the United States Weather Bureau, gives 
 a list of 156 rainfall stations in this state. Of these, forty-five 
 are in the Platte River drainage basin ; thirty-nine in the Ar- 
 kansas ; two in the water-shed of the Cimarron ; ten in the Rio 
 Grande basin, and sixty-two in the Colorado River drainage. 
 This totals 158, but two of these stations are counted twice; 
 that at Corona is common to the South Platte and the Colorado 
 drainage, while that at Marshall Pass is common to the Ar- 
 kansas and the Colorado. 
 
 The area of Colorado is 103,948 square miles. We thus 
 have on the average one rainfall station to each 663 square 
 miles, or, say, one to an area of twenty-six miles square. This 
 number might be considered adequate, if the conditions upon 
 which precipitation depends were even approximately uniform 
 throughout the state, which, however, they are not. 
 
 By way of comparison, we may note the distributions 
 of these stations in some other parts of the world. 
 
 In France the drainage basin of the Seine is 30,327 square 
 miles. The government there maintains 423 precipitation sta- 
 tions, or one to each seventy-two square miles. This is as 
 one for each two townships, as compared with one for each 
 eighteen townships in Colorado. 
 
 In the valley of the Rhone there is a precipitation station 
 for each ninety-six square miles ; in Switzerland, one for each 
 forty-four square miles. 
 
COMBTOCK] THE WATER SUPPLY OF COLORADO 127 
 
 The entire area of France is less than twice that of Colo- 
 rado, and if we would maintain precipitation records compar- 
 able with those abroad, we must have not less than 1,400 pre- 
 cipitation stations in the state of Colorado. Even the very 
 large number established in the basin of the Seine is deemed 
 insufficient by the engineers charged with the improvement 
 and maintenance of the water-ways in that region, and in the 
 most elaborate and exhaustive report on the flood of January, 
 1910, prepared by the government engineers and recently is- 
 sued by authority of the French government, a substantial in- 
 crease in the number of these stations is proposed. 
 
 At the present time, the practice in Colorado among those 
 who are not trained to scientific modes of thought, is to apply 
 the records of the nearest station to whatever area may be 
 under consideration, whether it be large or small, thus uncon- 
 sciously assuming a uniformity in the distribution of rainfall 
 which the most casual observer knows does not exist. 
 
 The question is frequently asked: What is the ratio of 
 run-off to rainfall in this or that drainage area ? This question 
 is not answerable for any drainage area in the state of Colo- 
 rado, for the obvious reason that we do not know how much 
 water falls in any such drainage area. 
 
 Meagre and unsatisfactory as our run-off records may be, 
 we know more about the total run-off than we do about the total 
 precipitation. 
 
 A second element directly measurable is the run-off, and 
 on this more money has been spent and more work done than 
 on any other, although the records and results are far from 
 satisfactory, partly because some of the work has been poorly 
 done, but chiefly because of lack of continuity. 
 
 Not counting stations maintained by private parties, the 
 records of which are not accessible to the public, there are 
 now seventy-three stream gauging stations in Colorado. Of 
 these, eighteen are located in the Platte water shed, twelve in 
 the Arkansas, nine in the Rio Grande, and thirty-four in the 
 drainage area of the Colorado. This last, of course, includes 
 
128 THE WATER SUPPLY OF COLORADO 
 
 more than one-third of all the state, being the entire area west 
 of the main range except that tributary to the Rio Grande. 
 
 This number, small as it is, is five times as great as it was 
 three years ago. It means an average of one stream gauging 
 station for each 1,424 square miles in the state. 
 
 In the basin of the Seine the French government main- 
 tains 120 stream gauging stations, or one for each 253 square 
 miles. 
 
 Concerning this phase of the water supply question, there 
 is little to be said except that there is need for greatly ex- 
 tending it, and strenuous efforts must be made to avoid any 
 break in the continuity of the records. 
 
 In the matter of evaporation measurements, almost noth- 
 ing has been done. Observations have been desultory and scat- 
 tered. Diligent search has failed to reveal more than one rec- 
 ord extending through an entire year. Such observations as 
 have been made have been made without uniformity of method 
 or procedure and are hardly comparable. 
 
 So far from being able to know the comparative evapora- 
 tion in the mountains and on the plains, we are not even in 
 position to state with definiteness the average annual evap- 
 oration at any one place in Colorado. This is without doubt a 
 task which should be undertaken by the State Hydrographic 
 Service, but it is a formidable one for several reasons. 
 
 Evaporation stations depend for their value upon measure- 
 ments which must be made with great precision and at fre- 
 quent intervals. This means the expenditure of a considerable 
 sum for the equipment of each station, and the attendance of a 
 skilled observer. The work cannot be entrusted to such observ- 
 ers as happen to be resident near the station, as is done with a 
 fair degree of satisfaction with stream gauging stations. Our 
 legislature should be asked to provide for an equipment of this 
 kind, and for the proper conduct of these observations. 
 
 With accurate knowledge of the total precipitation, the 
 total run-off, 'and the total evaporation, we can ascertain by 
 difference the quantity of water absorbed by the soil and the 
 
COMSTOCK] THE WATER SUPPLY OF COLORADO 129 
 
 vegetation. No method is apparent by which any direct meas- 
 urement of this quantity can be made. 
 
 Valuable work in the direction of the measurement of 
 ground water flow has been done during the past ten years 
 by a number of engineers following in the footsteps of Prof. 
 Charles S. Slichter. It is not unlikely that this may lead sooner 
 or later to some method by which we can determine directly the 
 quantity of water absorbed by the soil and its ultimate disposi- 
 tion. Along this line, I have nothing to suggest. 
 
 As said in my opening paragraph, I have only attempted 
 to state some problems demanding solution. The demand is 
 real, and the necessity for definite answers to some of these 
 questions is very great. For these reasons, it has seemed 
 proper and appropriate that they be called to the attention of 
 The Colorado Scientific Society.