Copyright & Fair-use Agreement
UNLV Special Collections provides copies of materials to facilitate private study, scholarship, or research. Material not in the public domain may be used according to fair use of copyrighted materials as defined by copyright law. Please cite us.
Please note that UNLV may not own the copyright to these materials and cannot provide permission to publish or distribute materials when UNLV is not the copyright holder. The user is solely responsible for determining the copyright status of materials and obtaining permission to use material from the copyright holder and for determining whether any permissions relating to any other rights are necessary for the intended use, and for obtaining all required permissions beyond that allowed by fair use.
Read more about our reproduction and use policy.
I agree.Information
Digital ID
Permalink
Details
Member of
More Info
Rights
Digital Provenance
Publisher
Transcription
^ Phosphorous Pentoxide (P.2 0 5)----—0.23 per cent Sulphur Trioxide (S.0.3) —---——0.52 * Carbon Dioxide (C.0.2) ----— ---3.24 * Volatile Matter--------------------- 3.15 " Humus-------------------0.78 per cent Nitrogen in humus---—-10.91 " * Ash-----------------------0.65 " ® Sol. Phos. Acid---------0.01 w ® This soil is a sandy loam containing a large quantity of all the mineral constituents necessary for plant life. This soil is especially rich in the most important plant constituents such as phosphoric acid, potash and lime* The soil does not contain an excess of alkali forming salts. From the analysis submitted and from my knowledge of soils of this character, X have no doubt but that it is well adapted to vines, vegetables, deciduous fruits and alfalfa. There is no tendency on this tract to an excess of alkali, and I have no hesitation at all in saying that the soil is first class in every respect. The Water. I do not believe that Mr. Bull or his associates have done any work in actual development of water. It is true that there are a number of wells in the walley and that these wells are evidently successful. Although I asked Mr. Bull repeatedly as to the wells and as to the ffjjfew, I was unable to get any information on this matter. I did, however, visit wells in the valley that have been dug by other people. I visited particularly a well belonging to Mr. Keith, who is in the N.F.Quarter of Sec.6, Township 10 N., Range 4 E. Hr. Keith was present and said that his well was 210 feet deep and that the water level is 190 feet. In digging - 2-