File:Dry farming in relation to rainfall and evaporation (1910) (14772726175).jpg

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Identifier: dryfarminginrela188brig (find matches)
Title: Dry farming in relation to rainfall and evaporation
Year: 1910 (1910s)
Authors: Briggs, Lyman J. (Lyman James), 1874-1963 United States. Department of Agriculture United States. Bureau of Plant Industry United States. Government Printing Office
Subjects: Dry farming
Publisher: Washington DC : G.P.O.
Contributing Library: U.S. Department of Agriculture, National Agricultural Library
Digitizing Sponsor: U.S. Department of Agriculture, National Agricultural Library

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e the small summer showers that are use-less on summer-tilled land always help the growing crop. Thus wehave a radically different system of farm practice in the Great Plainsfrom that found in the Intermountain country, owing in part to thedifference in the distribution of the monthly rainfall of the tworegions and in part to the greater rainfall in the Great Plains. THE RELATION OF THE CHARACTER OF RAINFALL TO ITS USE-FULNESS. The way in which the rain comes has a great deal to do with itsusefulness. Summer-fallowing methods, for example, are not welladapted to regions in which the rainfall comes largely in the form oflittle showers from one-tenth to one-half inch. Rains of this kindpenetrate the soil only a few inches, and the water is practically all a See Arid Farming in Utah, by Widtsoe and Merrill, Bulletin 91, Utah Agricul-tural Experiment Station; also Dry Farming in the Great Basin, by C. S. Scofield,Bulletin 103, Bureau of Plant Industry, U. S. Department of Agriculture,18§
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Briggs, Lyman J. (Lyman James), 1874-1963; United States. Department of Agriculture; United States. Bureau of Plant Industry;

United States. Government Printing Office
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no.188
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29 July 2014
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