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Assessing the Bare Soil Evaporation Via Surface Temperature Measurements

From the Proceedings of the 1975 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 11-12, 1975, Tempe, Arizona / Evaporation of water from bare soils is an important consideration in the scheduling of many farming operations in both irrigated and dryland agriculture. Accurate predictions of bare soil evaporation can serve as the basis for decisions to increase the acreage planted with a given crop. An alternative is presented to previous approaches to bare soil evaporation estimation by empirically correlating the ratio of daily totals of actual to potential evaporation and the amplitude of the diurnal surface soil temperature wave. Since evaporation is directly related to the surface soil water pressure, the soil thermal inertia technique might be capable of prescribing relative bare soil evaporation rates which, combined with potential evaporation calculations, could allow determination of actual evaporation rates over the entire range of soil drying.

Identiferoai:union.ndltd.org:arizona.edu/oai:arizona.openrepository.com:10150/300530
Date12 April 1975
CreatorsIdso, Sherwood B., Reginato, Robert J., Jackson, Ray D.
ContributorsAgricultural Research Service, U.S. Department of Agriculture, ARS, USDA, U. S. Water Conservation Laboratory, Phoenix, Arizona 85040
PublisherArizona-Nevada Academy of Science
Source SetsUniversity of Arizona
Languageen_US
Detected LanguageEnglish
Typetext, Proceedings
RightsCopyright ©, where appropriate, is held by the author.

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