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Further evidence of hysteresis as a factor in the evaporation from soils

dc.contributor.authorKing, Larry G., author
dc.contributor.authorSchleusener, Richard A., author
dc.date.accessioned2022-05-17T19:14:20Z
dc.date.available2022-05-17T19:14:20Z
dc.date.issued1961
dc.descriptionAtmospheric science technical paper no. 13 stamped on title page.
dc.descriptionFrom the Journal of Geophysical Research, volume 66, no. 12, December 1961.
dc.description.abstractEvaporation studies were conducted on a fine sand which was in contact with a water table and was subjected to diurnal cyclic atmospheric conditions. Previous studies under steady atmospheric conditions showed that an inverse relation between the rate of evaporation from soils and the rate of evaporation from a free-water surface occurred under certain conditions. These studies also showed that this inverse relationship was produced by decreased evaporativity as the depth to the water table was increased. A theoretical explanation of this phenomenon was presented on the basis of a hysteresis in the functional relation between permeability and saturation of soils. The data presented in the present paper show that this phenomenon also occurs under cyclic atmospheric conditions. The conclusion is that the inverse relationship could occur in soils under field conditions, and therefore it could be a significant cosideration in predicting evaporation from soils.
dc.format.mediumreports
dc.identifier.urihttps://hdl.handle.net/10217/235045
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationCatalog record number (MMS ID): 991023742539703361
dc.relationQC852 .C58 no. 13
dc.relation.ispartofAtmospheric Science Papers (Blue Books)
dc.relation.ispartofAtmospheric science technical paper, no. 13
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subjectEvaporation
dc.subjectSoil moisture -- Colorado -- Measurement
dc.subjectHysteresis
dc.titleFurther evidence of hysteresis as a factor in the evaporation from soils
dc.typeText
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