MEASURED AND APPROXIMATE FLUX-CONCENTRATION RELATIONS FOR ABSORPTION OF WATER BY SOIL.
Abstract
The flux-concentration relation of J. R. Philip is calculated using moisture profiles measured during absorption of water by a fine sand when water was supplied at both constant hydraulic potential and constant The general The general behavior of the measured flux-concentration relations was found to be consistent with those of the model soils calculated by Philip. Within the accuracy of the measurements, no significant time-dependence of the relation was found for the constant flux boundary condition over a large time span.
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Soil Science Society of America Journal
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