Three methods to calculate the unsaturated conductivity of soil from its moisture characteristic were tested. Calculated values were compared with direct measurements of conductivity for both sorption and desorption for a sand. Also, comparisons were made for three soil materials. The method of calculation proposed by Millington and Quirk (1959), when matched at the saturated conductivity, gave good results.
Water Resources Research – Wiley
Published: Sep 1, 1965
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