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Developing joint probability distributions of soil water retention characteristics

Water Resources Research · 1988 · Vol. 24(5) · pp. 755–769

Abstract

A method is presented for developing probability density functions for parameters of soil moisture relationships of capillary head [ h (θ)] and hydraulic conductivity [ K (θ)]. These soil moisture parameters are required for the assessment of water flow and solute transport in unsaturated media. The method employs a statistical multiple regression equation proposed in the literature for estimating [ h (θ)] or [ K (θ)] relationships using the soil saturated water content and the percentages of sand and clay. In the absence of known statistical distributions for either [ h (θ)] or [ K (θ)] relationships, the method facilitates modeling by providing variability estimates that can be used to examine the uncertainty associated with water flow or solute transport in unsaturated media.

Soil and Unsaturated FlowGroundwater flow and contamination studiesSoil Moisture and Remote SensingHydraulic conductivityWater contentSoil scienceVadose zoneEnvironmental scienceFlow (mathematics)Soil waterProbability distributionJoint probability distributionWater flow
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