Allen Philip_Basin Analysis.pdf

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Soil surface Discrete moisture films at grain contacts Continuous moisture films forming :r an interconnected system of & capillary films. Moisture content increasing with depth Continuous moisture films with entrapped air pockets. Moisture content at capillary saturation Water table h =height of equivalent rise in a capillary tube Fig. 7.1 The zones of moisture in the regolith, sho.,.mg the extent of the capillary fringe (after Carson 1969). critical to
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