Abstract
ABSTRACT ADYNAMIC simulation model has been developed to trace the movement of precipitation to the water table. One submodel uses measured precipitation to simulate the amount and distribution of water leaving the root zone. A second sub-model describes the subsequent movement of this water until it reaches the phreatic surface. The model has been used to simulate conditions on a Piedmont watershed with a water table at approximately 20 m depth. The results presented include computed evapotranspiration, moisture profiles for the un-saturated region and water table movement as compared to observed data.
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