A MODELING EVALUATION OF A METHOD FOR ESTIMATING GROUNDWATER USAGE BY PHREATOPHYTES
The USGS Variably Saturated 2-Dimensional (VS2D) model was used to simulate water flow in the vicinity of the water table as influenced by daily transpiration patterns. The simulated water-table fluctuations were analyzed using the White method. We found that this method can accurately quantify groundwater consumption if an appropriate value for the readily available specific yield is used. Results indicate that the readily available specific yield is generally less than the difference between the saturated water content and the residual water content for two reasons. First, the time scale over which the fluctuations are observed does not allow the soil moisture profiles to reach equilibrium. Second, in cases where the water table is near the ground surface, the thin vadose zone cannot release as much water as a thicker unsaturated zone. We determined that typical values of readily available specific yield can be obtained based on the textual characteristics of the sediment. An example application of the use of the White method for estimating groundwater consumption by transpiration in a riparian zone in west central Kansas will be presented.