HR: 0800h
AN: H31B-04    [Abstracts]
TI: MR2K: A Program to Calculate Drawdown, Velocity, Storage and Capture Response Functions
AU: * Maddock, T
EM: maddock@hwr.arizona.edu
AF: University of Arizona, Department of Hydrology 1133 E James E Rogers Way, Tucson, AZ 85721, United States
AB: A program, MR2K, used for calculating drawdown, velocity, storage loss, and capture response functions for multi-aquifer groundwater flow systems was developed. Capture is defined as the sum of the increase in aquifer recharge and decrease in aquifer discharge as a result of an applied stress from groundwater pumping. The capture phenomena treated are stream-aquifer leakance, reduction of evapotranspiration losses, flows to and from prescribed head boundaries, and increases or decreases in natural recharge or discharge from head- dependent boundaries. The response functions are independent of the magnitude of the pumping stresses, and are dependent on the type of partial differential equation, boundary and initial conditions and the parameters thereof, and the spatial and temporal locations of stresses. The aquifers modeled may have irregular-shaped boundaries and non- homogeneous transmissive and storage qualities. The stresses are groundwater withdrawals from wells. The utility of response functions arises from their capacity to be embedded in management models such as decision support systems. The response functions are incorporated into the objective function or constraints that couple the hydrologic system with the management system. Three response-function examples are presented for a hypothetic basin.
DE: 1800 HYDROLOGY
DE: 1830 Groundwater/surface water interaction
DE: 1880 Water management (6334)
SC: Hydrology [H]
MN: 2007 Joint Assembly