INTERACTION OF STREAM AND SLOPING AQUIFER RECEIVING CONSTANT RECHARGE

Definition sketch for discharging aquifer with constant replenishment. Analytical solution and special cases : no recharge occurs in a sloping aquifer , stream and horizontal aquifer interaction with or without constant recharge, sudden change in water level in the stream. Finite-element solution of non-linear Boussinesq equation and application with numerical example and analytical solution for water table variation in horizontal sloping aquifer due to stream aquifer interaction. Comparison of water table heights obtained by each method.