Steady-State Unconfined Aquifer Simulation of the Gareh-Bygone Plain, Iran : Steady-State Unconfined Aquifer Simulation
The first step of aquifer parameter and dependent variable estimation based on hydraulic modeling is generally to choose the best steady-state condition for the set time period. In order to define the best estimated hydraulic conductivity and boundary condition for Gareh-Bygone Plain in arid southern Iran, ten different steady-state conditions were simulated and calibrated with limited field obser