Abstract
The exact solution for the drawdown in and around a well of large diameter in a homogeneous, isotropic leaky aquifer induced by a time-dependent pumping rate is presented. The effect of the storage capacity of the well is considered. The leakage is assumed to be at a rate proportional to the drawdown at any point in the aquifer, i.e., linear leakage proposed by Jacob. Typical drawdown curves are presented in graphs by numerical integration of the analytic solution for various time-dependent pumping rates.
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