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A mathematical model for describing groundwater flow to a partially penetrating pumping well of a finite diameter in an anisotropic leaky confined aquifer is developed. The model accounts for the jointed effects of aquitard storage, aquifer anisotropy, and wellbore storage by treating the aquitard leakage as a boundary condition at the aquitard–aquifer interface rather than a volumetric source/sink...
We have discussed pumping induced leakage in a leaky-confined aquifer bounded by a relatively thin aquitard whose storage effect is neglected. Both constant-rate and constant-drawdown, fully penetrating vertical pumping wells are considered. We have derived closed-form analytical solutions of the steady-state leakage rates and volumes within any given radial distance from the well for both the constant-rate...
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