A quasi three-dimensional model was constructed to simulate the response of the Piney Point and Cheswold aquifers underlying Kent County, Delaware to ground-water withdrawals. The model included the Magothy, Piney Point, Cheswold, and unconfined aquifers, and was calibrated using historical pumpage and water-level data. Model calibration was accomplished through the use of both steady-state and transient-state simulations.
Please give proper credit to the Delaware Geological Survey.
Leahy, P.P., 1982, Ground-Water Resources of the Piney Point and Cheswold Aquifers in Central Delaware as Determined by a Flow Model: Delaware Geological Survey Bulletin 16.
Delaware Geological Survey
University of Delaware
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Newark, DE 19716
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