Estimation of Hydraulic Parameters from an Unconfined Aquifer Test Conducted in aGlacial Outwash Deposit, Cape Cod, Massachusetts

摘要

An acquifer test conducted in a sand and gravel, glacial outwash deposit on CapeCod, Massachusetts was analyzed by means of a model for flow to a partially penetrating well in a homogeneous, anisotropic unconfined aquifer. The model is designed to account for all significant mechanisms expected to influence drawdown in observation piezometers and in the pump well.