Unsteady Groundwater flow towards a well
DOI:
https://doi.org/10.4314/just.v9i1.1106Abstract
An alternative equation is derived to predict the variation of drawdown in a well with time in an extensive, homogeneous and isotropic aquifer. The equation is in the form of a series involving Bessel Functions of the zero and first order. The predicted variation of drawdown with time by this equation is found to be in excellent agreement with field data.
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