Transient drawdown solution for a constant pumping test in finite two-zone confined aquifers

13Citations
Citations of this article
8Readers
Mendeley users who have this article in their library.

Abstract

The drawdown solution has been widely used to analyze pumping test data for the determination of aquifer parameters when coupled with an optimization scheme. The solution can also be used to predict the drawdown due to pumping and design the dewatering system. The drawdown solution for flow toward a finite-radius well with a skin zone in a confined aquifer of infinite extent in radial direction had been developed before. To our best knowledge, the drawdown solution in confined aquifers of finite extent with a skin zone so far has never before been presented in the groundwater literature. This article presents a mathematical model for describing the drawdown distribution due to a constant-flux pumping from a finite-radius well with a skin zone in confined aquifers of finite extent. The analytical solution of the model is developed by applying the methods of Laplace transforms, Bromwich contour integral, and residue theorem. This solution can be used to investigate the effects of finite boundary and conductivity ratio on the drawdown distribution. In addition, the inverse relationship between Laplace- and time-domain variables is used to develop the large time solution which can reduce to the Thiem solution if there is no skin zone. © Author(s) 2012.

Cite

CITATION STYLE

APA

Wang, C. T., Yeh, H. D., & Tsai, C. S. (2012). Transient drawdown solution for a constant pumping test in finite two-zone confined aquifers. Hydrology and Earth System Sciences, 16(2), 441–449. https://doi.org/10.5194/hess-16-441-2012

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free