A generalized solution for groundwater head fluctuation in a tidal leaky aquifer system

17Citations
Citations of this article
5Readers
Mendeley users who have this article in their library.
Get full text

Abstract

A new analytical solution is developed for describing groundwater level fluctuations in a coupled leaky confined aquifer system which consists of an unconfined aquifer, confined aquifer, and an aquitard in between. The aquifer system has a tidal boundary at the seashore, a no flow boundary at remote inland side, and a confined aquifer extending under the sea and terminated with an outlet-capping. This new solution has shown to be a generalisation of most existing analytical solutions for a tidal aquifer system which includes single confined and leaky confined aquifers. In addition, the solution is used to explore the influences of the dimensionless leakance of the outlet-capping, the dimensionless hydraulic diffusivities, and the leakages of the inland and offshore aquitards on the head responses in the leaky confined aquifer. © Indian Academy of Sciences.

Cite

CITATION STYLE

APA

Chuang, M. H., & Yeh, H. D. (2011). A generalized solution for groundwater head fluctuation in a tidal leaky aquifer system. Journal of Earth System Science, 120(6), 1055–1066. https://doi.org/10.1007/s12040-011-0128-8

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