Steady non-Darcy seepage through confined aquifer of variable thickness

Authors

  • P. BASAK Centre for Water Resources Development and Management, Calicut
  • J. P. SONI Department of Civil Engineering, Punjab Agricultural University, Ludhiana, Punjab

DOI:

https://doi.org/10.54302/mausam.v31i1.4296

Abstract

A steady state analytical solution for the case of confined aquifer of variable thickness incorporating Forchheimer's non-linear velocity gradient response (i=av+bv2) is presented. The solution is compared with the available solution for Darcian linear flow. The effect of non-linearity in the flow response on the discharge characteristics and the piezometric pressure distribution in relation to the corresponding linear case is brought out.

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Published

1980-01-01

Issue

Vol. 31 No. 1 (1980): MAUSAM

Section

Shorter Contribution

Categories

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How to Cite

[1]
“Steady non-Darcy seepage through confined aquifer of variable thickness ”, MAUSAM, vol. 31, no. 1, pp. 145–150, Jan. 1980, doi: 10.54302/mausam.v31i1.4296.