Steady non-Darcy seepage through confined aquifer of variable thickness
DOI:
https://doi.org/10.54302/mausam.v31i1.4296Abstract
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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