Approximate Solution of Unsteady Groundwater Flows

Approximate Solution of Unsteady Groundwater Flows

Kantorovich's method for obtaining approximate solutions to problems of unsteady diffusion of heat and momentum is applied to unsteady ground water seepage flow problems. Simple profiles satisfying free surface boundary conditions in the spatial domain are assumed, leaving the time dependence t...

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Veröffentlicht in:Journal of hydraulic engineering (New York, N.Y.) N.Y.), 1986-10, Vol.112 (10), p.971-975
1. Verfasser: Onyegegbu, Samuel O
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Sprache:eng
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Applied sciences
Buildings. Public works
Exact sciences and technology
TECHNICAL NOTES
Water supply. Pipings. Water treatment
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container_title Journal of hydraulic engineering (New York, N.Y.)
container_volume 112
creator Onyegegbu, Samuel O
description Kantorovich's method for obtaining approximate solutions to problems of unsteady diffusion of heat and momentum is applied to unsteady ground water seepage flow problems. Simple profiles satisfying free surface boundary conditions in the spatial domain are assumed, leaving the time dependence to be determined from the governing equations. The governing nonlinear partial differential equation is thus reduced to a nonlinear ordinary differential equation whose exact solution is easily obtained. Results obtained using second-order profiles for both the sudden buildup case and the sudden drawdown case compare well with experimental data.
doi_str_mv 10.1061/(ASCE)0733-9429(1986)112:10(971)
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1943-7900
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source American Society of Civil Engineers:NESLI2:Journals:2014
subjects Applied sciences
Buildings. Public works
Exact sciences and technology
TECHNICAL NOTES
Water supply. Pipings. Water treatment
title Approximate Solution of Unsteady Groundwater Flows
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