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Unsteady Seepage toward Narrow Ditch
A linearized solution is obtained for the unsteady, free surface seepage toward a ditch in an infinitely deep aquifer. The complex potential is defined to be the solution of a first order, linear, partial differential equation, and examination of the general solution for this equation reveals that a seepage surface cannot be imposed along the ditch boundary in the linearized model. A numerical example is treated, and it is pointed out that the same results can be used to describe the unsteady recharge of an aquifer under similar boundary conditions.
Unsteady Seepage toward Narrow Ditch
A linearized solution is obtained for the unsteady, free surface seepage toward a ditch in an infinitely deep aquifer. The complex potential is defined to be the solution of a first order, linear, partial differential equation, and examination of the general solution for this equation reveals that a seepage surface cannot be imposed along the ditch boundary in the linearized model. A numerical example is treated, and it is pointed out that the same results can be used to describe the unsteady recharge of an aquifer under similar boundary conditions.
Unsteady Seepage toward Narrow Ditch
Hunt, Bruce W. (Autor:in)
Journal of the Hydraulics Division ; 96 ; 1953-1963
01.01.2021
111970-01-01 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
Erratum for “Unsteady Seepage toward Narrow Ditch”
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