The Laplace transform solution of a one dimensional groundwater recharge by spreading
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Abstract
An analytical expression for the moisture content distribution,
in a problem of one dimensional vertical groundwater recharge, has
been obtained by using the Laplace transform method. The average diffusivity coefficient over the whole range of moisture content is regarded as constant, and a linear variation of permeability with moisture content is assumed.
in a problem of one dimensional vertical groundwater recharge, has
been obtained by using the Laplace transform method. The average diffusivity coefficient over the whole range of moisture content is regarded as constant, and a linear variation of permeability with moisture content is assumed.
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How to Cite
(1)
VERMA, A. P. The Laplace Transform Solution of a One Dimensional Groundwater Recharge by Spreading. Ann. Geophys. 1969, 22 (1), 25-31. https://doi.org/10.4401/ag-5079.
