Distributed sources for unconfined groundwater flow in a half-space

O. D.L. Strack

doi:10.1016/0022-1694(78)90003-3

Distributed sources for unconfined groundwater flow in a half-space

O. D.L. Strack

Civil, Environmental, and Geo- Engineering

Research output: Contribution to journal › Article › peer-review

6 Scopus citations

Abstract

The exact solution to a problem of unconfined saturated flow of groundwater in a semi-infinite homogeneous and isotropic permeable medium is presented. The inflow and outflow occurs along an arbitrary number of segments of the phreatic surface. The inflow and outflow rates are constant along each segment but may vary from segment to segment. The solution is determined by conformal mapping techniques applying boundary integrals.

Original language	English (US)
Pages (from-to)	239-253
Number of pages	15
Journal	Journal of Hydrology
Volume	39
Issue number	3-4
DOIs	https://doi.org/10.1016/0022-1694(78)90003-3
State	Published - Dec 1978

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title = "Distributed sources for unconfined groundwater flow in a half-space",

abstract = "The exact solution to a problem of unconfined saturated flow of groundwater in a semi-infinite homogeneous and isotropic permeable medium is presented. The inflow and outflow occurs along an arbitrary number of segments of the phreatic surface. The inflow and outflow rates are constant along each segment but may vary from segment to segment. The solution is determined by conformal mapping techniques applying boundary integrals.",

author = "Strack, {O. D.L.}",

year = "1978",

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T1 - Distributed sources for unconfined groundwater flow in a half-space

AU - Strack, O. D.L.

PY - 1978/12

Y1 - 1978/12

N2 - The exact solution to a problem of unconfined saturated flow of groundwater in a semi-infinite homogeneous and isotropic permeable medium is presented. The inflow and outflow occurs along an arbitrary number of segments of the phreatic surface. The inflow and outflow rates are constant along each segment but may vary from segment to segment. The solution is determined by conformal mapping techniques applying boundary integrals.

AB - The exact solution to a problem of unconfined saturated flow of groundwater in a semi-infinite homogeneous and isotropic permeable medium is presented. The inflow and outflow occurs along an arbitrary number of segments of the phreatic surface. The inflow and outflow rates are constant along each segment but may vary from segment to segment. The solution is determined by conformal mapping techniques applying boundary integrals.

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U2 - 10.1016/0022-1694(78)90003-3

DO - 10.1016/0022-1694(78)90003-3

M3 - Article

AN - SCOPUS:0018159890

SN - 0022-1694

VL - 39

SP - 239

EP - 253

JO - Journal of Hydrology

JF - Journal of Hydrology

IS - 3-4

ER -

Distributed sources for unconfined groundwater flow in a half-space

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