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1987 | OriginalPaper | Chapter

Unconfined Groundwater Flow

Author : G. P. Lennon

Published in: Applications in Geomechanics

Publisher: Springer Berlin Heidelberg

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The general equation governing unconfined groundwater flow is a transient, three-dimensional partial differential equation with variable coefficients. As summarized in this chapter, for many problems the equation can be simplified such that the associated free space Green’s function is known. Then the Boundary Element Method (BEM) becomes a very efficient technique for solving for the location of the transient free surface.

Metadata
Title
Unconfined Groundwater Flow
Author
G. P. Lennon
Copyright Year
1987
Publisher
Springer Berlin Heidelberg
DOI
https://doi.org/10.1007/978-3-642-83012-9_8

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