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Theoretical analysis of regional groundwater flow: 1. Analytical and numerical solutions to the mathematical model

Theoretical analysis of regional groundwater flow: 1. Analytical and numerical solutions to the... It is possible to represent steady‐state regional groundwater flow in a three‐dimensional, nonhomogeneous, anisotropic basin by a mathematical model. The numerical finite‐difference approach can be used to solve the general case; the analytical separation of variables technique is restricted to two‐dimensional layered mediums. The numerical method is more versatile, mathematically simpler, and well suited to computer oriented methods of data storage. Computer results are in the form of plotted potential nets from which flow patterns can be constructed. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Water Resources Research Wiley

Theoretical analysis of regional groundwater flow: 1. Analytical and numerical solutions to the mathematical model

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References (21)

Publisher
Wiley
Copyright
Copyright © 1966 by the American Geophysical Union.
ISSN
0043-1397
eISSN
1944-7973
DOI
10.1029/WR002i004p00641
Publisher site
See Article on Publisher Site

Abstract

It is possible to represent steady‐state regional groundwater flow in a three‐dimensional, nonhomogeneous, anisotropic basin by a mathematical model. The numerical finite‐difference approach can be used to solve the general case; the analytical separation of variables technique is restricted to two‐dimensional layered mediums. The numerical method is more versatile, mathematically simpler, and well suited to computer oriented methods of data storage. Computer results are in the form of plotted potential nets from which flow patterns can be constructed.

Journal

Water Resources ResearchWiley

Published: Dec 1, 1966

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