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

Loading next page...
 
/lp/wiley/theoretical-analysis-of-regional-groundwater-flow-1-analytical-and-acWe6qHeI6
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

References

  • Variation of the permeability tensor ellipsoid in homogeneous anisotropic soils
    Liakopoulos, Liakopoulos
  • Capillary conduction of liquids through porous mediums
    Richards, Richards

You’re reading a free preview. Subscribe to read the entire article.


DeepDyve is your
personal research library

It’s your single place to instantly
discover and read the research
that matters to you.

Enjoy affordable access to
over 18 million articles from more than
15,000 peer-reviewed journals.

All for just $49/month

Explore the DeepDyve Library

Search

Query the DeepDyve database, plus search all of PubMed and Google Scholar seamlessly

Organize

Save any article or search result from DeepDyve, PubMed, and Google Scholar... all in one place.

Access

Get unlimited, online access to over 18 million full-text articles from more than 15,000 scientific journals.

Your journals are on DeepDyve

Read from thousands of the leading scholarly journals from SpringerNature, Elsevier, Wiley-Blackwell, Oxford University Press and more.

All the latest content is available, no embargo periods.

See the journals in your area

DeepDyve

Freelancer

DeepDyve

Pro

Price

FREE

$49/month
$360/year

Save searches from
Google Scholar,
PubMed

Create folders to
organize your research

Export folders, citations

Read DeepDyve articles

Abstract access only

Unlimited access to over
18 million full-text articles

Print

20 pages / month

PDF Discount

20% off