| dc.contributor.author |
Hemker, K |
en |
| dc.contributor.author |
Bakker, M |
en |
| dc.date.accessioned |
2014-06-06T06:44:47Z |
|
| dc.date.available |
2014-06-06T06:44:47Z |
|
| dc.date.issued |
2002 |
en |
| dc.identifier.issn |
01675648 |
en |
| dc.identifier.uri |
http://dx.doi.org/10.1016/S0167-5648(02)80135-6 |
en |
| dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/2068 |
|
| dc.title |
Analytic elements for flow in layered, anisotropic aquifers |
en |
| heal.type |
journalArticle |
en |
| heal.identifier.primary |
10.1016/S0167-5648(02)80135-6 |
en |
| heal.publicationDate |
2002 |
en |
| heal.abstract |
The Girinski potential for groundwater flow in stratified aquifers has been extended to allow for a different anisotropic horizontal hydraulic conductivity in each layer. The difference in anisotropy between layers creates a three-dimensional flow field, which may become complicated, for example near wells. © 2002 Elsevier B.V. All rights reserved. |
en |
| heal.journalName |
Developments in Water Science |
en |
| dc.identifier.issue |
C |
en |
| dc.identifier.volume |
47 |
en |
| dc.identifier.doi |
10.1016/S0167-5648(02)80135-6 |
en |
| dc.identifier.spage |
753 |
en |
| dc.identifier.epage |
754 |
en |