Analytic elements for flow in layered, anisotropic aquifers

Kick Hemker; Mark Bakker

doi:10.1016/S0167-5648(02)80135-6

Analytic elements for flow in layered, anisotropic aquifers

Kick Hemker^*, Mark Bakker

^*Corresponding author for this work

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

2 Citations (Scopus)

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.

Original language	English
Pages (from-to)	753-754
Number of pages	2
Journal	Developments in Water Science
Volume	47
Issue number	C
DOIs	https://doi.org/10.1016/S0167-5648(02)80135-6
Publication status	Published - 2002
Externally published	Yes

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10.1016/S0167-5648(02)80135-6

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title = "Analytic elements for flow in layered, anisotropic aquifers",

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.",

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AU - Bakker, Mark

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AB - 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.

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DO - 10.1016/S0167-5648(02)80135-6

M3 - Article

AN - SCOPUS:77956711449

SN - 0167-5648

VL - 47

SP - 753

EP - 754

JO - Developments in Water Science

JF - Developments in Water Science

IS - C

ER -

Analytic elements for flow in layered, anisotropic aquifers

Abstract

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