| dc.contributor.author |
Bakker, M |
en |
| dc.date.accessioned |
2014-06-06T06:45:44Z |
|
| dc.date.available |
2014-06-06T06:45:44Z |
|
| dc.date.issued |
2004 |
en |
| dc.identifier.issn |
03091708 |
en |
| dc.identifier.uri |
http://dx.doi.org/10.1016/j.advwatres.2004.02.015 |
en |
| dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/2585 |
|
| dc.subject |
Analytic element method |
en |
| dc.subject |
Elliptical inhomogeneity |
en |
| dc.subject |
Elliptical lake |
en |
| dc.subject |
Groundwater-surface water interaction |
en |
| dc.subject.other |
Aquifers |
en |
| dc.subject.other |
Boundary conditions |
en |
| dc.subject.other |
Difference equations |
en |
| dc.subject.other |
Groundwater |
en |
| dc.subject.other |
Lakes |
en |
| dc.subject.other |
Laplace transforms |
en |
| dc.subject.other |
Problem solving |
en |
| dc.subject.other |
Steady flow |
en |
| dc.subject.other |
Aquifer transmissivity |
en |
| dc.subject.other |
Discharge potential |
en |
| dc.subject.other |
Elliptical boundaries |
en |
| dc.subject.other |
Leaky lake beds |
en |
| dc.subject.other |
Water resources |
en |
| dc.subject.other |
analytical method |
en |
| dc.subject.other |
aquifer |
en |
| dc.subject.other |
flow modeling |
en |
| dc.subject.other |
groundwater flow |
en |
| dc.subject.other |
inhomogeneity |
en |
| dc.title |
Modeling groundwater flow to elliptical lakes and through multi-aquifer elliptical inhomogeneities |
en |
| heal.type |
journalArticle |
en |
| heal.identifier.primary |
10.1016/j.advwatres.2004.02.015 |
en |
| heal.publicationDate |
2004 |
en |
| heal.abstract |
Two new analytic element solutions are presented for steady flow problems with elliptical boundaries. The first solution concerns groundwater flow to shallow elliptical lakes with leaky lake beds in a single-aquifer. The second solution concerns groundwater flow through elliptical cylinder inhomogeneities in a multi-aquifer system. Both the transmissivity of each aquifer and the resistance of each leaky layer may differ between the inside and the outside of an inhomogeneity. The elliptical inhomogeneity may be bounded on top by a shallow elliptical lake with a leaky lake bed. Analytic element solutions are obtained for both problems through separation of variables of the Laplace and modified-Helmholtz differential equations in elliptical coordinates. The resulting equations for the discharge potential consist of infinite sums of products of exponentials, trigonometric functions, and modified-Mathieu functions. The series are truncated but still fulfill the differential equation exactly; boundary conditions are met approximately, but up to machine accuracy provided enough terms are used. The head and flow may be computed analytically at any point in the aquifer. Examples are given of uniform flow through an elliptical lake, a well pumping near two elliptical lakes, and uniform flow through three elliptical inhomogeneities in a multi-aquifer system. Mathieu functions may be applied in a similar fashion to solve other groundwater flow problems in semi-confined aquifers and leaky aquifer systems with elliptical internal or external boundaries. © 2004 Elsevier Ltd. All rights reserved. |
en |
| heal.journalName |
Advances in Water Resources |
en |
| dc.identifier.issue |
5 |
en |
| dc.identifier.volume |
27 |
en |
| dc.identifier.doi |
10.1016/j.advwatres.2004.02.015 |
en |
| dc.identifier.spage |
497 |
en |
| dc.identifier.epage |
506 |
en |