Analytic element modeling of embedded multiaquifer domains

dc.contributor.author	Bakker, M	en
dc.date.accessioned	2014-06-06T06:46:45Z
dc.date.available	2014-06-06T06:46:45Z
dc.date.issued	2006	en
dc.identifier.issn	0017467X	en
dc.identifier.uri	http://dx.doi.org/10.1111/j.1745-6584.2005.00080.x	en
dc.identifier.uri	http://62.217.125.90/xmlui/handle/123456789/3175
dc.subject.other	Approximation theory	en
dc.subject.other	Leakage (fluid)	en
dc.subject.other	Mathematical models	en
dc.subject.other	Analytic element modeling	en
dc.subject.other	Multiaquifer domains	en
dc.subject.other	Single-aquifer models	en
dc.subject.other	Aquifers	en
dc.subject.other	aquifer	en
dc.subject.other	hydraulic head	en
dc.subject.other	hydrogeology	en
dc.subject.other	leakage	en
dc.subject.other	mathematical analysis	en
dc.subject.other	algorithm	en
dc.subject.other	article	en
dc.subject.other	comparative study	en
dc.subject.other	environmental monitoring	en
dc.subject.other	finite element analysis	en
dc.subject.other	forecasting	en
dc.subject.other	hydrostatic pressure	en
dc.subject.other	river	en
dc.subject.other	theoretical model	en
dc.subject.other	water flow	en
dc.subject.other	water supply	en
dc.subject.other	Algorithms	en
dc.subject.other	Environmental Monitoring	en
dc.subject.other	Finite Element Analysis	en
dc.subject.other	Forecasting	en
dc.subject.other	Hydrostatic Pressure	en
dc.subject.other	Models, Theoretical	en
dc.subject.other	Rivers	en
dc.subject.other	Water Movements	en
dc.subject.other	Water Supply	en
dc.title	Analytic element modeling of embedded multiaquifer domains	en
heal.type	journalArticle	en
heal.identifier.primary	10.1111/j.1745-6584.2005.00080.x	en
heal.publicationDate	2006	en
heal.abstract	An analytic element approach is presented for the modeling of multiaquifer domains embedded in a single-aquifer model. The inside of each domain may consist of an arbitrary number of aquifers separated by leaky layers. The analytic element solution is obtained through a combination of existing single-aquifer and multiaquifer analytic elements and allows for the analytic computation of head and leakage at any point in the aquifer. Along the boundary of an embedded multiaquifer domain, the normal flux is continuous everywhere; continuity of head across the boundary is met exactly at collocations points and approximately, but very accurately, in between. The analytic element solution compares well with an existing exact solution. A hypothetical example with a river intersecting two embedded domains illustrates the practical application of the proposed approach. Copyright © 2005 The Author(s).	en
heal.journalName	Ground Water	en
dc.identifier.issue	1	en
dc.identifier.volume	44	en
dc.identifier.doi	10.1111/j.1745-6584.2005.00080.x	en
dc.identifier.spage	81	en
dc.identifier.epage	85	en