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Transient Flow into a Partially Penetrating Well during the Constant-Head Test in Unconfined Aquifers

dc.citation.epage1063en_US
dc.citation.issue9en_US
dc.citation.spage1054en_US
dc.citation.volume137en_US
dc.citation.woscount2
dc.contributor.authorChang, Ya-Chien_US
dc.contributor.authorChen, Geng-Yuanen_US
dc.contributor.authorYeh, Hund-Deren_US
dc.contributor.department環境工程研究所zh_TW
dc.contributor.departmentInstitute of Environmental Engineeringen_US
dc.date.accessioned2014-12-08T15:27:19Z
dc.date.available2014-12-08T15:27:19Z
dc.date.issued2011-09-01en_US
dc.description.abstractThis study derives a semianalytical solution for drawdown distribution during a constant-head test at a partially penetrating well in an unconfined aquifer. The constant-head condition is used to describe the boundary along the screen. In addition, a free-surface condition is used to delineate the upper boundary of the unconfined aquifer. The Laplace-domain solution is then derived using separation of variables and Laplace transform. This solution can be used to identify the aquifer parameters from the data of the constant-head test when integrated with an optimization scheme or to investigate the effects of vertical flow caused by the partially penetrating well and free-surface boundary in an unconfined aquifer. DOI: 10.1061/(ASCE)HY.1943-7900.0000392. (C) 2011 American Society of Civil Engineers.en_US
dc.identifier.doi10.1061/(ASCE)HY.1943-7900.0000392en_US
dc.identifier.issn0733-9429en_US
dc.identifier.journalJOURNAL OF HYDRAULIC ENGINEERING-ASCEen_US
dc.identifier.urihttp://dx.doi.org/10.1061/(ASCE)HY.1943-7900.0000392en_US
dc.identifier.urihttps://ir.lib.nycu.edu.tw/handle/11536/19570
dc.identifier.wosnumberWOS:000294780600017
dc.language.isoen_USen_US
dc.subjectUnconfined aquiferen_US
dc.subjectSemianalytical solutionen_US
dc.subjectPartially penetrating wellen_US
dc.subjectconstant-head testen_US
dc.titleTransient Flow into a Partially Penetrating Well during the Constant-Head Test in Unconfined Aquifersen_US
dc.typeArticleen_US

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