完整后设资料纪录
DC 栏位语言
dc.contributor.authorChang, Ching-Minen_US
dc.contributor.authorYeh, Hund-Deren_US
dc.date.accessioned2014-12-08T15:36:41Z-
dc.date.available2014-12-08T15:36:41Z-
dc.date.issued2014-09-01en_US
dc.identifier.issn0169-3913en_US
dc.identifier.urihttp://dx.doi.org/10.1007/s11242-014-0334-3en_US
dc.identifier.urihttp://hdl.handle.net/11536/25045-
dc.description.abstractIn this article, we attempt to quantify the variability of water pressure head in response to temporally correlated fluctuations in infiltration rate in partially saturated heterogeneous formations. This study concentrates on the unsaturated case of predominantly vertical movement of moisture. A closed-form solution is developed to analyze the impacts of the temporal correlation scale of infiltration fluctuations and the spatial correlation scale of log-saturated hydraulic conductivity () field on the variability in water pressure head. Our result indicates that the temporal correlation scale of infiltration process or the spatial correlation scale of field takes a role in increasing the variability in the pressure head.en_US
dc.language.isoen_USen_US
dc.subjectStochastic analysisen_US
dc.subjectUnsaturated flowen_US
dc.subjectWater pressure head varianceen_US
dc.titleStochastic Analysis of Unsaturated Flow Subject to Temporally Correlated Infiltrationen_US
dc.typeArticleen_US
dc.identifier.doi10.1007/s11242-014-0334-3en_US
dc.identifier.journalTRANSPORT IN POROUS MEDIAen_US
dc.citation.volume104en_US
dc.citation.issue2en_US
dc.citation.spage289en_US
dc.citation.epage298en_US
dc.contributor.department环境工程研究所zh_TW
dc.contributor.departmentInstitute of Environmental Engineeringen_US
dc.identifier.wosnumberWOS:000340599300003-
dc.citation.woscount0-
显示于类别:Articles


文件中的档案:

  1. 000340599300003.pdf

If it is a zip file, please download the file and unzip it, then open index.html in a browser to view the full text content.