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dc.contributor.authorChang, Ching-Minen_US
dc.contributor.authorYeh, Hund-Deren_US
dc.date.accessioned2014-12-08T15:38:16Z-
dc.date.available2014-12-08T15:38:16Z-
dc.date.issued2010-12-15en_US
dc.identifier.issn0022-1694en_US
dc.identifier.urihttp://dx.doi.org/10.1016/j.jhydrol.2010.10.016en_US
dc.identifier.urihttp://hdl.handle.net/11536/26222-
dc.description.abstractThe problem of two-dimensional groundwater flow in a heterogeneous unconfined aquifer under periodic random forcing in time is analyzed from a stochastic point of view It is assumed that the periodic random forcing namely random recharge can be represented by a sinusoidal function in time Analytical solutions are developed through the nonstationary spectral approach in conjunction with the principle of superposition The results namely the variances of hydraulic head and specific discharge are expressed in terms of statistical properties of hydraulic parameters and recharge field It can be concluded from the analytical results that the mean recharge rate and integral scale of spatially random recharge fluctuations play essential roles in enhancing the variability of hydraulic head and specific discharges (c) 2010 Elsevier B V All rights reserveden_US
dc.language.isoen_USen_US
dc.subjectStochastic analysisen_US
dc.subjectNonstationary spectral approachen_US
dc.subjectHeterogeneous unconfined aquifersen_US
dc.subjectPeriodic random rechargeen_US
dc.titleNonstationary stochastic analysis of flow in a heterogeneous unconfined aquifer subject to spatially-random periodic rechargeen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.jhydrol.2010.10.016en_US
dc.identifier.journalJOURNAL OF HYDROLOGYen_US
dc.citation.volume395en_US
dc.citation.issue3-4en_US
dc.citation.spage163en_US
dc.citation.epage168en_US
dc.contributor.department環境工程研究所zh_TW
dc.contributor.departmentInstitute of Environmental Engineeringen_US
dc.identifier.wosnumberWOS:000285856500003-
dc.citation.woscount3-
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