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dc.contributor.authorChang, Ching-Minen_US
dc.contributor.authorYeh, Hund-Deren_US
dc.date.accessioned2018-08-21T05:53:43Z-
dc.date.available2018-08-21T05:53:43Z-
dc.date.issued2018-05-30en_US
dc.identifier.issn0885-6087en_US
dc.identifier.urihttp://dx.doi.org/10.1002/hyp.11487en_US
dc.identifier.urihttp://hdl.handle.net/11536/145074-
dc.description.abstractThis study presents a Lagrangian description of advection dominated field-scale transport of inert solutes, namely, the statistics of advective solute travel time and trajectory, in nonstationary random groundwater flow fields. The vertical flow field is generated by the effects of changes in total stress applied in fluid-saturated heterogeneous deformable porous media. The Lagrangian statistics are developed directly from the velocity statistics based on the application of stochastic methodology such as the representation theorem and Fourier-Stieltjes integral representation. The focus of our numerical evaluation is placed on the influence of the soil compressibility on the Lagrangian statistics. The prediction on the statistics of solute travel time and trajectory may serve as the basic input to the environmental risk assessment.en_US
dc.language.isoen_USen_US
dc.subjectheterogeneous deformable porous mediaen_US
dc.subjectnonstationary groundwater flow fieldsen_US
dc.subjectsoil compressibilityen_US
dc.subjectstatistics of the solute travel timeen_US
dc.titleQuantification of Lagrangian travel time statistics under nonstationary random groundwater flow conditionsen_US
dc.typeArticleen_US
dc.identifier.doi10.1002/hyp.11487en_US
dc.identifier.journalHYDROLOGICAL PROCESSESen_US
dc.citation.volume32en_US
dc.citation.spage1561en_US
dc.citation.epage1570en_US
dc.contributor.department環境工程研究所zh_TW
dc.contributor.departmentInstitute of Environmental Engineeringen_US
dc.identifier.wosnumberWOS:000434115300004en_US
Appears in Collections:Articles