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dc.contributor.authorFerrante, Marco
dc.contributor.authorYeh, T.-C. Jim
dc.date.accessioned2016-06-22T18:06:22Z
dc.date.available2016-06-22T18:06:22Z
dc.date.issued1995-09-08
dc.identifier.urihttp://hdl.handle.net/10150/614164
dc.description.abstractA numerical model for the analysis of uncertainty propagation in flow through unsaturated soils is developed. This model is based on the first -order Taylor series expansion of the discretized Richards' equation, for one -dimensional flow. Soil hydrologic properties, the saturated hydraulic conductivity and the pore size distribution, are assumed to be stochastic processes in space. The surface boundary conditions are considered to be deterministic variable in time or stochastic time series. The purpose of this model is to examine the effect of uncertainty in boundary conditions and heterogeneity on the pressure head and flux variance profiles at various times.
dc.language.isoen_USen
dc.publisherDepartment of Hydrology and Water Resources, University of Arizona (Tucson, AZ)en
dc.relation.ispartofseriesTechnical Reports on Hydrology and Water Resources, No. 95-040en
dc.rightsCopyright © Arizona Board of Regentsen
dc.sourceProvided by the Department of Hydrology and Water Resources.en
dc.titleSTOCHASTIC ANALYSIS OF WATER FLOW IN HETEROGENEOUS UNSATURATED SOILS UNDER TRANSIENT CONDITIONSen_US
dc.typetexten
dc.typeTechnical Reporten
dc.contributor.departmentDepartment of Hydrology & Water Resources, The University of Arizonaen
dc.description.collectioninformationThis title from the Hydrology & Water Resources Technical Reports collection is made available by the Department of Hydrology & Atmospheric Sciences and the University Libraries, University of Arizona. If you have questions about titles in this collection, please contact repository@u.library.arizona.edu.en
refterms.dateFOA2018-06-18T03:49:06Z
html.description.abstractA numerical model for the analysis of uncertainty propagation in flow through unsaturated soils is developed. This model is based on the first -order Taylor series expansion of the discretized Richards' equation, for one -dimensional flow. Soil hydrologic properties, the saturated hydraulic conductivity and the pore size distribution, are assumed to be stochastic processes in space. The surface boundary conditions are considered to be deterministic variable in time or stochastic time series. The purpose of this model is to examine the effect of uncertainty in boundary conditions and heterogeneity on the pressure head and flux variance profiles at various times.


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