Please use this identifier to cite or link to this item: https://hdl.handle.net/10593/13888
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dc.contributor.authorSzymkiewicz, Adam-
dc.contributor.authorTisler, Witold-
dc.contributor.authorBurzyński, Kazimierz-
dc.date.accessioned2015-10-08T06:36:53Z-
dc.date.available2015-10-08T06:36:53Z-
dc.date.issued2015-09-
dc.identifier.citationGeologos, 2015, 21, 3. s.161-167pl_PL
dc.identifier.isbn978-83-232187-4-6-
dc.identifier.issn1426-8981-
dc.identifier.urihttp://hdl.handle.net/10593/13888-
dc.description.abstractFlow in unsaturated porous media is commonly described by the Richards equation. This equation is strongly nonlinear due to interrelationships between water pressure head (negative in unsaturated conditions), water content and hydrau- lic conductivity. The accuracy of numerical solution of the Richards equation often depends on the method used to estimate average hydraulic conductivity between neighbouring nodes or cells of the numerical grid. The present paper discusses application of the computer simulation code VS2DI to three test problems concerning infiltration into an ini- tially dry medium, using various methods for inter-cell conductivity calculation (arithmetic mean, geometric mean and upstream weighting). It is shown that the influence of the averaging method can be very large for coarse grid, but that it diminishes as cell size decreases. Overall, the arithmetic average produced the most reliable results for coarse grids. Moreover, the difference between results obtained with various methods is a convenient indicator of the adequacy of grid refinement.pl_PL
dc.language.isoenpl_PL
dc.publisherInstytut Geologii UAMpl_PL
dc.rightsinfo:eu-repo/semantics/openAccesspl_PL
dc.subjectnumerical modellingpl_PL
dc.subjectRichards equationpl_PL
dc.subjecthydraulic conductivitypl_PL
dc.titleExamples of numerical simulations of two- dimensional unsaturated flow with VS2DI code using different interblock conductivity averaging schemespl_PL
dc.typeArtykułpl_PL
Appears in Collections:Geologos, 2015, 21, 3

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