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dc.contributor.authorParlarge, J.-Y.
dc.contributor.authorFuentes, C.
dc.contributor.authorConnell, L. D.
dc.contributor.authorHornung, U.
dc.contributor.authorHaverkamp, R.
dc.contributor.authorHogarth, William
dc.contributor.authorPeters, R.
dc.contributor.authorElrick, D. E.
dc.date.accessioned2019-05-26T23:09:26Z
dc.date.available2019-05-26T23:09:26Z
dc.date.issued1994
dc.identifier.issn00221694en_US
dc.identifier.doi10.1016/0022-1694(94)90084-1en_US
dc.identifier.urihttp://hdl.handle.net/10072/121833
dc.description.abstractThe flow of water in a finite soil layer is analyzed with gravity, extending an earlier non-gravitational theory. Analytical approximations are obtained to predict the outflow at the lower surface when the potentials at the upper and lower surfaces are fixed. The accuracy of the predictions is checked by comparison with numerical simulations. The solution should be of importance to infer soil properties from outflow measurements in laboratory experiments. The time when outflow first begins and the steady state flow rate are especially useful for that purpose.en_US
dc.description.peerreviewedYesen_US
dc.languageEnglishen_US
dc.publisherElsevier Scienceen_US
dc.publisher.placeNetherlandsen_US
dc.relation.ispartofpagefrom335en_US
dc.relation.ispartofpageto350en_US
dc.relation.ispartofissue1-4en_US
dc.relation.ispartofjournalJournal of Hydrologyen_US
dc.relation.ispartofvolume156en_US
dc.subject.fieldofresearchENGINEERINGen_US
dc.subject.fieldofresearchcode090000en_US
dc.titleWater movement in a finite layer:Influence of gravity for constant water content at the surfaceen_US
dc.typeJournal articleen_US
dc.type.descriptionC1 - Peer Reviewed (HERDC)en_US
dc.type.codeC - Journal Articlesen_US
gro.facultyGriffith Sciences, Griffith School of Environmenten_US
gro.hasfulltextNo Full Text
gro.griffith.authorHogarth, William L.


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