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dc.contributor.authorHogarth, William
dc.contributor.authorRose, Calvin
dc.contributor.authorSander, Graham
dc.contributor.authorParlange, J.
dc.contributor.authorHairsine, P.
dc.contributor.authorLisle, I.
dc.date.accessioned2019-02-07T01:04:44Z
dc.date.available2019-02-07T01:04:44Z
dc.date.issued1999
dc.identifier.issn00221694
dc.identifier.doi10.1016/S0022-1694(99)00012-8
dc.identifier.urihttp://hdl.handle.net/10072/122168
dc.description.abstractA simple analytical approximation is obtained for erosion on a hillslope involving sediment transport when rainfall is the only source of water. The solution extends an earlier study requiring some numerical evaluation. Owing to its simplicity, the solution gives a clear understanding on the influence of the physical processes involved. Fundamentally, there is a very short time behavior associated with rainfall impact and a longer time behavior controlled by convection. It is this time decoupling which permits the solution to be expressed in simple terms. The short time analytical results can be used to simplify greatly numerical procedures.
dc.description.peerreviewedYes
dc.languageEnglish
dc.language.isoeng
dc.publisherElsevier Science
dc.publisher.placeNetherlands
dc.relation.ispartofpagefrom149
dc.relation.ispartofpageto156
dc.relation.ispartofissue1-2
dc.relation.ispartofjournalJournal of Hydrology
dc.relation.ispartofvolume217
dc.titleAddendum to Unsteady Soil Erosion Model
dc.typeJournal article
dc.type.descriptionC1 - Articles
dc.type.codeC - Journal Articles
gro.facultyGriffith Sciences, Griffith School of Environment
gro.hasfulltextNo Full Text
gro.griffith.authorRose, Calvin W.
gro.griffith.authorHogarth, William L.
gro.griffith.authorSander, Graham C.


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