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dc.contributor.authorLisle, I.
dc.contributor.authorRose, Calvin
dc.contributor.authorHogarth, William
dc.contributor.authorHairsine, P.
dc.contributor.authorSander, Graham
dc.contributor.authorParlange, J.
dc.date.accessioned2019-02-07T04:54:24Z
dc.date.available2019-02-07T04:54:24Z
dc.date.issued1998
dc.identifier.issn00221694en_US
dc.identifier.doi10.1016/S0022-1694(97)00123-6en_US
dc.identifier.urihttp://hdl.handle.net/10072/122225
dc.description.abstractA stochastic model governing the downslope transport of a sediment particle during an erosion event is described. Particles alternate between resting on the soil bed and being transported by the overland flow. Probability densities and moments are constructed for the distribution of a particle's position at a given time, and also for time of passage to a given location. We show that a suitable averaging of the stochastic particle motions in our model gives rise to the deterministic erosion differential of Hairsine and Rose (Hairsine, P., Rose, C., 1991. Soil Sci. Soc. Am. J. 55 (2), 320–324). The model generalized H. Einstein's stochastic model (Der Geschiebebetrieb als Wahrscheinlichkeitsproblem, Verlag Rascher, Zurich, 1937) for bedload transport in streams.en_US
dc.description.peerreviewedYesen_US
dc.languageEnglishen_US
dc.publisherElsevier Scienceen_US
dc.publisher.placeNetherlandsen_US
dc.relation.ispartofpagefrom217en_US
dc.relation.ispartofpageto230en_US
dc.relation.ispartofissue1-4en_US
dc.relation.ispartofjournalJournal of Hydrologyen_US
dc.relation.ispartofvolume204en_US
dc.titleStochastic Sediment Transport in Soil Erosionen_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


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