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dc.contributor.authorRose, Calvinen_US
dc.contributor.authorYu, Bofuen_US
dc.contributor.authorHogarth, Williamen_US
dc.contributor.authorOkom, Augustineen_US
dc.contributor.authorGhadiri, Hosseinen_US
dc.date.accessioned2017-05-03T11:33:54Z
dc.date.available2017-05-03T11:33:54Z
dc.date.issued2003en_US
dc.date.modified2010-07-06T07:00:39Z
dc.identifier.issn00221694en_US
dc.identifier.doi10.1016/S0022-1694(03)00184-7en_AU
dc.identifier.urihttp://hdl.handle.net/10072/6051
dc.description.abstractThe spatial and size distribution of sediment deposited from short periods of overland flow due to the effect of a simulated grass buffer strip was measured for low slopes of 1.6, 3.4 and 5.1%. These data were analysed so as to critically evaluate two alternative models of the process of re-entrainment of recently deposited sediment. A model of re-entrainment, previously thought to be appropriate only for a steady-state or equilibrium situation, was found to give better agreement with experiments than did a model previously used in the literature on this subject.en_US
dc.description.peerreviewedYesen_US
dc.description.publicationstatusYesen_AU
dc.languageEnglishen_US
dc.language.isoen_AU
dc.publisherElsevier Science B.V.en_US
dc.publisher.placeNetherlandsen_US
dc.publisher.urihttp://www.elsevier.com/locate/jhydrolen_AU
dc.relation.ispartofpagefrom33en_US
dc.relation.ispartofpageto51en_US
dc.relation.ispartofjournalJournal of Hydrologyen_US
dc.relation.ispartofvolume280en_US
dc.subject.fieldofresearchHISTORY AND ARCHAEOLOGYen_US
dc.subject.fieldofresearchcode210000en_US
dc.titleSediment deposition from flow at low gradients into a buffer strip - a critical test of re-entrainment theoryen_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.date.issued2003
gro.hasfulltextNo Full Text


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