Modelling upland and instream erosion, sediment and phosphorus transport in a large catchment
1999; Wiley; Volume: 13; Issue: 5 Linguagem: Inglês
10.1002/(sici)1099-1085(19990415)13
ISSN1099-1085
AutoresAnthony J. Jakeman, Timothy R. Green, Sara Beavis, Lu Zhang, C. R. Dietrich, P.F. Crapper,
Tópico(s)Soil and Water Nutrient Dynamics
ResumoHydrological ProcessesVolume 13, Issue 5 p. 745-752 Research Article Modelling upland and instream erosion, sediment and phosphorus transport in a large catchment Anthony J. Jakeman, Corresponding Author Anthony J. Jakeman Centre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, AustraliaCentre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, Australia.===Search for more papers by this authorTimothy R. Green, Timothy R. Green USDA—Agricultural Research Service, Great Plains Systems Research Unit, PO Box E, 301 South Howes Street, Fort Collins, CO 80522, USASearch for more papers by this authorSara G. Beavis, Sara G. Beavis Centre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, AustraliaSearch for more papers by this authorLi Zhang, Li Zhang Centre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, AustraliaSearch for more papers by this authorClaude R. Dietrich, Claude R. Dietrich Centre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, AustraliaSearch for more papers by this authorPeter F. Crapper, Peter F. Crapper CSIRO Land and Water, Canberra, ACT 2000, AustraliaSearch for more papers by this author Anthony J. Jakeman, Corresponding Author Anthony J. Jakeman Centre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, AustraliaCentre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, Australia.===Search for more papers by this authorTimothy R. Green, Timothy R. Green USDA—Agricultural Research Service, Great Plains Systems Research Unit, PO Box E, 301 South Howes Street, Fort Collins, CO 80522, USASearch for more papers by this authorSara G. Beavis, Sara G. Beavis Centre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, AustraliaSearch for more papers by this authorLi Zhang, Li Zhang Centre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, AustraliaSearch for more papers by this authorClaude R. Dietrich, Claude R. Dietrich Centre for Resource and Environmental Studies, The Australian National University, Canberra, ACT 0200, AustraliaSearch for more papers by this authorPeter F. Crapper, Peter F. Crapper CSIRO Land and Water, Canberra, ACT 2000, AustraliaSearch for more papers by this author First published: 29 April 1999 https://doi.org/10.1002/(SICI)1099-1085(19990415)13:5 3.0.CO;2-ECitations: 38AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onEmailFacebookTwitterLinkedInRedditWechat Abstract This overview presents background information to place the subsequent papers by Beavis et al., Dietrich et al. and Green et al. in the context of a unified approach. The modelling framework described here consists of two major components: an upland catchment model and an instream sediment transport model. The upland model simulates stream flow (Q), suspended sediment (SS) and associated phosphorus (P) using rainfall data, and is calibrated to daily stream flow time-series under historical conditions. The instream model routes SS and attached P from the outlet of upland catchments to gauging points downstream. The instream transport model can infer sources (resuspension and bank erosion) and sinks (deposition) within a reach. Aerial photographs are used to assess the on-site effects of climate and land cover/use on erosion and the drainage network. Changes in land cover/use and the effects on the drainage network are related to the parameters in the rainfall–runoff model so that associated effects on Q (and hence SS and P) can be assessed. 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