6533b835fe1ef96bd129eae3

RESEARCH PRODUCT

Sediment delivery processes at basin scale

Vito FerroMario Minacapilli

subject

Hydrologygeographygeography.geographical_feature_categoryMathematical modelfungiDrainage basinSedimentStructural basinhumanitiesBack-strippingAlluvionErosionAlluviumgeographic locationsGeologyWater Science and Technology

description

Abstract Since eroded sediments are produced from different sources distributed throughout a basin, sediment delivery processes at basin scale have to be modelled by a spatially distributed approach. In this paper a new theoretically based relationship is proposed for evaluating the sediment delivery ratio, SDRi, of each morphological unit, i, into which a basin is divided. Then, using the sediment balance equation written for the basin outlet, a relationship between the basin sediment delivery ratio, SDRW and the SDRi is deduced. This relationship is shown to be independent of the soil erosion model used. Finally, a morphological criterion for estimating a coefficient, β, is proposed.

yearjournalcountryeditionlanguage
1995-12-01
http://www.scopus.com/inward/record.url?eid=2-s2.0-0029505123&partnerID=MN8TOARS