Abstract
The physically-based distributed modeling approach to linking on-site rates of soil erosion in a basin to sediment yield at the basin outlet is examined. Processes considered are: hillslope erosion by raindrop impact, overland flow, gullying and mass movement; overland flow sediment routing; channel erosion, bed sediment infiltration and storage; and channel sediment routing. The sophistication of model numerical solution techniques is not matched by that of available data provision methodologies or the current understanding of the relevant processes.
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Bathurst, J.C., Wicks, J.M. (1991). Framework for Erosion and Sediment Yield Modeling. In: Bowles, D.S., O’Connell, P.E. (eds) Recent Advances in the Modeling of Hydrologic Systems. NATO ASI Series, vol 345. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-3480-4_13
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