Abstract
AbstractSoil erosion is a global environmental problem. To quantify water erosion rates at the field, hillslope or catchment scale, several spatially-distributed soil erosion models have been developed. The accuracy of those models depends largely on the sediment detachment and transport functions used, many of which were developed from empirical research. In this paper, the physical basis of the available sediment detachment and transport functions is reviewed, and their application boundaries determined. Well-known and widely-used sediment detachment and transport functions are discussed on the basis of composite force predictors, i.e. shear stress, stream power, unit stream power and effective stream power, and their suitability is elucidated based on information in the literature. It was found that only a few sediment detachment functions are available, and those have been poorly tested. Most erosion models ignore direct calculation of sediment detachment, but use the sediment transport capacity defic...
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CITATION STYLE
Ali, M., & Sterk, G. (2015). Availability and performance of sediment detachment and transport functions for overland flow conditions. Hydrological Sciences Journal, 60(9), 1550–1565. https://doi.org/10.1080/02626667.2014.948443
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