4.7 Article

Sediment transport capacity equation for soils from the Loess Plateau and northeast China

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Summary: The study found that in the Loess Plateau, the interrill erosion mechanism of Shenmu soil can be classified into two types: detachment-limited erosion in the initial rainfall phase and transport-limited erosion in the subsequent rainfall, or transport-limited erosion throughout the entire rainfall. Among various flow intensity parameters, stream power was found to be the most reliable for predicting interrill erosion rate, with a satisfactory coefficient of determination (R-2). However, the erosion rate model based on stream power showed low prediction accuracy for the two types of soil. Additionally, a general flow intensity parameter was derived to predict interrill erosion rate, with a high model efficiency of 0.94.

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