可冲蚀土壤部分经常从凸出物剥蚀并降落于洼地。

Erodible soil fractions are usually dislodged from projections and trapped in depression.

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试验结果表明，土壤剥蚀率随着水流剪切力的增加其对数呈线性关系。

The results showed that soil detachment rate increased with the increase of flow shear stress, their logarithm was linear.

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坡度和流量与土壤剥蚀率之间呈显著相关关系，流量对土壤剥蚀率的影响明显大于坡度；

There is a remarkable correlativity among soil detachment rate, discharge and slope, the impact of discharge on soil detachment rate is bigger than that of slope gradient.

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