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Why the universal soil loss equation and the revised version of it do not predict event erosion well

机译:为什么通用土壤流失方程及其修正版本不能很好地预测事件侵蚀

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摘要

The universal soil loss equation (USLE; Wischmeier and Smith, 1978) and its revised version (RUSLE; Renard et al., 1997) were developed to predict the long-term average annual erosion A from field-sized areas from six factors: R the rainfall-runoff (erosivity) factor, K the soil (erodibility) factor, L the slope length factor, S the slope gradient factor, C the crop and management factor and P the conservation support practice factor. The USLE/RUSLE model is often represented by the equation A = RKLSCP where R is the average annual sum of the event rainfall-runoff (erosivity) factor when this factor is given by the product of the kinetic energy of the rainstorm E and the maximum 30 min rainfall intensity I_30, L = S = C = P = 1.0 when the area is bare fallow on a 9% slope that is 22.13 m long with cultivation up and down the slope, and K is the average annual soil loss per unit of R when L = S = C = P = 1.0.
机译:建立了通用土壤流失方程(USLE; Wischmeier和Smith,1978)及其修订版(RUSLE; Renard等,1997),以从六个因素预测田间规模区域的长期平均年侵蚀A:R降雨径流(侵蚀性)因子,K(土壤侵蚀性)因子,L坡长因子,S坡度因子,C作物和管理因子以及P养护实践因子。 USLE / RUSLE模型通常用公式A = RKLSCP表示,其中R是事件降雨径流(侵蚀性)因子的年平均总和,而该因子是暴雨E动能与最大值的乘积。 30分钟降雨强度I_30,当该区域是裸露的休闲地,坡度为22.13 m,坡度为上下时,在9%的坡度上为裸露休耕地时,L = S = C = P = 1.0,K为每公顷土壤年平均土壤流失当L = S = C = P = 1.0时为R。

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