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A Case Study for Comparison of Predicted and Measured Soil Loss in Mountain Watershed using RUSLE Model

机译:利用RUSLE模型比较山区流域预测与实测土壤流失的案例研究

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摘要

The purpose of this research is to evaluate an availability of the Revised Universal Soil Loss Equation (RUSLE) for predicting soil loss values for a mountain watershed in Japan. Estimates of the erosion index (EI30) and the rainfall erosivity factor (R) of RUSLE can be obtained from daily rainfall data from 1993 to 1998. The soil credibility and topographic factors of RUSLE were evaluated using soil sampling and digital elevation data respectively. The data of soil loss at a measurement station in t he Kawamukai watershed was used for verification of this model. The average values of annual soil ioss measured and predicted for the watershed are 27.7 kg,ha,y and 28.9 kg,ha,y respectively. The difference between them is only 4 percent. Thus, it is concluded that the RUSLE model can predict reasonable soil loss in Kawamukai watershed during the study period.
机译:这项研究的目的是评估修订的通用土壤流失方程(RUSLE)的可用性,该方程可用于预测日本山区流域的土壤流失值。可以从1993年至1998年的每日降雨数据中估算RUSLE的侵蚀指数(EI30)和降雨侵蚀力因子(R)。分别使用土壤采样和数字高程数据评估RUSLE的土壤可信度和地形因子。在Kawamukai流域的一个测量站的土壤流失数据被用于验证该模型。该分水岭测得和预测的年度土壤ios平均值分别为27.7 kg,ha,y和28.9 kg,ha,y。它们之间的差异仅为4%。因此,可以得出结论:在研究期间,RUSLE模型可以预测Kawamukai流域的合理土壤流失。

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