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Simulation of Soil and Water Loss in the Upper Huaihe River Basin using the Xinanjiang Model

机译:新江模型上淮河流域土壤和水分损失模拟

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The Xinanjiang model is coupled with the Modified Universal Soil Loss Equation to simulate the soil and water loss in the upper Huaihe River. The outputs show that xinanjiang model can simulate runoff and sediment well, and the total runoff was generally less than 10% for both model calibration and validation with the Nash-Sutcliffe efficiency larger than 0.78 respectively. The computed sediment graphs were in good agreement with the observed ones, i.e. the relative errors of the computed total sediment yield was generally less than 20% for both model calibration and validation with the Nash-Sutcliffe efficiency larger than 0.62 respectively.
机译:新南江模型与改进的通用土壤损失方程联合,以模拟上淮河上部土壤和水分损失。该输出显示,新南江模型可以模拟径流和沉积物,并且对于模型校准和验证分别大于0.78的零售效率,总径流通常小于10%。计算的沉积物图与观察到的沉积物相一致,即计算的总沉积物产量的相对误差通常小于20%,对于模型校准和验证分别大于0.62的纳什·索菲利效率。

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