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Assessment of soil erosion at large watershed scale using RUSLE and GIS: A case study in the Loess Plateau of China

机译:基于RUSLE和GIS的大流域土壤侵蚀评价-以中国黄土高原为例。

摘要

Soil erosion is a serious problem in the Loess Plateau of China, and assessment of soil erosion at large watershed scale is urgently need. This study used RUSLE and GIS to assess soil loss in the Yanhe watershed. All factors used in the RUSLE were calculated for the watershed using local data. RUSLE-factor maps were made. The mean values of the R-factor, K-factor, LS-factor, C-factor and P-factor were 970 209 MJ km(-2) h(-1) a(-1), 0.0195 Mg h MJ(-1) mm(-1), 10.27, 0.33359 and 0.2135 respectively. The mean value of the annual average soil loss was found to be 14 458 Mg km(-2) per year, and the soil loss rate in most areas was between 5000 and 20 000 Mg km(-2) per year. There is more erosion in the centre and southeast than in the northwest of Yanhe watershed. Because of the limitations of the RUSLE and spatial heterogeneity, more work should be done on the RUSLE-factor accuracy, scale effects, etc. Furthermore, it is necessary to apply some physical models in the future, to identify the transport and deposition processes of sediment at a large scale. Copyright (c) 2005 John Wiley S Sons, Ltd.
机译:黄土高原地区水土流失是一个严重的问题,迫切需要对大流域的水土流失进行评估。这项研究使用RUSLE和GIS评估了延河流域的土壤流失。使用本地数据计算了RUSLE中使用的所有因子。绘制了RUSLE因子图。 R因子,K因子,LS因子,C因子和P因子的平均值分别为970209 MJ km(-2)h(-1)a(-1),0.0195 Mg h MJ(- 1)mm(-1),10.27、0.33359和0.2135。发现年平均水土流失的平均值为每年14 458 Mg km(-2),并且大多数地区的水土流失率在每年5000至20000 Mg km(-2)之间。延河流域的中部和东南部比西北部的侵蚀要多。由于RUSLE和空间异质性的局限性,应在RUSLE因子的准确性,尺度效应等方面做更多的工作。此外,将来有必要应用一些物理模型来确定铁矿的输运和沉积过程。大规模沉积。版权所有(c)2005 John Wiley S Sons,Ltd.

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