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Regional soil erosion risk mapping using RUSLE, GIS,and remote sensing: a case study in Miyun Watershed,North China

机译:基于RUSLE,GIS和遥感的区域土壤侵蚀风险图谱研究-以华北密云流域为例

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This paper applied the Revised Universal Soil Loss Equation (RUSLE), remote-sensing technique, and geographic information system (GIS) to map the soil erosion risk in Miyun Watershed, North China. The soil erosion parameters were evaluated in different ways: the R factor map was developed from the rainfall data, the K factor map was obtained from the soil map, the C factor map was generated based on a back propagation (BP) neural network method of Landsat ETM+ data with a correlation coefficient (r) of 0.929 to the field collected data, and a digital elevation model (DEM) with a spatial resolution of 30 m was derived from topographical map at the scale of 1:50,000 to develop the LS factor map. P factor map was assumed as 1 for the watershed because only a very small area has conservation practices. By integrating the six factor maps in GIS through pixel-based computing, the spatial distribution of soil loss in the upper watershed of Miyun reservoir was obtained by the RUSLE model. The results showed that the annual average soil loss for the upper watershed of Miyun reservoir was 9.86 t ha(-1) ya~(-1) in 2005, and the area of 47.5 km~2 (0.3%) experiences extremely severe erosion risk, which needs suitable conservation measures to be adopted on a priority basis. The spatial distribution of erosion risk classes was 66.88% very low, 21.90% low, 6.19% moderate, 2.90% severe, and 1.84% very severe. Among all counties and cities in the study area, Huairou County is in the extremely severe level of soil erosion risk, about 39.6% of land suffer from soil erosion, while Guyuan County in the very low level of soil erosion risk suffered from 17.79% of soil erosion in 2005. Therefore, the areas which are in the extremely severe level of soil erosion risk need immediate attention from soil conservation point of view.
机译:本文应用修订后的通用土壤流失方程(RUSLE),遥感技术和地理信息系统(GIS)绘制了华北密云流域的土壤侵蚀风险图。以不同的方式评估土壤侵蚀参数:从降雨数据中绘制R因子图,从土壤图获得K因子图,并根据土壤的反向传播(BP)神经网络方法生成C因子图。与野外采集的数据的相关系数(r)为0.929的Landsat ETM +数据,并从地形图以1:50,000的比例尺导出空间分辨率为30 m的数字高程模型(DEM),以开发LS因子地图。 P因子图被假定为该流域的1,因为只有很小的区域具有保护措施。通过基于像素的计算将六因子图谱整合到GIS中,利用RUSLE模型获得了密云水库上游流域土壤流失的空间分布。结果表明,2005年密云水库上游流域的年平均土壤流失量为9.86 t ha(-1)ya〜(-1),面积为47.5 km〜2(0.3%)的水土流失极度严重。 ,需要优先采取适当的保护措施。侵蚀风险类别的空间分布为:极低66.88%,极低21.90%,中度6.19%,重度2.90%和极度1.84%。在研究区所有县市中,怀柔县水土流失风险处于极其严重的水平,约有39.6%的土地遭受水土流失,而固原县水土流失风险处于极低水平,则占17.79%。 2005年的水土流失。因此,从水土保持的角度来看,处于水土流失风险极度严重的地区需要立即引起注意。

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