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Analysis of spatial and temporal changes of soil erosion in Anning river basin

机译:安宁流域水土流失时空变化分析。

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Anning River basin as an important soil erosion monitoring and reserve in Sichuan Province. It is of great significance to grasp the temporal and spatial changes of soil erosion in this area in time to realize the comprehensive treatment of regional soil erosion. Based on the revision of the general soil erosion equation (RUSLE), the present situation of soil erosion erosion in 1995-2015 years in this area was monitored, and the classification was completed according to the national grading criteria, and the following results were mainly achieved:(1) Soil erosion in Anning river basin as a whole presents a low gradient change in the eastern High West.(2) The proportion of raster in soil erosion area of each grade also showed different structural differences, which showed that the degree of micro > Mild > Moderate > Strong > Extremely > severe, and the proportion of raster in mild and below intensity erosion area reached more than 80%, and the whole basin was at mildly below erosion level.(3) One-dimensional linear regression analysis shows, within 20 years, about 90% of the raster cell slope in this area is negative, the overall change trend of soil erosion in this area shows a significant improvement
机译:安宁河流域是四川省重要的水土流失监测与保护区。及时掌握该地区水土流失的时空变化对实现区域水土流失的综合治理具有重要意义。在修订一般土壤侵蚀方程(RUSLE)的基础上,对该地区1995-2015年的土壤侵蚀侵蚀现状进行了监测,并按照国家分级标准完成了分类,主要结果如下:实现了:(1)东部高西部地区整体水土流失呈现较低的梯度变化;(2)各等级水土流失面积的栅格比例也表现出不同的结构差异,表明程度微观>轻度>中度>强>极度>重度,中度及以下强度侵蚀区的栅格比例达到80%以上,整个盆地处于侵蚀度以下(3)一维线性回归分析表明,在20年内,该地区约90%的栅格单元坡度为负,该地区水土流失的总体变化趋势显示出显着改善

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