An Analysis of the Spatial Distribution of Soil Erosion in Shitai County

Xianfu Cheng, Feng Yu, L. Deng
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Abstract

Spatial distribution of soil erosion is studied in Shitai County, based on the universal soil loss equation and the GIS spatial analysis, the relationships between soil erosion, terrain, soil types, and land uses have been investigated in this paper. The results show that the total amount of soil erosion is 2850069.39 t/a in 2007. Moderate erosion area is predominant, occupying 34.16% of the region. Spatial distribution pattern of soil erosion is an obvious block distribution characteristic. Soil erosion is the strongest from 200m to 500m in different elevation zones in the study area. Soil erosion at a 15° to 30° incline is the strongest and the weakest is over 35°. Soil erosion in the northeast is the strongest, but soil erosion in the southeast is intermediate. The strongest erosion is in forestland soil of different land use types, and the second strongest is in grassland soil. Red soil and limestone soil have the most prominent erosion, while erosion in stony soil is the weakest.
石台县水土流失空间分布分析
以石台县为研究对象,基于通用水土流失方程和GIS空间分析,探讨了土壤侵蚀与地形、土壤类型和土地利用之间的关系。结果表明:2007年土壤侵蚀总量为2850069.39 t/a;以中度侵蚀区为主,占区域面积的34.16%。土壤侵蚀的空间分布格局具有明显的块状分布特征。研究区不同高程带200m ~ 500m土壤侵蚀最强。坡度为15°~ 30°时土壤侵蚀最强,坡度大于35°时土壤侵蚀最弱。东北地区水土流失最严重,东南地区水土流失居中。不同土地利用类型的林地土壤侵蚀强度最大,草地土壤次之。红壤和石灰岩土的侵蚀最突出,石质土的侵蚀最弱。
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