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Study on soil erosion in Hudan river basin based on TM imagery

机译:基于TM影像的互丹河流域水土流失研究。

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Huangyuan county is located in the eastern part of Qinghai province and is the transition zone of Loess Plateau and Qinghai-Tibet Plateau. While the ecological environment in Huangyuan county is fragile and is mainly characterized as serous soil erosion, frequent natural disasters. It is very important to study the soil erosion. Hudan river basin was selected to study the soil erosion in Huangyuan county. The soil erosion information was extracted from Landsat 5 TM data in 1987, 2000 and 2010. To classify and grade soil erosion was according to the classification standard, Classification Standard for Soil Erosion, issued by the Ministry of Water Resources of the People's Republic of China. The types of soil erosion in the basin were classified as water erosion, freeze-thaw erosion and engineering erosion based on TM imagery, field survey and historical data. Water erosion was the most important part and accounted for more than 90% of the whole area. Weak water erosion increased significantly during the period, mainly distributing in the north of the basin. Slight-degree water erosion increased from 1987 to 2000, while there was a steep reduce during the period from 2000 to 2010. Freeze-thaw erosion distributed mainly in northern areas with high altitude. What Engineering erosion affected were narrow valley areas suitable for human settlements and agricultural production.
机译:yuan源县位于青海省东部,是黄土高原和青藏高原的过渡带。 Huang源县的生态环境脆弱,主要表现为水土流失,自然灾害频发。研究土壤侵蚀非常重要。选择了dan丹河流域来研究Huang源县的水土流失。从1987、2000和2010年的Landsat 5 TM数据中提取土壤侵蚀信息。按照中华人民共和国水利部颁布的《土壤侵蚀分类标准》分类标准对土壤侵蚀进行分类和分级。 。根据TM影像,野外调查和历史数据,该流域的土壤侵蚀类型分为水蚀,冻融侵蚀和工程侵蚀。水蚀是最重要的部分,占整个面积的90%以上。弱水蚀在此期间显着增加,主要分布在盆地北部。 1987年至2000年,轻微水蚀增加,而2000年至2010年期间水蚀急剧减少。冻融侵蚀主要分布在高海拔的北部地区。受工程侵蚀影响的是适合人类住区和农业生产的狭窄山谷地区。

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