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Volume 21 Issue 6
Dec 2010
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Article Contents
Li Hui, Chen Xiaoling, Kyoung Jae Lim, Cai Xiaobin, Myung Sagong. Assessment of Soil Erosion and Sediment Yield in Liao Watershed, Jiangxi Province, China, Using USLE, GIS, and RS. Journal of Earth Science, 2010, 21(6): 941-953. doi: 10.1007/s12583-010-0147-4
Citation: Li Hui, Chen Xiaoling, Kyoung Jae Lim, Cai Xiaobin, Myung Sagong. Assessment of Soil Erosion and Sediment Yield in Liao Watershed, Jiangxi Province, China, Using USLE, GIS, and RS. Journal of Earth Science, 2010, 21(6): 941-953. doi: 10.1007/s12583-010-0147-4

Assessment of Soil Erosion and Sediment Yield in Liao Watershed, Jiangxi Province, China, Using USLE, GIS, and RS

doi: 10.1007/s12583-010-0147-4
Funds:  This study was supported by China Technological Supporting Program (No. 2007BAC23B05), the Special Research Fund for Prevention of Geological Disasters in Three Gorges Reservoir Area (No. SXKY3-6-1), the Natural Science Foundation of Hubei Province (No. 2009CDB104), and the Opening Foundation of State Key Laboratory for Information Engineering in Surveying, Mapping, and Remote Sensing, Wuhan University (No. (09)Key 01)
More Information
  • Corresponding author: Li Hui, leelmars@gmail.com
  • Received Date: 13 Jul 2010
  • Accepted Date: 10 Sep 2010
  • Publish Date: 01 Dec 2010
  • Soil erosion by water is a serious problem all over the world. In China, about 1 790 000 km2 of land suffers from water erosion, which accounts for 18.3% of China's total area. This study was conducted in the Liao (潦) watershed in Jiangxi (江西) Province to assess annual soil erosion and sediment yield using the Universal Soil Loss Equation (USLE). A geographic information system (GIS) was used to generate maps of the USLE factors, which include rainfall erosivity (R), soil erodibility (K), slope length and steepness (LS), cover (C), and conservation practice (P) factors. By integrating these factors in a GIS, a spatial distribution of soil erosion over the Liao watershed was obtained. The soil erosion was found to vary from nil for flat and well-covered areas to more than 500 t/ha/a in mountainous places with sparse vegetation. The average soil erosion is 18.2 t/ha/a with a standard deviation of 109.3 t/ha/a. The spatial distribution of erosion classes was estimated. About 39.5% of the watershed is under the tolerant erosion rate, and 60.5% of the study area experienced erosion to different extents. A spatially distributed sediment delivery ratio (SDR) module was developed to account for soil erosion and deposition. It was found that the SDR value at the outlet of the Liao watershed was 0.206, and the sediment yield was 1.32 million t/a, which was 20% higher than the measured sediment. The results can be used to identify the soil erosion hot spots and develop the best soil erosion management practices and help estimate the quantity of soil that was transported into the downstream Poyang (鄱阳) Lake.

     

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