Soil Erosion Dynamics in Maotiao River Watershed of Guizhou Province
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GUO Xiao-jun1,2,CUI Peng1,ZHU Xin-hua1,2(1.Key Laboratory of Mountain Hazards and Surface Process,Chinese Academy of Sciences,Chengdu Institute of Mountain Hazards and Environment,CAS,Chengdu,Sichuan 610041,China,2.Graduate University of the Chinese Academy of Sciences,Beijing 100049,China)

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S157.4

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    Abstract:

    Taken Maotiao River watershed of Guizhou Province as a case study,this paper simulated the spatial distribution of soil erosion in 1973,1990 and 2007,respectively,using GIS and the RUSLE model.Current status of soil erosion and its dynamic change were characterized.The results could provide scientific guidance for soil erosion control in the study area.The results show that serious soil erosion occurred mainly in the lower and western upper reaches of Maotiao River watershed.The major sediment sources included the areas classified as strong,extremely strong and severe erosion zones.In terms of land use,dry farmland and grassland were the dominant land use types resulting in serious soil erosion.The total area of minimal and weak soil erosion zones reduced during the period of 1973-1990,while highly eroded areas increased significantly.During the period of 1990-2007,the total area of strong,extremely strong and severe erosion zones decreased significantly,with an increase of the total area of minimal soil erosion.Soil erosion occurred mainly on lands with a slope grade of 6°~25°,where more attention should be paid to and some practical measures should be taken to reduce soil loss.

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许月卿,冯艳,周东,郭飞阁.贵州省猫跳河流域土壤侵蚀动态变化分析[J].水土保持通报英文版,2011,(1):186-190

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History
  • Received:April 01,2010
  • Revised:November 11,2010
  • Adopted:
  • Online: October 25,2012
  • Published: