首页> 中文期刊>中国高等学校学术文摘·林学 >Effects of changes in land use and land cover on sediment discharge of runoff in a typical watershed in the hill and gully loess region of northwest China

Effects of changes in land use and land cover on sediment discharge of runoff in a typical watershed in the hill and gully loess region of northwest China

     

摘要

Land use plays a much more important role than other factors, such as climate, soil properties, topo-graphic features, vegetation coverage, human activities and others, in affecting soil erosion and sediment discharge. In order to understand the effects of changes in land use on sediment discharge and to provide a theoretical basis for land use planning, management and ecological restoration, we used the controlled Qiaozidong watershed and the uncontrolled Qiaozixi watershed in the third sub-region of the Loess Plateau as examples and analyzed the effects of land use and land cover on the discharge of sediments. The results show that the impact of land use and land cover on the annual amount of sediment discharge is significant. Compared with the uncontrolled watershed during similar periods, the amount of sediment discharged from the con-trolled watershed was reduced by 44%, 75% and 86%, respectively, in wet, normal and dry years. In the controlled watershed, compared with the period from 1986 to 1994, the amount of sediments discharged was less during the period from 1995 to 2004. The impact of land use and land cover on sediment discharge demonstrated characteristics of seasonal fluctuation. The effects of sediment reduction in the controlled watershed were greater than those in the uncontrolled watershed in May and September. In the con-trolled watershed, the reduction effect coincided with the distribution of rainfall. The amount of discharged flood sediments is closely correlated with rainfall, rainfall intens-ity in a 60 min period and the volume of flood. The rain-storm-runoff process and the rainstorm-sediment discharge process demonstrate that land cover has a strong regulatory and control function in the flood process and sediment discharge in rainstorms. For the controlled water-shed, given the same precipitation frequency distribution, the average amount of sediment discharged during the land use period from 1995 to 2004 was less than that during the earlier land use period from 1986 to 1994 under every recurrent period.

著录项

  • 来源
    《中国高等学校学术文摘·林学》|2008年第3期|334-341|共8页
  • 作者单位

    China Institute of Water Resources and Hydropower Research,Beijing 100044,China;

    Key Laboratory of Soil & Water Conservation and Desertification Combating,Ministry of Education,Beijing Forestry University,Beijing 100083,China;

    Department of Land and Water Resources Engineering,Royal Institute of Technology,Stockholm,SE-100 44,Sweden;

    China Institute of Water Resources and Hydropower Research,Beijing 100044,China;

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  • 正文语种 chi
  • 中图分类 林业;
  • 关键词

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