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长江上游紫色土丘陵区小流域地面侵蚀量的确定 被引量:14

Determination of Surface Erosion of the Small Watersheeds in the Hilly Area of Purple Soils in the Upper Reaches of the Yangtze River
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摘要 紫色土丘陵区小流域地面侵蚀类型主要有面蚀、沟蚀和母质侵蚀三种,本文采用铯-137同位素示踪法测算了小流域坡面土壤侵蚀模数的多年平均值;用小区法、径流场法和侵蚀针测法分别测定了相同降雨条件下小流域内面蚀、沟蚀和母质侵蚀的侵蚀模数,进而换算出紫色土丘陵区单元小流域地面侵蚀的多年平均侵蚀模数。所得结果为求取小流域泥沙输移比及预报地面侵蚀量建立了基础。 There are three types of the surface erosion in the small watersheds in the hilly area of purple soils. In this paper , using Cs-137 as a tracer,the long term average modulus of erosion of slopeland of small watershed is determined,while annual soil loss of slope land,.gully and parent materialsare determined by experimental plots, runoff experimental field and erosion pin respectvely under the same rainfall condition. Thus their relative ratio is obtained. Then the long-term average modulus ofsurface erosion of the elemental small watershed is calculated. The results made it possible to calculatesediment delivery ratio and to predict surface erosion of the small watershed.
出处 《长江科学院院报》 CSCD 北大核心 1995年第1期51-56,共6页 Journal of Changjiang River Scientific Research Institute
基金 长江水土保持局资助
关键词 紫色土 地面 侵蚀 长江上游 单元小流域 surface erosion Cs-137 tracer method purple soils elemental small watershed
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参考文献3

  • 1李青云,孙厚才,蒋顺清.Cs示踪法测算小流域土壤侵蚀量[J]科技通报,1993(06).
  • 2张信宝,李少龙,王成华,谭万沛,赵庆昌,张一云,严美琼,刘亚伦,蒋锦江.Cs法测算梁峁坡农耕地土壤侵蚀量的初探[J]水土保持通报,1988(05).
  • 3吴士佳.四川省水土流失分区和水土保持工作[J]水土保持通报,1986(03).

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