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中国沙漠 ›› 1999, Vol. 19 ›› Issue (3): 293-295.

• 论文 • 上一篇    下一篇

柴达木盆地东南部土壤风蚀研究

张胜邦1, 董旭1, 刘玉璋2, 张更权1, 刘建军1   

  1. 1. 青海省林业勘察设计院, 青海西宁 810007;
    2. 中国科学院兰州沙漠研究所, 甘肃兰州 730000
  • 收稿日期:1998-06-08 修回日期:1999-02-20 出版日期:1999-06-20 发布日期:1999-06-20
  • 作者简介:张胜邦(1962-),男(汉族),青海西宁人,工程师,从事沙漠治理及林业规划设计研究。

Soil Erosion Modelling Study in Southeastern Qaidam Basin

ZHANG Sheng bang1, DONG Xu1, LIU Yu zhang2, ZHANG Geng quan1, LIU Jian jun1   

  1. 1. Qinhai Academy of Forestry Survey and Design, Xining 810007, China;
    2. Institute of Desert Research, Chinese Academy Sciences, Lanzhou 730000, China
  • Received:1998-06-08 Revised:1999-02-20 Online:1999-06-20 Published:1999-06-20

摘要: 柴达木盆地东南部土壤风蚀风洞模拟实验结果表明,土壤风蚀强度随风力作用和下垫面因子不同而不同。净风对土壤风蚀作用较小,但在挟沙风作用下,风蚀强烈。地表类型不同风蚀强度变化很大,流动沙地是耕地(小麦留茬)的数百倍。土壤质地不同起沙风速不同,细沙和极细沙比例越高风蚀量越大。翻耕地与未翻耕地风蚀变化悬殊,翻耕地风蚀量是未翻耕地的10倍以上。自然植被和人为留茬均有抑制风蚀的作用。

关键词: 柴达木盆地, 风沙环境, 风蚀, 模拟实验

Abstract: Soil erosion on different soil types in southeastern Qaidam Basin was modelled in wind tunnel. It was concluded that the degree of soil erosion was changing with wind forces and underlying surfaces. Soil erosion was less when wind only, but more when sand carring wind. The degree of soil erosion changed obviously with the underlying surfaces: more fine and superfine sands in soil, and more soil erosion; several hunderd times of eroded soil amounts on sand shifting land than on farmland (with wheat stubbles); ten times more of eroded soil amounts on ploughed farmlands than on unploughed ones. Natural vegetation and stubbles all have the function of preventing soil erosion.

Key words: Qaidam Basin, wind sand environment, erosion, modelling experiment

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