吉林省西部沙地土壤风蚀机理分析
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贵州省自然科学基金项目(Z073079);国家重点基础研究发展规划项目(2006CB403206-6);教育部重点项目(2005141);贵州大学科研启动基金项目(X060056)


Mechanism of Soil Erosion by Wind on Sandy Land in West Jilin Province
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    摘要:

    风蚀危害是吉林省西部沙地的主要自然灾害之一。通过典型样地调查和室内风洞试验,分析了该区沙地土壤风蚀机理。结果表明,土壤风蚀随地表粗糙度、土壤含水量和有机质含量的增加而减小,其风蚀量与地表粗糙度、土壤含水量近似地呈负指数关系,与土壤有机质含量呈负相关。风是吉林省西部沙地产生风蚀的主要源动力,当风速超过临界起沙风速时,土壤侵蚀量与风速的3次方成正比,其风蚀性气候因子为155.2,春季最大(76.2)。在空间分布上,该区风蚀性气候因子和侵蚀性风能均自东向西递增,西北部的通榆县为最大。

    Abstract:

    Soil erosion by wind is one of the main natural disasters on the sandy land in West Jilin Province.Based on field investigation,tests,and indoor wind tunnel experiment,the mechanism of soil erosion by wind on sandy land is analyzed.Analyses indicate that soil erosion by wind constantly decreases with the increases in surface roughness,soil moisture content,and organic matter content.A negative exponential relation with surface roughness and soil moisture content and a negative relation with organic matter content are found.Wind is the main force driving soil erosion on the sandy land in the region.When wind velocity exceeds the critical velocity,soil erosion is proportional to the third power of wind velocity.Climate factor for soil erosion by wind is 155.2.Erosion in spring is the severest(76.2).Spatially, both erosive climate factor and erosive wind energy increase from west to east. Yutong County in the northwest part of the region has the greater values.

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戴全厚,喻理飞,刘明义,王艳.吉林省西部沙地土壤风蚀机理分析[J].水土保持通报,2008,(3):81-84,96

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  • 收稿日期:2007-10-17
  • 最后修改日期:2008-01-24
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  • 在线发布日期: 2014-11-26
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