荣姣凤,张海涛,毛宁.土壤风蚀量随风速的变化规律研究[J].干旱地区农业研究,2004,(2):149~153
土壤风蚀量随风速的变化规律研究
Study on the changing laws of wind-blown mass affected by wind speed
  
DOI:10.7606/j.issn.1000-7601.2004.02.32
中文关键词:  风洞试验  农田土壤  沙子  生土  风蚀量
英文关键词:field wind tunnel  cultivated soil  sand  immature soil  wind-blown mass
基金项目:农业科技成果转化基金(02EFN216900734)
作者单位
荣姣凤 中国农业大学北京 100083 
张海涛 中国农业大学北京 100083 
毛宁 中国农业大学北京 100083 
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中文摘要:
      使用野外风洞作为风蚀研究的试验手段,通过农田土壤、沙及生土的风洞试验研究发现,农田土壤的风蚀量随风速呈指数函数变化,沙及生土的风蚀量随风速呈幂函数变化。试验研究还表明,农田土壤的风蚀量与表土层(3cm)的含水量呈显著负相关,沙的风蚀量与含水量的相关性不显著。风蚀导致土壤中的细颗粒成分大量损失,这是土壤颗粒粗化的原因所在。
英文摘要:
      The field experiment was conducted on the cultivated soil, sand and immature soil by using field wind tunnel. The results show: that the relationship between wind erosion quantity and wind velocity is fitled well in exponential functions for the cultivated soil, and in power functions for the sand and immature soil. There is a negative correlation between the quantity of wind erosion and the topsoil (30 cm) water content for the cultivated soil, but there is no evident dependency relation between the quantity of wind erosion and water content for sand. A large amount of fine particles in the soil is lost during the wind erosion, which is the main causation of siol particle coarsening.
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