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一种确定原状土样非饱和水力传导度的方法 被引量:4

A METHOD FOR DETERMINING UNSATURATED HYDRAULIC CONDUCTIVITY OF UNDISTURBED SOIL SAMPLE
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摘要 提出了一种新的求参方法──“同定参数法”,按该方法求原状土样参数的原理设计制作了求参装置,在求参过程中,通过迭代法修正水分特征曲线,求得原状土样非饱和水力传导度。 A new experiment method for determining parameters of soil water movement is put forward, which is that two parameters are determined in the same one experiment According to the principle of determining undisturbed soil sample parameters, a new device is designed and introduced. Through successive correction of the assumed soil water characteristic curve by iteration method, unsaturated hydraulic conductivity of the undisturbed soil sample is obtained. At the same time, the soil water characteristic of curve of the soil sample is also obtained.
出处 《土壤学报》 CAS CSCD 北大核心 2000年第3期419-423,共5页 Acta Pedologica Sinica
基金 国家自然科学基金!"八五"重大项目(49391604)
关键词 原状土样 水分特征曲线 非饱和水力传导度 Undisturbed soil sample, Soil water characteristic curve, Unsaturated conductivity
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二级参考文献2

  • 1沈荣开,D·B·Jaynes.间歇入渗情况下土壤水运动滞后作用的影响[J]水利学报,1988(10).
  • 2沈荣开.土壤水运动滞后机理的试验研究[J]水利学报,1987(04).

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