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首页> 外文期刊>Journal of plant nutrition and soil science >A relatively simple scaling method for describing the unsaturated hydraulic functions of stony soils
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A relatively simple scaling method for describing the unsaturated hydraulic functions of stony soils

机译:描述石质土壤非饱和水力功能的一种相对简单的缩放方法

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摘要

Few if any methods exist to estimate the effects of stone content (stoniness) on the unsaturated soil hydraulic properties. A relatively simple scaling method is presented to estimate the hydraulic conductivity of unsaturated stony soils having different stone contents. A key assumption of the method is that van Genuchten's water retention parameters α and n of the fine soil fraction are the same as those of the stony soil. The method further assumes a linearly decreasing relationship between the saturated hydraulic conductivity and the stone content, based on previous numerical simulations. Using the proposed method, it is possible to calculate the hydraulic conductivity of unsaturated stony soils, knowing the saturated hydraulic conductivity of the fine soil fraction, the retention curve of the fine soil fraction, and the particular stoniness of the soil.
机译:几乎没有任何方法可以估算出石材含量(石质)对非饱和土壤水硬性的影响。提出了一种相对简单的缩放方法来估算具有不同石材含量的非饱和石质土壤的水力传导率。该方法的关键假设是细土部分的van Genuchten保水参数α和n与石质土壤的保水参数相同。基于先前的数值模拟,该方法还假设饱和导水率与石材含量之间呈线性递减关系。使用所提出的方法,可以知道不饱和石质土的水力传导率,而要知道细土级分的饱和水力传导率,细土级分的保持曲线以及土壤的特殊石质性。

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