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Estimating soil water characteristic curve based on soil-particle-size distribution curve and local void ratio

机译:基于土壤粒径分布曲线和局部孔隙率的土壤水分特征曲线估算

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Soil water characteristic (SWC) curve is a fundamental soil property. However, its measurement is expensive and time-consuming. Therefore, many physical and mathematical methods were derived for its estimation instead of its measurement. One of these methods is Arya et al. (1999) model which estimates SWC curve from soil particle-size data assuming a constant void ratio. In this paper, SWC curves of thirty Iranian soils were estimated by using the model of Arya et al. (1999) based on local void ratio, and then the proposed model was validated for eighteen different soils by using a new derived equation for considering local void ratio. The results indicated that the local void ratio approach improved the estimation of SWC curve.
机译:土壤水分特征(SWC)曲线是土壤的基本特性。然而,其测量昂贵且费时。因此,推导了许多物理和数学方法来进行估计而不是进行测量。这些方法之一是Arya等。 (1999年)的模型假设土壤孔隙率恒定,可从土壤粒径数据估算SWC曲线。本文利用Arya等人的模型估算了30种伊朗土壤的SWC曲线。 (1999年)基于局部孔隙率,然后通过使用一个新的考虑局部孔隙率的推导方程对18种不同土壤进行了验证。结果表明,局部空隙率法改善了SWC曲线的估计。

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