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Estimation of the soil-water characteristic curve from the grain size distribution of coarse-grained soils

机译:粗粒土晶粒尺寸分布的土壤 - 水特征曲线估算

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摘要

Coarse-grained soil, such as aggregate and coarse sand, is commonly selected to construct a capillary barrier system (CBS). The barrier effect in the CBS is mainly dependent on the hydraulic properties of the coarse-grained soils. It is noted that direct methods (such as experimental measurement) for the determination of the hydraulic properties (including the soil-water characteristic curve (SWCC) and coefficient of permeability) of soil are time-consuming and costly. As a result, indirect methods for the determination of the SWCC and permeability function of soil are commonly adopted by researchers and engineers. In this paper, a new method is proposed for the estimation of the SWCC from the grain-size distribution (GSD) of coarse-grained soils. The proposed method is based on the assumptions that the soil does not experience any volume change and the hysteresis of the SWCC is ignored. A contact angle larger than zero is adopted in this study. The results computed from the proposed model agree well with the experimental data from published studies.
机译:通常选择粗粒土壤,例如骨料和粗砂,以构建毛细管屏障系统(CBS)。 CBS中的阻挡效应主要取决于粗粒土壤的液压性能。应注意,用于测定土壤的液压性能(包括土壤 - 水特征曲线(SWCC)和渗透系数)的直接方法(包括土壤 - 水特征曲线(SWCC)和渗透系数)是耗时且昂贵的。结果,研究人员和工程师通常采用用于确定土壤的SWCC和渗透函数的间接方法。本文提出了一种新方法,用于估计来自粗粒土壤的晶粒尺寸分布(GSD)的SWCC。该方法基于土壤不经历任何体积变化的假设,并且SWCC的滞后被忽略。本研究采用大于零的接触角​​。从拟议模型计算的结果与来自已发布研究的实验数据相得益彰。

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