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A New Soil-Water Characteristic Curve Model for Unsaturated Loess Based on Wetting-Induced Pore Deformation

机译:基于润湿诱导的孔隙变形的不饱和黄土的新土壤 - 水特性曲线模型

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摘要

The soil-water characteristic curve (SWCC) is the basis for describing seepage, strength, and constitutive model of unsaturated soil. The existing SWCC models do not work accurately for evaluating loess, because they do not consider the pore deformation that is induced by wetting. The present study develops a new SWCC model for unsaturated loess. The model considers the effect of wetting-induced pore deformation (WIPD) on the SWCC. The new model includes 6 parameters, which could be confirmed by laboratory tests. The pore volume function (PVF) was described by the WIPD. The shift factor ξ1i and the compression factor ξ2i were introduced into the model. The relationship between the void ratio e and ξ1i and ξ2i was established using the average pore radius. The new SWCC model for saturated loess was improved based on the classical van Genuchten (V-G) model. If the WIPD had not been considered, the new model would regress into the classical V-G model. SWCC tests of unsaturated loess with different void ratios were carried out to verify the new model. The model parameters were calibrated in the original state, and the SWCCs of different void ratios were predicted by the new model and found to be in good agreement with the test results.
机译:土壤 - 水特征曲线(SWCC)是描述不饱和土壤渗流,强度和本构模型的基础。现有的SWCC型号不准确地适用于评估黄土,因为它们不考虑通过润湿引起的孔变形。本研究为不饱和黄土开发了一种新的SWCC模型。该模型考虑了润湿诱导的孔变形(WIPD)对SWCC的影响。新模型包括6个参数,可以通过实验室测试确认。 WIPD描述了孔体积函数(PVF)。将换档因子ξ1i和压缩因子χ2i引入模型中。使用平均孔径半径建立空隙率E和ξ1i和ξ2i之间的关系。基于古典van Genuchten(V-G)模型,改善了新的SWCC模型。如果未考虑WIPD,则新模型将在古典V-G模型中归入。进行了具有不同空隙率比的不饱和黄土的SWCC测试以验证新模型。模型参数在原始状态下校准,并通过新模型预测不同空隙率的SWCC,发现与测试结果吻合良好。

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