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Soil-water characteristic curves and permeability of Shanghai soft soils

机译:土壤 - 水特征曲线和上海软土的渗透性

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Soil-water characteristics curve (SWCC) is a fundamental constitutive relation for the explanation of the engineering behavior of unsaturated soil. The study of SWCC is helpful for reducing the time and cost of unsaturated soil testing for engineering purposes. Some properties of unsaturated soils, such as shear strength and permeability, can be predicted from it. After a brief introduction to osmotic technique and vapour phase method, the SWCCs of Shanghai soft soil have been obtained and some basic characteristics of the SWCCs have been analyzed. Coefficient of permeability is an important parameter for unsaturated soils, but the wide range in coefficient of permeability has been proven to be a major obstacle in analyzing seepage problems. Childs and Collis-George proposed a model for predicting the coefficient of permeability based on the random variation of pore size. It was improved several times and proved to be effective. Based on this model, the relative coefficients of permeability of Shanghai soft soil are predicted from the soil-water characteristic curves. Results show that unsaturated permeability of Shanghai soft soil changes nonlinearly with suction.
机译:土壤 - 水特征曲线(SWCC)是对不饱和土工程行为的解释的基本组成关系。对SWCC的研究有助于减少工程目的不饱和土验的时间和成本。可以从中预测不饱和土壤的一些不饱和土的性质,例如剪切强度和渗透性。在简要介绍渗透技术和气相方法后,已经获得了上海软土的SWCC,并分析了SWCC的一些基本特征。渗透系数是不饱和土壤的重要参数,但是在分析渗流问题方面被证明是渗透系数的广泛范围。 Childs和Collis-George提出了一种用于基于孔径的随机变异来预测渗透系数的模型。它有几次改善并证明是有效的。基于该模型,从土壤 - 水特征曲线预测上海软土的渗透性的相对系数。结果表明,上海软土的不饱和渗透性随吸力而变化。

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