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Including degree of capillary saturation into constitutive modelling of unsaturated soils

机译:将毛细管饱和度纳入非饱和土的本构模型

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The degree of saturation (S) of soil can be separated into two components: the degree of capillary saturation (S') that is based on the capillary water and the degree of adsorptive saturation (S '') that is based on the adsorbed water. This paper discusses the role of the degree of capillary saturation (S') in modelling the coupled hydro mechanical behaviour of unsaturated soils and proposes a new constitutive model for unsaturated soils by using the degree of capillary saturation (S') and the effective inter-particle stress tap. An enhanced hydraulic model is introduced to describe the hydraulic hysteresis and hydro-mechanical interaction in terms of the degree of capillary saturation (S'). In the proposed constitutive model, the shear strength, yield stress and deformation behaviour of unsaturated soils are governed directly by the above two constitutive variables, namely oil and S'. To be in line with the existing finite element frameworks for unsaturated soils, the proposed model is eventually generalised to constitutive functions consisting of only primary variables such as the net stress (sigma(ij)), suction (s) and degree of saturation (S). The typical performance of the model for simulating the characteristic trends of unsaturated soil behaviour is discussed in several different scenarios. The model is then validated against a variety of experimental data in the literature, and the results show that a reasonable agreement can be obtained using this new constitutive model.
机译:土壤的饱和度(S)可以分为两个部分:基于毛细管水的毛细管饱和度(S')和基于吸附水的吸附饱和度(S'') 。本文讨论了毛细饱和度(S')在模拟非饱和土的水力耦合行为中的作用,并通过利用毛细饱和度(S')和有效相互作用来提出一种新的非饱和土本构模型。粒子应力水龙头。引入了增强的水力模型,以毛细管饱和度(S')来描述水力滞后和水力相互作用。在提出的本构模型中,非饱和土的抗剪强度,屈服应力和变形特性直接受上述两个本构变量即油和S'的支配。为了与不饱和土壤的现有有限元框架相一致,所提出的模型最终被推广到仅包含主要变量(例如净应力(sigma(ij)),吸力(s)和饱和度(S))的本构函数。 )。在几种不同的情况下,讨论了用于模拟非饱和土行为特征趋势的模型的典型性能。然后针对文献中的各种实验数据对该模型进行了验证,结果表明,使用这种新的本构模型可以获得合理的一致性。

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