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Constitutive Modelling of Coupled Thermo-Hydro-Mechanical Behaviour in Unsaturated Soils

机译:非饱和土中热-水-力耦合行为的本构模型

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A thermo-hydro-mechanical constitutive model for unsaturated soils is proposed in this paper based on the existing models. The thermal softening phenomenon, i.e. decreases in value of the pre-consolidation pressure and in critical value of the suction of the SI (Suction Increasing) curve with heating process, are quantitatively modelled by using the experimental data and previous work [1-3]. The thermal yield behavior is also described in the present model [4]. A backward Euler return mapping procedure [5] in order to deal with non-smooth multi-surface plasticity is implemented in the finite element code CONVILAG. The comparisons of the results obtained from the numerical modelling of the constitutive behavior with existing experimental results show that the present model can simulate the thermo-hydro-mechanical behavior in unsaturated soils with satisfaction. Some other numerical results given in the paper also validate the versatility and applicability of the present constitutive model. The model has been extended to include the influences of chemo-mechanical effects, such as chemical softening [6] and cohesion change with respect to contaminant concentration. The coupled THMC constitutive model with it numerical modelling for unsaturated soils, as one of the important job, is performed in our research team.
机译:在现有模型的基础上,提出了非饱和土的热-水-力学本构模型。利用实验数据和先前的工作[1-3]对热软化现象(即预固结压力值的减小和SI(吸力增加)曲线的吸力的临界值随加热过程的降低)进行了建模。 。在当前模型中也描述了热屈服行为[4]。在有限元代码CONVILAG中实现了向后的Euler返回映射过程[5],以处理非光滑的多表面可塑性。将本构行为数值模型与现有实验结果进行比较,结果表明,该模型可以满意地模拟非饱和土壤中的热-水-力学行为。本文给出的其他一些数值结果也验证了本构模型的多功能性和适用性。该模型已扩展到包括化学机械效应的影响,例如化学软化[6]和相对于污染物浓度的内聚力变化。在我们的研究团队中,进行的耦合THMC本构模型及其对非饱和土的数值模拟是一项重要的工作。

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