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A thermo-elasto-plastic model for normally consolidated and overconsolidated soils

机译:正常固结和超固结土的热弹塑性模型

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摘要

A constitutive, non-isothermal unified hardening (UH) model is presented to interpret the thermo-elastoplastic behaviours of normally consolidated (NC) and overconsolidated (OC) clays. Two yield surfaces (the current yield surface and the reference yield surface) are adopted in the proposed model. A unified hardening parameter (H) is developed to describe the evolution of the current yield surface, and the plastic volumetric strain is employed to quantify the hardening of the reference yield surface. The similarity ratio (R_T) between the current yield surface and the reference yield surface, which is a function of the temperature and plastic volumetric strain, is developed to govern the volume change behaviour and the shear strength of soils with different stress histories and at varying temperatures. The proposed model is then validated through test results in the literature.
机译:提出了本构非等温统一硬化(UH)模型来解释正常固结(NC)和超固结(OC)粘土的热弹塑性行为。该模型采用了两个屈服面(当前屈服面和参考屈服面)。开发了统一的硬化参数(H)来描述当前屈服面的演变,并使用塑性体积应变来量化参考屈服面的硬化。当前屈服面与参考屈服面之间的相似度(R_T)是温度和塑性体积应变的函数,用于控制不同应力历史和不同应力下土壤的体积变化行为和剪切强度。温度。然后通过文献中的测试结果来验证所提出的模型。

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