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A thermo-hydro-mechanical constitutive model and its numerical modelling for unsaturated soils

机译:非饱和土的热-水-力学本构模型及其数值模拟

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A thermo-hydro-mechanical (THM) constitutive model for unsaturated soils is proposed in this paper based on the existing models. The influences of temperature on the hydro-mechanical behaviour in unsaturated soils are described in the model. Particularly, 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, is quantitatively modelled by using the experimental data and previous work [J. Geotech. Eng. ASCE 116 (12) (1990) 1765; J. Geotech. Eng. ASCE 116 (12) (1990) 1778; Can. Geotech. J. 25 (1988) 807; Int. J. Numer. Anal. Meth. Geomech. 22 (1998) 549; Can. Geotech. J. 37 (2000) 607; Characterisation and thermo-hydro-mechanical behaviour of unsaturated Boom clay: an experimental study. Thesis Doctoral 1999, Technical University of Catalonia (UPC), Barcelona, Spain]. Numerical modelling of the proposed THM model has also been implemented within the finite element code LAGACOM. Finally, the comparisons of the results obtained from the numerical modelling of the constitutive behaviour with existing experimental results show that the present model can simulate the thermo-hydro-mechanical behaviour in unsaturated soils with satisfaction. Some other numerical results given in the paper also validate the versatility and applicability of the present constitutive model.
机译:在现有模型的基础上,提出了非饱和土的热-水-力学(THM)本构模型。模型中描述了温度对非饱和土壤中水力-力学行为的影响。特别是,通过使用实验数据和先前的工作来定量地模拟热软化现象,即预固结压力的值减小以及SI(吸力增加)曲线的吸力的临界值随加热过程的降低。 Geotech。 。 ASCE 116(12)(1990)1765; J. Geotech。 。 ASCE 116(12)(1990)1778;能够。 Geotech。 J.25(1988)807;诠释J.纽默肛门方法Geomech。 22(1998)549;能够。 Geotech。 J.37(2000)607;非饱和动臂粘土的表征及其热-水-力学行为:一项实验研究。西班牙巴塞罗那,加泰罗尼亚技术大学(UPC),1999年获得博士学位论文。拟议的THM模型的数值建模也已在有限元代码LAGACOM中实现。最后,将本构关系的数值模型所得结果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。

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