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Experimental investigation and constitutive modelling of thermo-hydro-mechanical coupling in unsaturated soils.

机译:非饱和土壤中热-水-力耦合的实验研究和本构模型。

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摘要

A thermo-elastic-plastic model for unsaturated soils has been presented based on theeffective stress principle considering the thermo-mechanical and suction couplingeffects. The thermo-elastic-plastic constitutive equations for stress-strain relations of thesolid skeleton and changes in fluid content and entropy for unsaturated soils have beenestablished. A plasticity model is derived from energy considerations. The modelderived covers both associative and non-associative flow behaviours and the modifiedCam-Clay is considered as a special case. All model coefficients are identified in termsof measurable parameters.To verify the proposed model, an experimental program has been developed. A series ofcontrolled laboratory tests were carried out on a compacted silt sample using a triaxialequipment modified for testing unsaturated soils at elevated temperatures. Imageprocessingtechnique was used for measuring the volume change of the samplessubjected to mechanical, thermal and hydric loading.It is shown that the effective critical state parameters M, κ and λ are independent oftemperature and matric suction. Nevertheless, the shape of loading collapse (LC) curvewas affected by temperature and suction. Furthermore, the temperature change affectedthe soil water characteristic curve and an increase in temperature caused a decrease inthe air entry suction.The simulations from the proposed model are compared with the experimental results.The model calibration was performed to extract the model parameters from theexperimental results. Good agreement between the results predicted using the proposedmodel and the experimental results was obtained in all cases.
机译:基于有效应力原理,提出了考虑热力耦合和吸力耦合效应的非饱和土热弹塑性模型。建立了固体骨架的应力-应变关系以及非饱和土的流体含量和熵的变化的热弹塑性本构方程。可塑性模型是从能源考虑得出的。源自模型的模型涵盖了关联和非关联的流动行为,并且修改后的Cam-Clay被视为特例。所有模型系数均根据可测量参数进行识别。为了验证所提出的模型,开发了一个实验程序。使用改良的三轴设备对压实的粉土样品进行了一系列受控的实验室测试,这些设备经过改良,可以在高温下测试非饱和土壤。图像处理技术用于测量受机械,热和液压载荷作用的样品的体积变化。结果表明,有效临界状态参数M,α和与温度和基质吸力无关。然而,负荷塌陷(LC)曲线的形状受温度和吸力的影响。此外,温度变化影响土壤水分特征曲线,温度升高导致进风吸力下降。将所建模型的仿真结果与实验结果进行比较,进行模型校准以从实验结果中提取模型参数。在所有情况下,使用提议的模型预测的结果与实验结果之间都取得了很好的一致性。

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