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Analysis of a Field Experiment to Assess the Performance of an Anisotropic Plasticity Model for Cohesive Soils

机译:评估粘性土各向异性塑性模型性能的现场试验分析

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A recently conducted field experiment is used to assess the significance of initial and induced anisotropy on the response of a layered soil system consisting of Ko-consolidated clay layers with different over-consolidation ratios. The soil is subjected to the weight of a trial soil embankment. To assess the role of soil anisotropy in the observed response of the layered soil system, a detailed nonlinear finite element analysis using a fully-coupled effective stress approach is conducted. The clayey soils are modeled by using two different constitutive models: an anisotropic soil plasticity model (SANI Clay) and the well-known isotropic clay plasticity model (modified CAM Clay). Both models were calibrated based on the laboratory and in-situ test data available for the soils. The results of the numerical simulations indicate that the proper modeling of initial and induced anisotropy has an important effect on the computed settlement of the layered soil and on the deformation of the soil embankment. It is observed that while the finite element simulations using SANI Clay closely reproduce the observed settlement of the soil embankment, the modified Cam Clay model underestimates the ultimate settlement of the embankment. There are also significant differences in the computed lateral displacements using the two constitutive models. The effect of soil anisotropy on generation and dissipation of excess pore pressures within the clay layers is also investigated and the results are presented.
机译:最近进行的野外实验被用来评估初始各向异性和诱导各向异性对由不同固结比的高固结粘土层组成的层状土壤体系的响应的重要性。土壤承受试验性土壤路堤的重量。为了评估土壤各向异性在分层土壤系统的观测响应中的作用,采用了全耦合有效应力方法进行了详细的非线性有限元分析。使用两种不同的本构模型对粘土进行建模:各向异性土壤可塑性模型(SANI Clay)和众所周知的各向同性粘土可塑性模型(改良的CAM Clay)。两种模型均根据可用于土壤的实验室和原位测试数据进行了校准。数值模拟结果表明,初始各向异性和诱导各向异性的正确建模对层状土的计算沉降和路堤变形具有重要影响。可以看出,尽管使用SANI Clay进行的有限元模拟紧密地再现了所观察到的路堤沉降,但改进的Cam Clay模型却低估了路堤的最终沉降。使用两个本构模型在计算出的横向位移方面也存在显着差异。还研究了土壤各向异性对粘土层内多余孔隙压力的产生和消散的影响,并给出了结果。

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