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沈佳轶, 陈前, 库猛, 王立忠. 基于CEL的灵敏性黏土斜坡渐进破坏数值模拟研究[J]. 岩土工程学报, 2022, 44(12): 2297-2303. DOI: 10.11779/CJGE202212017
引用本文: 沈佳轶, 陈前, 库猛, 王立忠. 基于CEL的灵敏性黏土斜坡渐进破坏数值模拟研究[J]. 岩土工程学报, 2022, 44(12): 2297-2303. DOI: 10.11779/CJGE202212017
SHEN Jia-yi, CHEN Qian, KU Meng, WANG Li-zhong. Numerical simulation of progressive failure of sensitive clay slopes using CEL method[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(12): 2297-2303. DOI: 10.11779/CJGE202212017
Citation: SHEN Jia-yi, CHEN Qian, KU Meng, WANG Li-zhong. Numerical simulation of progressive failure of sensitive clay slopes using CEL method[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(12): 2297-2303. DOI: 10.11779/CJGE202212017

基于CEL的灵敏性黏土斜坡渐进破坏数值模拟研究

Numerical simulation of progressive failure of sensitive clay slopes using CEL method

  • 摘要: 为了揭示灵敏性黏土斜坡渐进破坏机理,以加拿大Saint-Jude滑坡为研究案例,采用耦合欧拉-拉格朗日(Coupled Eulerian-Lagrangian,CEL)框架下的欧拉方法,开展灵敏性黏土斜坡渐进破坏数值模拟研究。研究结果表明:CEL数值模拟得到的Saint-Jude滑坡地形与现场勘测滑坡地形基本一致;CEL数值模拟方法可以有效地模拟灵敏性黏土斜坡从初始失稳破坏到后续渐进破坏的全过程,真实还原Saint-Jude滑坡的渐进破坏模式;CEL数值模拟方法有效地模拟灵敏性黏土斜坡渐进破坏过程中剪应力的演化特征,从而揭示灵敏性黏土斜坡渐进破坏机理。

     

    Abstract: In order to reveal the mechanism of the progressive failure of sensitive clay slopes, the Saint-Jude landslide in Canada is used as a research case, and the Eulerian approach under the coupled Eulerian-Lagrangian (CEL) framework is used to carry out the numerical simulation. The research results show that: (1) The topography of the Saint-Jude landslide obtained by the CEL numerical simulation is basically consistent with the field surveyed one. (2) The CEL numerical simulation method can effectively simulate the sensitive clay landslides from the initial instability failure to the subsequent progressive failure, and the progressive failure mode of the Saint-Jude landslide can be truly simulated. (3) The CEL numerical simulation method effectively captures the characteristics of shear stress during the progressive failure of the sensitive clay slope, thereby revealing the mechanism of progressive failure of sensitive clay slopes.

     

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