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李栋伟, 汪仁和, 范菊红. 白垩系冻结软岩非线性流变模型试验研究[J]. 岩土工程学报, 2011, 33(3): 398.
引用本文: 李栋伟, 汪仁和, 范菊红. 白垩系冻结软岩非线性流变模型试验研究[J]. 岩土工程学报, 2011, 33(3): 398.
LI Dong-wei, WANG Ren-he, FAN Ju-hong. Nonlinear rheological model for frozen soft rock during Cretaceous period[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(3): 398.
Citation: LI Dong-wei, WANG Ren-he, FAN Ju-hong. Nonlinear rheological model for frozen soft rock during Cretaceous period[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(3): 398.

白垩系冻结软岩非线性流变模型试验研究

Nonlinear rheological model for frozen soft rock during Cretaceous period

  • 摘要: 通过高围压固结、低温冻结后再加卸载的试验方法模拟白垩系冻结软岩地下工程施工应力状态变化过程,大量的试验结果表明:白垩系地层冻结软岩存在起始临界应力阈值,且符合Mises强度函数准则;冻结软岩黏滞系数是时间的一次函数,拟合相关系数达0.99以上。根据试验提出了冻结软岩黏弹塑非线性蠕变本构力学模型,将现场实测结果与计算值进行对比:两者变形规律完全一致且数值较吻合,从而验证了低温软岩本构模型的正确性,可为冻结地下工程和寒区岩土工程数值计算提供参考。

     

    Abstract: The test method of consolidation by high confining pressure, freezing at low temperature and loading-unloading is employed to simulate the change process of stress state of underground engineering in Cretaceous frozen soft rock during construction. A large number of test results show that there is an initial critical stress threshold value in Cretaceous frozen soft rock, and it meets the Mises strength function criteria. The viscosity coefficient of frozen soft rock is a linear function of time, and the fitting correlation coefficient is up to 0.99. A frozen soft rock nonlinear viscoelastic-plastic creep constitutive mechanical model is proposed. The creep test results are compared with the calculated values, and their deformation laws are exactly the same and the values are in good agreement. The low temperature soft rock constitutive model is validated to be correct and can provide numerical calculation reference for the frozen underground engineering and geotechnical engineering in cold regions.

     

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