深部硐室塑性区围岩软化特性分析

    Analysis on softening characteristics of surrounding rock in plastic zones of deep caverns

    • 摘要: 岩体介质的非线性和非均匀性表现在任意尺度上,基于连续性假设建立的几何方程以及本构方程难以适用于工程岩体的峰后变形与破坏过程,考虑到连续介质力学求解工程围岩应力与变形问题时所存在的现实短板,仅利用边界条件与平衡方程,以平均近似数学方法描述了围岩软化区内的应力分布,估算了圆形硐室塑性软化区的初始半径,并反演出了峰后内摩擦角的软化规律,结果表明软化规律可通过Boltzmann函数较好地描述;利用质量守恒定律对围岩变形进行了分析,研究结果可为深部地下工程长期稳定支护设计提供理论依据。

       

      Abstract: The nonlinearity and inhomogeneity of rock mass are manifested at any scale. Geometric equations and constitutive equations based on the continuity assumption cannot accurately characterize the post-peak deformation and failure processes of engineering rock masses. Considering the practical shortcomings of continuum mechanics in solving the stress and deformation in surrounding rock, this study employs only boundary conditions and equilibrium equations, and describes the stress distribution in the surrounding rock softening zone via an averaging approximation. Furthermore, the initial radius of the softening zone of circular openings estimated, and the softening law of the post-peak internal friction angle is back-calculated. The results show that the softening law can be well described by the Boltzmann function. In addition, the mass conservation law is applied to analyze the deformation of the surrounding rock. The research results can provide theoretical reference for the design of long-term stability support in deep underground engineering.

       

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