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中文核心期刊

应力波作用下隧洞顶板围岩块体失稳滑动解析理论研究

ANALYTICAL THEORY ON INSTABILITY SLIDING OF SURROUNDING ROCK BLOCKS IN TUNNEL ROOF UNDER STRESS WAVE ACTIONS

  • 摘要: 由于地质结构和开挖面的影响, 隧洞围岩通常被切割成不同形状和尺寸的块体. 其中, 一些关键块体在开挖卸载后仍然保持稳定, 但当受到应力波(如爆破振动和地震等)的干扰时可能会失去稳定性并滑动. 基于应力波传播理论推导了隧洞围岩顶板矩形关键块体动力失稳滑动解析模型, 在计算块体滑动位移过程中, 考虑了块体间节理的不同闭合−张开模式, 并采用线弹性模型和库仑滑移模型来描述节理的法向和切向行为. 通过UDEC数值模型验证了解析模型的有效性和可靠性. 随后, 基于解析模型探讨了可能影响块体失稳滑动的参数. 研究结果表明: 在应力波作用下, 隧洞围岩块体间节理面会闭合−张开, 在张开过程中节理面的摩擦力会逐渐降低, 甚至为零, 块体间节理面的超低摩擦和无摩擦阶段对块体滑动位移的影响最大; 当应力波垂直作用于围岩块体结构面且强度足以诱使节理面张开时, 影响块体滑动位移较大的参数是节理面初始法向应力、应力波振幅、频率和块体岩性, 单周期正弦应力波下块体滑动位移的变化在0.659 ~ 1.502 mm之间; 其次为节理初始法向刚度、块体尺寸, 块体滑动位移的变化在0.15 ~ 0.168 mm之间.

     

    Abstract: Due to the effect of geological structure and excavation surface, the surrounding rock of the tunnel is usually cut into blocks with different shapes and scales. Among them, some key blocks remain stable after excavation unloading, however, they may lose their stability and slide when disturbed by stress waves, e.g., blasting vibration or earthquakes. Based on the theory of stress wave propagation, an analytical model for the dynamic instability and sliding of rectangular key blocks in the roof of tunnel surrounding rock was derived. In the calculation of block slide displacement, different close-open modes of joints between blocks are considered, and linear elastic model and Coulomb slip model are used to describe the normal and tangential behavior of joints. The effectiveness and reliability of the analytical model were verified through UDEC numerical model. Then, the parameters that may affect the instability and slide of the block were discussed based on the analytical model. The research results indicate that the joint surfaces between the tunnel surrounding rock blocks will close and open under the action of stress waves. During the opening process, the friction force between the joint surfaces will gradually decrease or even become zero. The ultra-low friction and non friction stages of the joint surfaces between the blocks have the greatest impact on the slide displacement of the blocks. When the stress wave acts vertically on the structural surface of the surrounding rock block and its strength is sufficient to induce the opening of the joint surface, the parameters that significantly affect the slide displacement of the block are the initial normal stress of the joint surface, the amplitude and frequency of the stress wave, and the rock type of the block. The variation of the slide displacement of the block under a single period sine stress wave is between 0.659 and 1.502 mm. The influence of initial normal stiffness of joints and block size is followed, and the variation of block slide displacement is between 0.15 and 0.168 mm.

     

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