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    开挖和降雨影响下岩溶隧道隔水岩体突水灾变机理

    Catastrophic Mechanism of Water-Resistant Rock Mass Ahead of Karst Tunnel Under the Action of Excavation and Rainfall

    • 摘要: 围绕岩溶隧道裂隙型隔水岩体突水灾变机理,基于断裂力学和两带理论推导了裂隙型隔水岩体发生岩桥拉剪破坏下临界水压力和失稳突水判据,系统分析了隧道开挖卸荷、降雨以及降雨与隧道开挖耦合作用下裂隙型隔水岩体的破坏机制.采用可考虑岩体结构特征的三维离散元方法研究了不同扰动条件下灾变演化过程.研究结果表明:随隧道近接岩溶,掌子面位移机制由开挖卸荷主导转为卸荷-渗流耦合作用,位移和水压持续增长,且中心点位移显著大于周边,呈现突变特征;降雨使掌子面位移不断增加,临界破坏前增速急剧上升;开挖与降雨耦合作用加剧了位移增长速率,其变化规律与单一作用相似但响应更剧烈.该研究成果可为岩溶隧道突水灾害防控和应急救援提供理论依据.

       

      Abstract: Focused on the water inrush mechanism of fissure water-resistant rock mass ahead of karst tunnel,the water pressure and instability criterion for tensile-shear failure of rock bridges in fissure water-resistant were derived,and the failure mechanisms under tunnel excavation,rainfall,and their coupled effects were systematically analyzed.The three-dimensional discrete element numerical simulation method capable of accounting for rock structural characteristics was employed to analyze the catastrophic evolution laws during under various disturbance conditions.The results indicate that as the tunnel approaches the karst cavity,the tunnel face displacement transitions from being dominated by excavation unloading to a coupled unloading-seepage effect,with both displacement and water pressure increasing continuously.The displacement at the center of the face is significantly larger than at the periphery and exhibits abrupt changes.Rainfall leads to a continuous increase in face displacement,with a sharp acceleration in the growth rate immediately prior to critical failure.The coupled effect of excavation and rainfall further intensifies the displacement growth rate,while the overall trends remain similar to those under individual effect,but the response is more severe.The research outcomes can provide a theoretical basis for the prevention and control of water inrush and emergency response in karst tunnels.

       

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