基于三维离散-连续耦合方法的跨活动断裂隧洞错断破坏机制研究
Disruption and destruction mechanism of cross-active fault tunnels based on 3D discrete-continuous coupling method
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摘要: 在中国西部强震区兴建的大型水利工程中,输水隧洞常不可避免地横跨多条区域性活动断裂,受活断裂错断运动影响,这些输水隧洞面临着严重的错断威胁。传统隧洞抗错断数值模拟方法多将围岩简单考虑为等效连续体,不能从细观尺度模拟断裂错动时围岩的破裂过程和大变形现象。将三维离散-连续耦合方法引入跨活动断裂隧洞抗错断问题的研究上,研究在断裂错动作用下衬砌的内力响应,及围岩破裂的细观特征。在该分析方法中,采用离散元球形颗粒表征围岩,同时将隧洞衬砌结构考虑为连续单元体。验证接触边界上耦合力的相容性与连续性的同时,通过参数标定使离散区域与连续区域的宏观属性一致,在此基础上建立穿越活动断裂隧洞的三维离散-连续耦合数值模型。利用这一方法,讨论了不同断裂错距影响下隧洞因断裂错动而产生的位移变化与力学响应,并从细观角度对围岩破坏特征进行了探讨。获得的结论可以为穿越活断裂隧洞的抗错断设计提供一定参考。Abstract: In the large-scale water conservancy projects built in strong earthquake regions in western China, the water conveyance tunnels inevitably crosse multiple regional active faults. Affected by the movement of the active faults, these water conveyance tunnels are faced with a serious threat of dislocation. The traditional anti-breaking numerical simulation methods for tunnels mostly consider the surrounding rock as the equivalent continuum, and they cannot simulate the fracture process from microscale and large deformation phenomenon of the surrounding rock when the fault is dislocated. The 3D discrete-continuum coupling method is used to study the anti-dislocation problem in a tunnel crossing active faults, and the mechanical response of the linings and the micro fracture characteristics of the surrounding rock mass under the action of fault dislocation are studied. In this analysis method, the discrete element spherical particles are used to model the surrounding rock mass, simultaneously, the lining structure of the tunnel is considered as a continuous zone. The compatibility and continuity of the coupling force at the contact boundary are verified, at the same time, the discrete region is consistent with the macroattributes of the continuous region through parameter calibration. On this basis, a 3D discrete-continuous coupling numerical model for tunnels crossing active faults is established. Using this method, the displacements and mechanical responses of the tunnels due to fault dislocation under different movement quantities of fault as well as the failure characteristics of the surrounding rock mass are discussed from the microscale. The conclusions may provide some reference for the anti-fault design of tunnels crossing active faults.