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Numerical Simulation on Zonal Disintegration in Deep Surrounding Rock Mass

机译:围岩深层岩体区分解的数值模拟

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Zonal disintegration have been discovered in many underground tunnels with the increasing of embedded depth. The formation mechanism of such phenomenon is difficult to explain under the framework of traditional rock mechanics, and the fractured shape and forming conditions are unclear. The numerical simulation was carried out to research the generating condition and forming process of zonal disintegration. Via comparing the results with the geomechanical model test, the zonal disintegration phenomenon was confirmed and its mechanism is revealed. It is found to be the result of circular fracture which develops within surrounding rock mass under the high geostress. The fractured shape of zonal disintegration was determined, and the radii of the fractured zones were found to fulfill the relationship of geometric progression. The numerical results were in accordance with the model test findings. The mechanism of the zonal disintegration was revealed by theoretical analysis based on fracture mechanics. The fractured zones are reportedly circular and concentric to the cavern. Each fracture zone ruptured at the elastic-plastic boundary of the surrounding rocks and then coalesced into the circular form. The geometric progression ratio was found to be related to the mechanical parameters and the ground stress of the surrounding rocks.
机译:在许多地下隧道中发现了区分解,随着嵌入深度的增加。这种现象的形成机制难以在传统岩石力学的框架下解释,并且裂缝形状和形成条件尚不清楚。进行数值模拟,以研究生成条件及其区分解的形成过程。通过将结果与地质力学模型试验进行比较,确认了区域崩解现象,并揭示了其机制。发现是圆形骨折的结果,该骨折在高地距离下的周围岩石质量内发展。确定了区内崩解的裂缝形状,发现裂缝区的半径达到几何进展的关系。数值结果符合模型测试结果。基于骨折力学的理论分析揭示了区分解的机制。据报道,骨折区域是圆形和同心的洞穴。每个骨折区域在周围岩石的弹性边界处破裂,然后聚集成圆形形式。发现几何进展比与机械参数和周围岩石的地基应力有关。

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