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Numerical Simulation on Zonal Disintegration in Deep Surrounding Rock Mass

机译:深部围岩分区破坏的数值模拟。

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摘要

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:随着埋深的增加,在许多地下隧道中发现了带状崩解。在传统岩石力学的框架下,这种现象的形成机理难以解释,断裂的形态和形成条件尚不清楚。通过数值模拟研究了区域崩解的产生条件和形成过程。通过将结果与地质力学模型试验相比较,证实了区域崩解现象,并揭示了其机理。发现这是圆形裂缝的结果,该裂缝是在高地应力下在围岩内部形成的。确定了带状崩解的断裂形状,发现断裂带的半径满足几何级数的关系。数值结果与模型测试结果一致。通过基于断裂力学的理论分析揭示了层状崩解的机理。据报道,断裂带是圆形的,与洞穴同心。每个断裂带在围岩的弹塑性边界处破裂,然后合并为圆形。发现几何级数比与力学参数和围岩的地面应力有关。

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