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Estimation of rockburst wall-rock velocity invoked by slab flexure sources in deep tunnels

机译:深隧道中板状挠性源引起的岩爆壁岩速度估算

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摘要

For rock support in burst-prone ground, the wall-rock velocity adjacent to the surface of underground openings is a vital support design parameter, and depends on the seismic source mechanism inducing rockburst damage. In this study, to estimate the wall-rock velocity evoked only by rock slab buckling (an important rockburst source mechanism), a comprehensive velocity assessment method is proposed, using an excellent slab column buckling model with a small eccentricity, which relies on a novel compressive or tensile buckling failure criterion of rock slab. The true-triaxial loading–unloading tests and rockburst case analyses reveal that rock mass slabbing induced by high rock stress has major impacts on the evolution and formation of buckling rockburst in deep tunnels. Using a method based on the energy balance principle, the slabbing thickness of intact rock mass is also calculated by an analytical method, which indicates that the slabbing thickness parameter has a nonlinear relation to the following six parameters: uniaxial tensile strength (UTS), uniaxial compressive strength (UCS), normal stress (σ_n), length of joint (L), friction angle (ф_r), and joint roughness coefficient (JRC). These proposed models and methods have been quite successfully applied to rockburst and slabbing cases occurring in deep tunnels. These applications show that slab flexure is an important source mechanism invoking high wall-rock velocities and leading to severe rockburst damages in the area surrounding deep tunnels.
机译:对于易爆地面中的岩石支撑,与地下洞口表面相邻的壁-岩速是至关重要的支撑设计参数,并且取决于引起岩爆破坏的地震源机制。在这项研究中,为了估计仅由板坯屈曲引起的壁岩速度(一种重要的岩爆源机制),提出了一种综合的速度评估方法,该方法采用了一种新颖的,具有小偏心率的优良板坯柱屈曲模型,该方法基于一种新颖的方法。板的压缩或拉伸屈曲破坏准则真三轴装卸试验和岩爆案例分析表明,高岩石应力引起的岩体平板对深部隧道屈曲岩爆的演化和形成有重要影响。使用基于能量平衡原理的方法,还通过解析方法来计算完整岩体的平板厚度,这表明平板厚度参数与以下六个参数具有非线性关系:单轴抗拉强度(UTS),单轴抗压强度(UCS),法向应力(σ_n),接头长度(L),摩擦角(ф_r)和接头粗糙度系数(JRC)。这些建议的模型和方法已经非常成功地应用于深部隧道发生的岩爆和平板情况。这些应用表明,平板挠曲是激活高围岩速度并导致深部隧道周围区域严重岩爆破坏的重要动力源机制。

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