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2D numerical analysis of rock damage induced by dynamic in-situ stress redistribution and blast loading in underground blasting excavation

机译:地下爆破开挖过程中地应力动态分布和爆炸荷载对岩石破坏的二维数值分析

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摘要

When underground cavities are created in initially stressed rock masses by the drill and blast method, an unwanted excavation damage zone (EDZ) is induced around the cavities due to the combined effects of in-situ stress redistribution and blast loading. During rock fragmentation by blasting, the in-situ stress on blast-created excavation boundaries is suddenly released. The in-situ stress redistribution is a dynamic process that starts from the transient release of stress and reaches a final static stress state after excavation. For a circular tunnel that is excavated underground by full-face millisecond delay blasting, 2D finite element simulation is performed to investigate the rock damage induced by the dynamic in-situ stress redistribution and blast loading. The critical peak particle velocity (PPV) for the initiation of blast damage in pre-stressed rock masses is also numerically studied. The results show that the transient stress release generates additional stress waves, resulting in a larger damage zone compared with that following quasi-static stress redistribution. The effect that the additional stress waves have on rock damage becomes more obvious as the in-situ stress levels and excavation dimensions increase and as the stress release duration decreases. Blast-induced tensile stress in the circumferential direction of a tunnel is neutralized by compressive in-situ stress. In deep-buried or high-stressed tunnel excavation, dynamic stress redistribution is responsible for the formation of EDZ; the critical PPV for the initiation of blast damage first increases and then decreases with an increase in the in-situ stress. Therefore, in underground blasting excavation, the factors that affect the level of in-situ stress such as tunnel depths should be considered with respect to the blasting vibration standards and damage criteria.
机译:当通过钻孔和爆破方法在最初受力的岩体中形成地下洞时,由于现场应力再分配和爆破载荷的共同作用,在洞周围会产生有害的开挖破坏区(EDZ)。在爆破造成的岩石碎裂过程中,爆炸产生的开挖边界上的原地应力会突然释放。原位应力再分布是一个动态过程,其过程是从应力的瞬时释放开始,到开挖后达到最终的静态应力状态。对于通过全断面毫秒延迟爆破在地下开挖的圆形隧道,进行了二维有限元模拟,以研究动态地应力再分配和爆破载荷对岩石的破坏。还对在预应力岩体中爆炸破坏的临界峰值粒子速度(PPV)进行了数值研究。结果表明,与准静态应力再分布相比,瞬态应力释放会产生额外的应力波,从而导致更大的损伤区域。随着原地应力水平和开挖尺寸的增加以及应力释放持续时间的减少,附加应力波对岩石破坏的影响变得更加明显。爆炸在隧道圆周方向上产生的拉伸应力被压缩原位应力抵消。在深埋或高应力隧道开挖中,动应力的重新分布负责形成EDZ。爆炸破坏引发的临界PPV首先增加,然后随着原位应力的增加而降低。因此,在地下爆破开挖中,应考虑爆破振动标准和破坏标准,考虑影响地应力水平的因素,例如隧道深度。

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