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Influence of Rock Strength on the Propagation of Slotted Cartridge Blasting-Induced Directional Cracks

机译:岩石强度对开槽盒喷射诱导方向裂纹传播的影响

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摘要

Based on theories of explosive mechanics and rock fracture mechanics, the influence mechanism of rock strength on the propagation length of the primary crack in the directional fracture blasting with slotted cartridge has been investigated deeply to propose the relation equation between the rock strength and the propagation length of the primary crack. Theoretically, the maximum length am of the primary crack increases with the enhancing rock strength parameters. The explicit dynamic analysis software LS-DYNA has been used to simulate the slotted cartridge blasting in the mudstone, sandstone, and granite with different strengths in order to reveal the effect of rock strength on the propagation length and velocity of the primary crack and the stress distribution characteristics in rock. The numerical results show the primary crack easily bifurcates and attain a much shorter propagation length in the mudstone with the minimum strength, and there are radial cracks appearing in the nonslotted direction. When rock strength rises, the propagation length, velocity, and duration of the primary crack and the concentration degree of effective stress in the slotted direction will all increase in the sandstone and granite, but there is an opposite influence trend of rock strength in the stage of the initial guide crack’s formation. The cracking velocity has an overall oscillation downtrend whose swing amplitude enhances clearly with the increasing rock strength, signifying the more unsteady propagation of the primary crack in the higher strength rock.
机译:基于爆炸力学和岩石骨折力学的理论,深深地研究了岩石盒的定向断裂爆破中初级裂纹传播长度的影响机理,提出了岩石强度与传播长度之间的关系方程主要裂缝。从理论上讲,主裂纹的最大长度AM随着增强的岩石强度参数而增加。显式动态分析软件LS-DYNA已被用于模拟泥岩,砂岩和花岗岩中的开槽墨盒,以不同的优点,以揭示岩石强度对初级裂纹和应力的传播长度和速度的影响岩石中的分布特征。数值结果显示主裂缝容易分叉并在泥岩中具有最小强度的泥岩中的更短的传播长度,并且在非透明方向上出现径向裂缝。当岩石强度升高时,初级裂纹的传播长度,速度和持续程度和开槽方向的有效应力的浓度将全部增加砂岩和花岗岩,但舞台上的岩石强度存在相反的影响趋势初始导向裂缝的形成。裂缝速度具有整体振荡下调,其摆幅随着岩石强度的增加而显着增强,意味着在更高强度岩石中的主要裂缝更不稳定地传播。

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