Effect of in-situ stress on fracture formation process of rock mass in presplit blasting
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摘要: 地应力显著影响岩体爆破裂纹的扩展行为和分布特征,导致深部岩体超/欠挖等问题。本文基于弹性力学理论建立了地应力下岩体预裂爆破理论模型,通过Laplace变换和数值反演的方法分析了爆炸应力波的衰减规律,讨论了地应力对岩体预裂爆破应力场分布的影响。此外,采用显式动力学有限元方法模拟了静水压力和非静水压力条件下岩体预裂爆破的压力演化过程和裂纹扩展行为,并通过Hough变换的方法定量表征了爆炸裂纹的分布特征。研究结果表明:深部岩体预裂爆破成缝困难主要是由于地应力削弱了爆炸引起的切向拉应力作用,孔间岩体质点因切向位移受限而无法形成拉伸破裂面,拉伸破裂成缝机制通过切向拉应力演化和质点位移矢量变化得以验证。基于应力波干涉破坏理论提出的预裂爆破孔间成缝准则可以预测岩体孔间裂纹是否贯穿,得到的不同地应力条件下装药直径和孔距的关系可用于指导预裂孔布置方式,从而为岩体预裂爆破提供理论指导。
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Abstract: The evolution and distribution characteristics of cracks in presplit blasting can be significantly affected by the in-situ stress, leading to problems such as over/under excavation in deep rock masses. In this investigation, a theoretical model for rock presplit blasting under initial stress was developed based on elastic mechanics. The propagation and attenuation process of explosion stress waves were analyzed by the combination of Laplace transforms and numerical inversion. Then, the influence of initial static stress on the blasting dynamic stress field distribution in presplitting was analyzed. In addition, the explicit dynamic numerical approach was employed to simulate the failure process in presplit blasting under both hydrostatic pressure and anisotropy pressure conditions, and the effects of static and dynamic stresses on cracking behavior and pressure evolution are reproduced and discussed. Moreover, the distribution characteristics of blasting cracks are quantitatively characterized by the Hough transform method. The results showed that the crack coalescence difficulty in deep rock presplitting is primarily attributed to the reduction of tangential tensile stress induced by the in-situ stress. The rock particles between boreholes fail to form tensile fracture planes due to restricted tangential displacements, which was demonstrated by the evolution of circumferential tensile stress and particle displacement vectors. Furthermore, the crack coalescence criterion in presplit blasting was proposed to predict whether inter-borehole cracks penetrate based on the theory of stress wave interference damage, and the relationship between charge diameter and hole spacing under various in-situ stress can guide the arrangement of boreholes, thus improving the presplit blasting effectiveness for deep rock masses. -
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