Volume 40 Issue 7
Jul.  2020
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YANG Jianhua, SUN Wenbin, YAO Chi, ZHANG Xiaobo. Mechanism of rock fragmentation by multi-hole blasting in highly-stressed rock masses[J]. Explosion And Shock Waves, 2020, 40(7): 075202. doi: 10.11883/bzycj-2019-0427
Citation: YANG Jianhua, SUN Wenbin, YAO Chi, ZHANG Xiaobo. Mechanism of rock fragmentation by multi-hole blasting in highly-stressed rock masses[J]. Explosion And Shock Waves, 2020, 40(7): 075202. doi: 10.11883/bzycj-2019-0427

Mechanism of rock fragmentation by multi-hole blasting in highly-stressed rock masses

doi: 10.11883/bzycj-2019-0427
  • Received Date: 2019-11-07
  • Rev Recd Date: 2020-04-20
  • Publish Date: 2020-07-01
  • During blasting in deep rock masses, the rock fragmentation is contributed to the combined effects of blast loading and high in-situ stress. An analysis model based on simplifying assumptions was developed for double-hole blasting in highly-stressed rock masses, and the crack propagation and dynamic stress evolution surrounding the blastholes were studied by using the coupled SPH (smoothed particle hydrodynamics)-FEM(finite element method) method. The results show that the blast-induced rock cracking is mainly caused by the dynamic circumferential tensile stress generated from blast loading. However, in the rock masses subjected to in-situ stress, the dynamic circumferential tensile stress is reduced in magnitude and duration due to the compressive effect of the in-situ stress. Therefore, the in-situ stress plays a role in inhibiting the rock fragmentation caused by blasting. For the case of multi-hole blasting in a hydrostatic in-situ stress field, the crack propagation perpendicular to the connecting line between the adjacent holes is more easily inhibited by the in-situ stress. The length of blast-induced crack growth decreases with an increase in the in-situ stress level. With regard to a non-hydrostatic in-situ stress field, the crack propagation along the direction of the minimum principal in-situ stress is most severely suppressed, and thus the cracks grow preferentially along the maximum principal stress direction. Therefore, arranging the blastholes along the maximum principal stress direction and shortening the spacing between the blastholes will facilitate the crack connections and the formation of excavation surfaces.
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