曹晓立, 高文学, 吕洪涛, 李竟艳, 张琪. 鲁坨路路堑边坡爆破应力波传播规律[J]. 北京工业大学学报, 2020, 46(3): 245-252. DOI: 10.11936/bjutxb2018060021
    引用本文: 曹晓立, 高文学, 吕洪涛, 李竟艳, 张琪. 鲁坨路路堑边坡爆破应力波传播规律[J]. 北京工业大学学报, 2020, 46(3): 245-252. DOI: 10.11936/bjutxb2018060021
    CAO Xiaoli, GAO Wenxue, LÜ Hongtao, LI Jingyan, ZHANG Qi. Propagation Law of Blasting Stress Wave in Lutuo Road Cutting Slope[J]. Journal of Beijing University of Technology, 2020, 46(3): 245-252. DOI: 10.11936/bjutxb2018060021
    Citation: CAO Xiaoli, GAO Wenxue, LÜ Hongtao, LI Jingyan, ZHANG Qi. Propagation Law of Blasting Stress Wave in Lutuo Road Cutting Slope[J]. Journal of Beijing University of Technology, 2020, 46(3): 245-252. DOI: 10.11936/bjutxb2018060021

    鲁坨路路堑边坡爆破应力波传播规律

    Propagation Law of Blasting Stress Wave in Lutuo Road Cutting Slope

    • 摘要: 为了解决边坡岩体内爆破应力波与介质相互作用以及爆破荷载作用下边坡动力稳定性问题,依托鲁坨路路堑边坡爆破工程,在现场爆破振动测试的基础上采用数值模拟的方法对边坡坡面以及岩体内部质点的振动速度、应力场等分布规律进行深入研究.结果表明:1)对于坡面质点,水平爆心距与高程的增加均会使爆破峰值振速总体呈衰减趋势,但台阶边缘"鞭梢效应"明显,且距离爆源越近,峰值振速放大系数越大.2)边坡台阶坡角处应力集中显著,但峰值应力与峰值振速并非在同一位置出现.因此,不能将台阶外缘峰值振速作为评价边坡稳定性的单一指标.3)对于岩体内部质点,爆破振动响应也随爆心距的增大逐渐衰减,但坡面和岩层分界面对应力波的反射叠加会造成岩体质点的峰值振速和应力均有所放大.

       

      Abstract: To solve the problem of interaction between the blasting stress wave and the medium in the rock mass of the slope and the dynamic stability of the slope under the blasting load, based on the blasting vibration of Lutuo road cutting slope, the vibration velocity, stress field, etc. of the slope surface and the media internal particle were deeply studied by using numerical simulation methods in this paper. Results show that:1) For the particles at the slope surface, the increase of the horizontal blasting distance and the elevation cause the peak velocity of the blasting to decrease. However, the whiplash effect at the edge of the step is obvious, and the closer to the source, the larger the amplification factor of the peak vibration velocity is. 2) The stress concentration at the foot of the slope is significant. However, the maximum value of the stress does not coincide with the position where the peak vibration velocity occurs. Therefore, it is not reasonable to simply use the peak vibration velocity of the particle at the edge of the slope as an indicator for evaluating the stability of the slope. 3) For the particles inside the rock mass, the blasting vibration also gradually decays with the increase of the distance to the blasting source. However, the superposition of the reflection of the stress wave on the slope and the rock interface will cause the peak vibration velocity to be enlarged, and the stress on the rock mass will also increase.

       

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