Propagation and Attenuation Characteristics of Blast-induced Stress Waves in Layered Soft Rock

  • 摘要: 为探究水平层状软岩地层中节理对爆破应力波传播与衰减特性的影响,依托成自高速铁路长征隧道工程,采用LS-DYNA数值模拟方法,分析研究不同节理厚度与间距条件下节理岩体模型中爆破应力波传播规律、振动衰减及能量耗散特性,明确节理几何特性对振动衰减分区的影响,并结合现场监测验证数值模拟方法的可靠性。研究结果表明,节理厚度和间距显著影响应力波的能量耗散与衰减特性,当节理厚度超过0.4倍装药半径时,振速衰减幅值趋于稳定;随着节理厚度的增加,应力波反射能量逐渐增强,透射能量显著减少,且反射与透射能量的变化趋势趋于稳定;多层节理条件下,振动合速度峰值随节理间距增大而减小,且其衰减速率呈规律性变化;基于振速衰减分区研究,提出节理岩体爆破控制的影响分区标准;现场监测获得的爆破引起的地表质点振动速度与数值模拟结果具有一致性。

     

    Abstract: To investigate the influence of joints in horizontally stratified soft rock formations on the propagation and attenuation characteristics of blast-induced stress waves, this study employs LS-DYNA numerical simulations based on the Changzheng Tunnel on the Chengdu-Zigong high-speed railway. The research systematically analyzes the propagation patterns, vibration attenuation, and energy dissipation characteristics of stress waves in jointed rock masses under varying joint thicknesses and spacings, elucidating the impact of joint geometric characteristics on vibration attenuation zoning. Field monitoring data further validate the reliability of the numerical approach. Key findings reveal that joint thickness and spacing significantly govern stress wave energy dissipation and attenuation. When the joint thickness exceeds 0.4 times the charge radius, the amplitude of vibration velocity attenuation stabilizes. Increased joint thickness enhances stress wave reflection energy while markedly reducing transmitted energy,with both trends reaching equilibrium beyond critical thresholds. Under multi-joint conditions, the peak resultant vibration velocity decreases with larger joint spacings, exhibiting predictable decay rates. Based on vibration attenuation zoning, a new classification standard for blast control in jointed rock masses is proposed. Field-measured surface particle vibration velocities demonstrate strong agreement with numerical results.

     

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