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穿越赋水断层隧道地震动力响应振动台模型试验研究

Shaking table model test study on seismic dynamic response of tunnels crossing water-bearing faults

  • 摘要: 为研究穿越赋水断层隧道围岩动力响应特征,以我国西南高烈度地震区某穿越断层破碎带隧道工程为例,开展大型振动台模型试验研究。通过从时域、频域及时频域多维度综合分析赋水断层隧道地震动力响应规律,结合隧道应变演化特征与破坏现象,揭示赋水断层隧道地震破坏机理。结果表明:0.2g地震作用下,赋水断层会显著影响隧道各监测断面的加速度响应,且完整围岩区域隧道动力放大效应平均增幅大于赋水断层段。断层注水后Fourier谱分析显示隧道各断面拱顶、拱腰、拱底的振幅变化趋势基本一致,而高频段振幅均有不同程度增幅;HHT时频分析表明断层注水后,隧道频谱特征由注水前的单峰值分布转变为多峰值分布。断层注水后隧道不同部位的受力状态发生明显改变;赋水断层段隧道裂缝发育更为严重,主要集中于拱顶、拱腰及拱底两侧部位,而完整围岩段隧道破坏则集中于拱底与拱腰区域。以上研究有助于为跨赋水断层隧道实际工程确定合理的抗震设防设计方案,对认识跨赋水断层隧道的地震动力响应特征具有重要意义。

     

    Abstract: To investigate the dynamic response characteristics of surrounding rock in tunnels crossing water-bearing faults, a large-scale shaking table model test was conducted. A tunnel project crossing a fault fracture zone in a high-seismic-intensity area of Southwest China was taken as the research object. By comprehensively analyzing the seismic dynamic response of water-bearing fault tunnels from multiple dimensions, including the time domain, frequency domain, and time-frequency domain, and by combining the strain evolution characteristics and failure phenomena of the tunnel, the seismic failure mechanism of water-bearing fault tunnels was revealed. The results show that under a 0.2g earthquake, the water-bearing fault significantly influences the acceleration response of each monitored tunnel section, The average increase of the dynamic amplification effect of in the intact surrounding rock area is greater than that in the water-bearing fault section. Fourier spectrum analysis after fault water injection indicates that the amplitude variation trends of the vault, arch waist, and arch bottom of each tunnel section are basically consistent, while the amplitudes in the high-frequency band all increase to varying degrees. HHT time-frequency analysis shows that after fault water injection, the overall amplitude of the tunnel response is significantly reduced, and the spectral characteristics change from a single-peak distribution before water injection to a multi-peak distribution. After fault water injection, the stress state of different parts of the tunnel changes significantly; the crack development in the tunnel section passing through the water-bearing fault is more severe, mainly concentrated in the vault, arch waist, and arch bottom, while the damage of the tunnel in the intact surrounding rock section is concentrated on both sides of the arch bottom and the arch waist area. This research contributes to determining a rational seismic fortification design for practical engineering of tunnels crossing water-bearing faults and is of great significance for understanding the seismic dynamic response characteristics of such tunnels.

     

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