三维地震波超前地质预报及其应用效果

3D advanced geological prediction based on reflected seismic waves and its application effects

  • 摘要:
    目的 针对传统隧道地震反射波超前地质预报技术受限于二维观测系统几何局限导致的异常体空间定位偏差问题,建立基于实际隧道几何结构的三维地震波超前预报方法。
    方法 采用“理论分析–数值模拟–工程验证”技术路径,解决了三维探测系统的波场重构、空间建模、偏移成像等关键技术难题。基于几何地震学原理论证了三维观测对异常体探测范围及定位精度的提升效应;应用旋转交错网格有限差分法实现了隧道全空间TTI介质三维波场正演,引入通量校正传输技术(FCT)抑制数值频散;结合快速行进法(fast marching method,FMM)计算波前走时,采用改进型Kirchhoff积分算法实现了三维偏移成像。
    结果 鄂西铁路隧道现场试验表明:三维方法在掌子面前方20 m(里程412 m)处精准探测到密集裂隙发育带;异常体定位范围较二维预报方法缩小20%;三维预报成果图可多角度展示异常体空间形态。
    结论 三维地震反射波超前地质预报技术提升了地质异常体的空间定位能力与解释直观性,为隧道施工地质灾害防控提供有效技术支撑。

     

    Abstract:
    Objective For the advance geological prediction of tunnels based on reflected seismic waves, the traditional 2D observation method tends to cause spatial positioning deviations of anomalies. To overcome this limitation, this study developed a 3D seismic wave-based advance geological prediction method according to the actual geometries of tunnels.
    Methods Using the technical path consisting of theoretical analysis, numerical simulation, and engineering verification, this study solved key technical challenges including 3D wavefield reconstruction, spatial modeling, and migration imaging in the 3D detection system. Based on the principle of geometric seismology, this study demonstrated the enhancement effects of 3D observation on the detection range and positioning accuracy of anomalies. Then, using the rotated staggered-grid finite-difference (RSFD) method, this study achieved the 3D wavefield forward modeling for tilted transversely isotropic (TTI) media in the full tunnel space, with flux-corrected transport (FCT) technology introduced to suppress numerical dispersion. In combination with the calculation of wavefront traveltimes using the fast marching method (FMM), this study achieved 3D migration imaging using the improved Kirchhoff integral theorem.
    Results Field tests in a railway tunnel in western Hubei Province indicate that the 3D advance geological prediction method detected a zone with dense fractures 20 m ahead of the tunnel face (at chainage 412). The anomaly body range detected using the 3D advance geological prediction method decreased by 20% compared to that determined using the 2D method. The result maps of the 3D advance geological prediction allowed for the presentation of the spatial morphology of the anomaly body from multiple perspectives.
    Conclusion The 3D advance geological prediction technology based on reflected seismic waves can enhance the spatial positioning capability and interpretation intuitiveness of geological anomalies, providing effective technical support for preventing and controlling geological hazards during tunnel construction.

     

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