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利用非随机交通震源进行面波成像

Surface-wave imaging with nonrandom traffic seismic sources

  • 摘要: 车辆交通产生的高频(>1 Hz)地震噪声可作为城市浅地表结构成像的有效震源。然而,交通震源的时空分布并不是随机的。其时间上非随机性表现在车轮载荷的重复脉冲导致信号自相关,引起互相关函数中产生虚假信号;其空间上非随机性表现在交通源沿道路集中分布(非均匀),不满足传统地震干涉测量中“噪声源随机分布”的假设,造成面波相速度测量偏差。本文从时间和空间两个角度综述解决方案:在时间上,避免对短时地震记录使用“归一化”等预处理手段(可能扭曲波形),采用互相干或反褶积消除震源项影响;在空间上,一方面可以通过稳相区信号筛选或滤波实现可靠的地震干涉测量,另一方面可以通过聚束分析或匹配场处理识别定位主导震源,然后根据实际震源位置进行真实面波相速度测量。本文提出优化的交通震源面波成像流程,结合噪声源定位、稳相区信号分析和互相干技术,实现从超短时长(数十秒)交通噪声中提取可靠的高频面波信号。为城市浅地表结构探测和监测提供绿色、高效、低成本的地震成像方法。

     

    Abstract: Passive surface wave imaging has been a powerful tool for near-surface characterization in urban areas, which extracts surface wave signals from ambient seismic noise and then estimates subsurface shear wave velocity by inversion of the measured phase velocity. The high-frequency (approximately >1 Hz) seismic noise fields in urban environments are dominantly induced by human activities such as the vehicle traffic. Traffic seismic sources are nonrandomly distributed in time and space. Applying standard interferometric techniques to recordings from these nonrandom noise sources makes the Green’s function liable to estimation errors. We analyze the influence of using nonrandom traffic seismic sources for surface wave imaging. With nonrandom traffic seismic sources in time, spurious signals are generated in the cross-correlation function. With nonrandom traffic seismic sources in space, surface-wave phase velocities could be overestimated in the dispersion measurement. We provide an overview of solutions for surface-wave imaging with nonrandom traffic seismic sources in time and space, aiming to improve the retrieval of high-frequency surface waves and achieve reliable results from ultrashort (tens of seconds) observations for near-surface characterization.

     

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