Illuminating Urban Near-Surface with Distributed Acoustic Sensing Multimodal Noise Surface-Wave Imaging

Yuhang Lei, Baoshan Wang
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Abstract

Urban subsurface exploration requires high spatial and temporal resolution, cost-effective operation, and minimal interference with urban activities. Distributed acoustic sensing (DAS)—an innovative seismic observation tool—emerges as a promising solution for urban surveys. In this study, we repurposed a 7.9 km telecommunication cable traversing Hefei into a seismic observation array with 3850 channels spaced at 2 m intervals. Noise cross-correlation functions (NCFs) were constructed from recordings by iDAS2 and ZD-DAS interrogators along the entire cable. Spatial variation in the NCFs was observed and attributed to different traffic conditions. Employing the recently developed modified frequency–Bessel transform method to NCFs from the 2 km southern subsection of the optic cable, we extracted broadband, high-resolution multimodal dispersion curves. The inverted near-surface structure beneath the cable unveiled a sediment thinning trend from the center to the periphery of the Hefei basin, consistent with borehole inspections. The three-station interferometry (C3) method and beamforming with the Bessel kernel function are applied to mitigate challenges arising from the weak coupling between the cable and the Earth, as well as persistent localized noise sources. These techniques facilitated the acquisition of broadband surface waves. Distinct secondary scatters are observed in NCFs near channels 2090 and 2287, accompanied by a substantial velocity contrast of 30%–40%, suggesting the existence of a blind fault. The study reaffirms the significant potential of DAS arrays for high-resolution imaging of subsurface structures in challenging urban environments, emphasizing the importance of advanced processing techniques to enhance imaging accuracy and robustness.
利用分布式声学传感多模态噪声面波成像技术照亮城市近地表
城市地下勘探需要高空间和时间分辨率、经济高效的操作以及对城市活动的最小干扰。分布式声学传感(DAS)--一种创新的地震观测工具--成为城市勘测的一种有前途的解决方案。在这项研究中,我们将横穿合肥的一条 7.9 公里长的电信电缆改造成了一个地震观测阵列,其中有 3850 个间隔为 2 米的道。根据 iDAS2 和 ZD-DAS 询问器在整条电缆上的记录构建了噪声交叉相关函数(NCF)。观察到 NCF 的空间变化,并将其归因于不同的交通状况。我们对光缆南部 2 公里分段的 NCF 采用了最近开发的修正频率-贝塞尔变换方法,提取了宽带、高分辨率的多模态频散曲线。光缆下方的反演近地表结构揭示了合肥盆地沉积物从中心向外围变薄的趋势,这与钻孔检测结果一致。三站干涉测量(C3)方法和贝塞尔核函数波束成形技术的应用减轻了电缆与地球之间的弱耦合以及持续局部噪声源带来的挑战。这些技术有助于获取宽带表面波。在通道 2090 和 2287 附近的 NCF 中观测到了明显的二次散射,并伴有 30%-40% 的巨大速度对比,表明存在盲断层。这项研究再次证实了 DAS 阵列在具有挑战性的城市环境中对地下结构进行高分辨率成像的巨大潜力,同时强调了先进处理技术对提高成像精度和稳健性的重要性。
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