Three-Dimensional Urban Subsurface Space Tomography with Dense Ambient Noise Seismic Array

IF 4.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Ruizhe Sun, Jing Li, Yingwei Yan, Hui Liu, Lige Bai, Yuqing Chen
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Abstract

Two-dimensional dense seismic ambient noise array techniques have been widely used to image and monitor subsurface structure characterization in complex urban environments. It does not have limitations in the layout under the limitation of urban space, which is more suitable for 3D S-velocity imaging. In traditional ambient seismic noise tomography, the narrowband filtering (NBF) method has many possible dispersion branches. Aliases would appear in the dispersive image, and the dispersion curve inversion also depends on the initial model. To obtain high-accuracy 3D S-velocity imaging in urban seismology, we developed a robust workflow of data processing and S-velocity tomography for 2D dense ambient noise arrays. Firstly, differing from the NBF method, we adopt the continuous wavelet transform (CWT) as an alternative method to measure the phase velocity from the interstation noise cross-correlation function (NCF) without 2π ambiguity. Then, we proposed the sequential dispersion curve inversion (DCI) strategy, which combines the Dix linear inversion and preconditioned fast descent (PFD) method to invert the S-velocity structure without prior information. Finally, the 3D S-velocity model is generated by the 3D spatial interpolation. The proposed workflow is applied to the 2D dense ambient seismic array dataset in Changchun City. The quality evaluation methods include residual iteration error, horizontal-to-vertical spectral ratio (HVSR) map, and electrical resistivity tomography (ERT). All tests indicate that the developed workflow provides a reliable 3D S-velocity model, which offers a reference for urban subsurface space exploration.

Abstract Image

利用密集环境噪声地震阵列进行三维城市地下空间断层扫描
二维密集地震环境噪声阵列技术已被广泛应用于复杂城市环境下的地下结构特征成像和监测。二维密集地震环境噪声阵列技术在复杂的城市环境中被广泛应用,它不受城市空间布局的限制,更适用于三维 S-速度成像。在传统的环境地震噪声层析成像中,窄带滤波(NBF)方法有许多可能的频散分支。在频散图像中会出现别名,频散曲线反演也取决于初始模型。为了在城市地震学中获得高精度的三维 S-速度成像,我们为二维密集环境噪声阵列开发了一套强大的数据处理和 S-速度层析成像工作流程。首先,有别于 NBF 方法,我们采用连续小波变换(CWT)作为替代方法,从站间噪声交叉相关函数(NCF)中测量相位速度,且无 2π 模糊性。然后,我们提出了序列频散曲线反演(DCI)策略,该策略结合了 Dix 线性反演和预处理快速下降(PFD)方法,在没有先验信息的情况下反演 S-速度结构。最后,通过三维空间插值生成三维 S-速度模型。提出的工作流程应用于长春市的二维密集环境地震阵列数据集。质量评估方法包括残余迭代误差、水平垂直谱比(HVSR)图和电阻率层析(ERT)。所有测试表明,开发的工作流程提供了可靠的三维 S-速度模型,为城市地下空间探测提供了参考。
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来源期刊
Surveys in Geophysics
Surveys in Geophysics 地学-地球化学与地球物理
CiteScore
10.00
自引率
10.90%
发文量
64
审稿时长
4.5 months
期刊介绍: Surveys in Geophysics publishes refereed review articles on the physical, chemical and biological processes occurring within the Earth, on its surface, in its atmosphere and in the near-Earth space environment, including relations with other bodies in the solar system. Observations, their interpretation, theory and modelling are covered in papers dealing with any of the Earth and space sciences.
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