Effective seismic force retrieval from surface measurement for SH-wave reconstruction

被引:3
作者
Guidio, Bruno [1 ]
Goh, Heedong [2 ,3 ]
Jeong, Chanseok [1 ,4 ]
机构
[1] Cent Michigan Univ, Sch Engn & Technol, Mt Pleasant, MI 48859 USA
[2] Univ Texas Austin, Chandra Dept Elect & Comp Engn, Austin, TX 78712 USA
[3] CUNY, Adv Sci Res Ctr, Photon Initiat, New York, NY 10031 USA
[4] Cent Michigan Univ, Earth & Ecosyst Sci Program, Mt Pleasant, MI 48859 USA
基金
美国国家科学基金会;
关键词
Passive-seismic inversion; Domain reduction method (DRM); Effective seismic force vector; Discretize-then-optimize (DTO) approach; Reconstruction of seismic responses; Full-waveform inversion; DOMAIN REDUCTION METHOD; MULTICHANNEL ANALYSIS; LOCALIZED REGIONS; INVERSION; VELOCITY; DECONVOLUTION; AMPLIFICATION; MOTIONS; SITES;
D O I
10.1016/j.soildyn.2022.107682
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
We present a new method to obtain dynamic body force at virtual interfaces to reconstruct shear wave motions induced by a source outside a truncated computational domain. Specifically, a partial differential equation (PDE)-constrained optimization method is used to minimize the misfit between measured motions at a limited number of sensors on the ground surface and their counterparts reconstructed from optimized forces. Numerical results show that the optimized forces accurately reconstruct the targeted ground motions in the surface and the interior of the domain. The proposed optimization framework yields a particular force vector among other valid solutions allowed by the domain reduction method (DRM). Per this optimized or inverted force vector, the reconstructed wave field is identical to its reference counterpart in the domain of interest but may differ in the exterior domain from the reference one. However, we remark that the inverted solution is valid and introduce a simple post-process that can modify the solution to achieve an alternative force vector corresponding to the reference wave field. We also study the desired sensor spacing to accurately reconstruct the wave responses for a given dominant frequency of interest. We remark that the presented method is omnidirectionally applicable in terms of the incident angle of an incoming wave and is effective for any given material heterogeneity and geometry of layering of a reduced domain. The presented inversion method requires information on the wave speeds and dimensions of only a reduced domain. Namely, it does not need any information on the geophysical profile of an enlarged domain or a seismic source profile outside a reduced domain. Thus, the computational cost of the method is compact even though it leads to the highfidelity reconstruction of wave response in the reduced domain, allowing for studying and predicting ground and structural responses using real seismic measurements.
引用
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页数:20
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