4.7 Article

Acoustic waveform inversion in frequency domain: Application to a tunnel environment

Journal

UNDERGROUND SPACE
Volume 6, Issue 5, Pages 560-576

Publisher

KEAI PUBLISHING LTD
DOI: 10.1016/j.undsp.2021.01.001

Keywords

Wave propagation; Acoustics; Perfectly matched layers; Full waveform inversion; Seismic imaging; Tunneling; Absorbing boundaries

Funding

  1. German Research Foundation (DFG) within the Collaborative Research Center [SFB 837]

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Waveform inversion is utilized to determine an optimal model for the velocity field of a ground structure by establishing a realistic forward computer model using a suitable numerical approach and solving the forward problem in the frequency domain with higher-order finite elements. The velocity field is inverted over specific frequencies to reduce computational costs and the nonlinearity of the inverse problem. Results are presented for different frequency sets, source and receiver locations in a two-dimensional model, and attenuation effects are also investigated, along with blind tests on unknown synthetic models to simulate realistic scenarios. Finally, the inversion results in a three-dimensional space are illustrated.
Waveform inversion is an approach used to find an optimal model for the velocity field of a ground structure such that the dynamic response is close enough to the given seismic data. First, a suitable numerical approach is employed to establish a realistic forward computer model. The forward problem is solved in the frequency domain using higher-order finite elements. The velocity field is inverted over a specific number of discrete frequencies, thereby reducing the computational cost of the forward calculation and the nonlinearity of the inverse problem. The results are presented for different frequency sets and with different source and receiver locations for a two-dimensional model. The influence of attenuation effects is also investigated. The results of two blind tests are presented where only the seismic records of an unknown synthetic model with an inhomogeneous material parameter distribution are provided to mimic a more realistic case. Finally, the result of the inversion in a three-dimensional space is illustrated.

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