TY - JOUR
T1 - A fast wavefield reconstruction inversion solution in the frequency domain
AU - Lin, Yuzhao
AU - Van Leeuwen, Tristan
AU - Liu, Huaishan
AU - Sun, Jian
AU - Xing, Lei
N1 - Funding Information:
This work was supported by the fellowship of the China Postdoctoral Science Foundation under grant 2022M722970 and Shandong Provincial Nature Science Foundation under grant ZR2022QD036, in part by the National Natural Science Foundation of China under grant 91958206, the National Natural Science Foundation of China under grant 42276055, and the Fundamental Research Funds for the Central Universities under grant 202262008. Several colleagues have helped with suggestions for the improvement of this paper, and we would particularly like to thank the editor, associate editor A. Baumstein, reviewer G. Rizzuti, and other two anonymous reviewers for their constructive comments and suggestions.
Publisher Copyright:
© 2023 Society of Exploration Geophysicists.
PY - 2023/5/1
Y1 - 2023/5/1
N2 - Full-waveform inversion (FWI) aims at estimating subsurface physical parameters by minimizing the misfit between simulated data and observations. FWI relies heavily on an accurate initial model and is less robust to measurement noise and physical assumptions in modeling. Compared with FWI, wavefield reconstruction inversion (WRI) is more robust to these uncertainties but faces high computational costs. To overcome these challenges, we have developed a new form of WRI. This reformulation takes the form of a traditional FWI formula, which includes a medium-dependent weight function, and can be easily incorporated into the current FWI workflow. This weight function contains the covariance matrices to characterize the distribution of uncertainties in measurements and physical assumptions. We discuss various options of the theoretical covariance matrix of the new inversion method and find how they relate to various well-known approaches, including FWI, WRI, and extended FWI. On the basis of the preceding comparison, we develop a theoretical covariance matrix definition based on the source. Numerical experiments demonstrate that our method with a source-dependent theoretical covariance matrix is more computationally efficient than conventional WRI while preserving a certain degree of robustness.
AB - Full-waveform inversion (FWI) aims at estimating subsurface physical parameters by minimizing the misfit between simulated data and observations. FWI relies heavily on an accurate initial model and is less robust to measurement noise and physical assumptions in modeling. Compared with FWI, wavefield reconstruction inversion (WRI) is more robust to these uncertainties but faces high computational costs. To overcome these challenges, we have developed a new form of WRI. This reformulation takes the form of a traditional FWI formula, which includes a medium-dependent weight function, and can be easily incorporated into the current FWI workflow. This weight function contains the covariance matrices to characterize the distribution of uncertainties in measurements and physical assumptions. We discuss various options of the theoretical covariance matrix of the new inversion method and find how they relate to various well-known approaches, including FWI, WRI, and extended FWI. On the basis of the preceding comparison, we develop a theoretical covariance matrix definition based on the source. Numerical experiments demonstrate that our method with a source-dependent theoretical covariance matrix is more computationally efficient than conventional WRI while preserving a certain degree of robustness.
KW - algorithm
KW - frequency domain
KW - full-waveform inversion
UR - http://www.scopus.com/inward/record.url?scp=85153388554&partnerID=8YFLogxK
U2 - 10.1190/geo2022-0023.1
DO - 10.1190/geo2022-0023.1
M3 - Article
AN - SCOPUS:85153388554
SN - 0016-8033
VL - 88
SP - R257-R267
JO - Geophysics
JF - Geophysics
IS - 3
ER -