Efficient Acoustic Reverse Time Migration With an Attenuated and Reversible Random Boundary

Pre-stack reverse time migration (RTM) based on the two-way wave equation has been proved to be the most accurate seismic migration method theoretically. However, it requires reverse-order access to the wavefield calculated in forward time. In recursion computing, such out-of-order access requires t...

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Main Authors: Qingqing Li, Li-Yun Fu, Ru-Shan Wu, Qizhen Du
Format: Article
Language:English
Published: IEEE 2020-01-01
Series:IEEE Access
Subjects:
Online Access:https://ieeexplore.ieee.org/document/9001069/
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author Qingqing Li
Li-Yun Fu
Ru-Shan Wu
Qizhen Du
author_facet Qingqing Li
Li-Yun Fu
Ru-Shan Wu
Qizhen Du
author_sort Qingqing Li
collection DOAJ
description Pre-stack reverse time migration (RTM) based on the two-way wave equation has been proved to be the most accurate seismic migration method theoretically. However, it requires reverse-order access to the wavefield calculated in forward time. In recursion computing, such out-of-order access requires that most of the recursion history should be stored on the hard disk. For massive amounts of seismic data, loading the saved wavefield data from the disk during imaging has been the bottleneck of RTM, restricting its wide application. To solve this problem, the wavefield in forward time must be reconstructed in reverse order. Although the random boundary can avoid the disk requirement by creating random velocity around the computational domain when propagate the source function. However, the random wavefield reflected from the boundary can generate unwanted artifacts in the final images. In this paper, we develop an attenuated and reversible random boundary condition which is implemented by mixing the reversible attenuation and random boundary conditions. Similar to the random boundary scheme, the proposed method just needs to save the last one or two wavefield snapshots into the memory in forward process. It then reconstructs the source wavefield in reverse order, while greatly reduces the disk input and output (I/O) requirements. Taking the attenuated property into consideration, the artificial events reflected from the boundary can be eliminated. Thus, our method can improve the imaging quality largely compared with the random boundary scheme. Numerical results demonstrate that the RTM images with our proposed attenuated and reversible random boundary condition can not only eliminate the unwanted artifacts, but also improve the computational efficiency greatly.
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spelling doaj.art-48089021d06f492c8d0638040beeb2632022-12-21T23:26:23ZengIEEEIEEE Access2169-35362020-01-018345983461010.1109/ACCESS.2020.29748629001069Efficient Acoustic Reverse Time Migration With an Attenuated and Reversible Random BoundaryQingqing Li0https://orcid.org/0000-0003-1600-8632Li-Yun Fu1Ru-Shan Wu2Qizhen Du3School of Geosciences, China University of Petroleum (East China), Qingdao, ChinaSchool of Geosciences, China University of Petroleum (East China), Qingdao, ChinaDepartment of Earth and Planetary Sciences, Modeling and Imaging Laboratory, University of California at Santa Cruz, Santa Cruz, CA, USASchool of Geosciences, China University of Petroleum (East China), Qingdao, ChinaPre-stack reverse time migration (RTM) based on the two-way wave equation has been proved to be the most accurate seismic migration method theoretically. However, it requires reverse-order access to the wavefield calculated in forward time. In recursion computing, such out-of-order access requires that most of the recursion history should be stored on the hard disk. For massive amounts of seismic data, loading the saved wavefield data from the disk during imaging has been the bottleneck of RTM, restricting its wide application. To solve this problem, the wavefield in forward time must be reconstructed in reverse order. Although the random boundary can avoid the disk requirement by creating random velocity around the computational domain when propagate the source function. However, the random wavefield reflected from the boundary can generate unwanted artifacts in the final images. In this paper, we develop an attenuated and reversible random boundary condition which is implemented by mixing the reversible attenuation and random boundary conditions. Similar to the random boundary scheme, the proposed method just needs to save the last one or two wavefield snapshots into the memory in forward process. It then reconstructs the source wavefield in reverse order, while greatly reduces the disk input and output (I/O) requirements. Taking the attenuated property into consideration, the artificial events reflected from the boundary can be eliminated. Thus, our method can improve the imaging quality largely compared with the random boundary scheme. Numerical results demonstrate that the RTM images with our proposed attenuated and reversible random boundary condition can not only eliminate the unwanted artifacts, but also improve the computational efficiency greatly.https://ieeexplore.ieee.org/document/9001069/Computational efficiencyreverse time migrationattenuationrandom boundary condition
spellingShingle Qingqing Li
Li-Yun Fu
Ru-Shan Wu
Qizhen Du
Efficient Acoustic Reverse Time Migration With an Attenuated and Reversible Random Boundary
IEEE Access
Computational efficiency
reverse time migration
attenuation
random boundary condition
title Efficient Acoustic Reverse Time Migration With an Attenuated and Reversible Random Boundary
title_full Efficient Acoustic Reverse Time Migration With an Attenuated and Reversible Random Boundary
title_fullStr Efficient Acoustic Reverse Time Migration With an Attenuated and Reversible Random Boundary
title_full_unstemmed Efficient Acoustic Reverse Time Migration With an Attenuated and Reversible Random Boundary
title_short Efficient Acoustic Reverse Time Migration With an Attenuated and Reversible Random Boundary
title_sort efficient acoustic reverse time migration with an attenuated and reversible random boundary
topic Computational efficiency
reverse time migration
attenuation
random boundary condition
url https://ieeexplore.ieee.org/document/9001069/
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AT liyunfu efficientacousticreversetimemigrationwithanattenuatedandreversiblerandomboundary
AT rushanwu efficientacousticreversetimemigrationwithanattenuatedandreversiblerandomboundary
AT qizhendu efficientacousticreversetimemigrationwithanattenuatedandreversiblerandomboundary