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Interpretaion of synthetic seismic time-lapse monitoring data for Korea CCS project based on the

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dc.contributor.author오주원-
dc.contributor.author민동주-
dc.contributor.author김원기-
dc.contributor.author허철-
dc.contributor.author강성길-
dc.date.accessioned2021-12-08T17:41:08Z-
dc.date.available2021-12-08T17:41:08Z-
dc.date.issued20120920-
dc.identifier.urihttps://www.kriso.re.kr/sciwatch/handle/2021.sw.kriso/5189-
dc.description.abstractRecently, the CCS (Carbon Capture and Storage) is one of the promising methods to reduce the CO2 emission. To evaluate the success of the CCS project, various geophysical monitoring techniques have been applied. Among them, the time-lapse seismic monitoring is one of the effective methods to investigate the migration of CO2 plume. To monitor the injected CO2 plume accurately, it is needed to interpret seismic monitoring data using not only the imaging technique but also the full waveform inversion, because subsurface material properties can be estimated through the inversion. However, previous works for interpreting seismic monitoring data are mainly based on the imaging technique. In this study, we perform the frequency-domain full waveform inversion for synthetic data obtained by the acoustic-elastic coupled modeling for the geological model made after Ulleung Basin, which is one of the CO2 storage prospects in Korea. We suppose the injection layer is located in fault-related anticlines in the Dolgorae Deformed Belt and, for more realistic situation, we contaminate the synthetic monitoring data with random noise and outliers. We perform the time-lapse full waveform inversion in two scenarios. One scenario is that the injected CO2 plume migrates within the injection layer and is stably captured. The other scenario is that the injected CO2 plume leaks through the weak part of the cap rock. seismic monitoring is one of the effective methods to investigate the migration of CO2 plume. To monitor the injected CO2 plume accurately, it is needed to interpret seismic monitoring data using not only the imaging technique but also the full waveform inversion, because subsurface material properties can be estimated through the inversion. However, previous works for interpreting seismic monitoring data are mainly based on the imaging technique. In this study, we perform the frequency-domain full waveform inversion for synthetic data obtained-
dc.language영어-
dc.language.isoENG-
dc.titleInterpretaion of synthetic seismic time-lapse monitoring data for Korea CCS project based on the-
dc.title.alternativeInterpretaion of synthetic seismic time-lapse monitoring data for Korea CCS project based on the-
dc.typeConference-
dc.citation.titleAmerican Geophysical Union’s 45th annual Fall Meeting-
dc.citation.volume1-
dc.citation.number1-
dc.citation.startPage1-
dc.citation.endPage1-
dc.citation.conferenceNameAmerican Geophysical Union’s 45th annual Fall Meeting-
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Kang, Seong-Gil
연구전략본부 (국제해사기술센터)
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