Modeling CO2 vertical migration based on seismic frequency-dependent AVO responses. (8th March 2016)

• Record Type: Journal Article
• Authors: Li, Bonan; Liu, Cai; Lu, Qi; Pang, Shuo
• Is Part Of: Journal of geophysics and engineering. Volume 13:Number 2(2016:Apr.)
• Page Start: 164
• Page End: 171
• Publication Date: 2016-03-08
• Subjects: CO2 migration -- time-lapse seismic monitoring -- frequency-dependent AVO inversion -- time-frequency analysis; Geophysics -- Periodicals; Prospecting -- Geophysical methods -- Periodicals; Engineering -- Periodicals; 622.1505
• DOI: 10.1088/1742-2132/13/2/164
• Languages: English
• ISSNs: 1742-2132

Abstract

Abstract: Injection of CO2 into a geological subsurface will cause seismic dispersion and attenuation, which will change with the migration of the CO2 plume. Therefore, temporal attenuation changes from the seismic section with the CO2 plume can provide additional information about CO2 storage, migration, and possible leakage. The frequency-dependent amplitude variation with offset (FDAVO) attribute, as a seismic characteristic, which quantifies frequency-dependent anomalies from various kinds of sources, is widely applied in fields of hydrocarbon indication and fluid identification. In this work we aim to investigate the potential of the FDAVO attribute as a monitoring tool during the process of CO2 migration. We combine the Buckley–Leverett equation and the patchy-saturation model to simulate the substitution process. We then apply a novel tool, the FDAVO inversion method, to estimate the dispersion level at the target interface. What is more, the characteristic of the frequency-dependent attribute versus time is studied for the first time. The result of the numerical simulation reveals that: (1) caused by CO2 injection, there is significant dispersion and attenuation within the seismic band; (2) the level of dispersion reflects the migration of CO2 plume; (3) dispersion anomalies are well quantified by the inverted FDAVO attributes, which can be utilized to characterize the vertical distribution of the CO2 plume.