Abstract
In this study, we explore the use of different wavefields recorded in VSP surveys to conduct time-lapse seismic monitoring of CO2 migration in the subsurface. To do so, we perform a series of VSP experiments employing a surface source and an array of borehole hydrophones to establish correlations between the recorded wavefields (e.g., direct, reflected, and guided waves) and the presence of heterogeneities in the formation surrounding the borehole, which may be affected by the presence of CO2. We analyze changes in seismic signals acquired before and during a CO2 injection experiment at the Svelvik CO2 Field Laboratory, focusing on typical VSP attributes used for seismic characterization (e.g., arrival time shifts and amplitude decay of direct waves) and less common wave types (e.g., tube waves) that may provide additional insights into CO2 presence near the borehole.