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Time-lapse 4D seismic imaging has become one of the most reliable technologies to monitor the areal extent and dynamic behavior of CO2 plumes during and after injection. When combined with pressure and temperature data from monitoring wells, 4D seismic surveys can provide high-resolution insight into CO2 distribution and migration patterns. However, applying 4D seismic monitoring to depleted hydrocarbon reservoirs which are often considered attractive CO2 storage candidates due to their well-characterized geology and existing infrastructure poses unique challenges.
The study concluded that CO2 exhibits complex acoustic behavior under pressure, with its velocity initially decreasing and then increasing beyond ∼2000 psi, affecting seismic detectability due to changes in acoustic impedance. Pressure depletion from historical gas production increases seismic velocities by compressing the rock matrix, while CO2 injection reduces effective stress and lowers velocities, enabling time-lapse seismic monitoring. Residual hydrocarbons mixed with CO2 form a denser, slower fluid phase, enhancing 4D seismic contrast. Aquifer support plays a critical role in conformance monitoring, with active aquifers amplifying acoustic changes and improving plume tracking. Synthetic seismic modeling confirms that CO2 injection causes significant amplitude variations, driven by pore pressure and saturation changes, aiding subsurface interpretation.