Idris Bukar, Rebecca E. Bell, Ann Muggeridge, Sam Krevor

Large scale geological storage of CO₂ is being deployed worldwide to reduce greenhouse gas emissions to the atmosphere. Previous modelling studies have investigated the potential for CO₂ migration along faults. We observe such migration at a commercial-scale, demonstration CO₂ storage project, including subsequent emergence of the CO₂ into overlying permeable layers. Previous attempts at interpreting the time-lapse seismic data using amplitude attributes were hindered by noise from the limited survey repeatability combined with a weak signal due to the stiffness of the rock. Here we apply an alternative interpretation of the seismic data using time shift attributes, resulting in clear plume anomalies. In addition to migrating up the fault, we observe the plume diverted by the start of injection at a neighboring project. This work provides field observations of theorized plume behaviors and demonstrates an approach to overcome challenges in interpreting seismic monitoring data for geological CO₂ storage.