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CO2 Sequestration

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SEAM Update: SEAM CO2 project: Evaluating geophysical methods for characterization of CO2 injections


Reservoir Description: The main reservoir in the ongoing model (onshore pilot) consists of a sequence of stacked turbidites located below a shale caprock. Two reservoirs exist at different depths above the caprock that are potential locations for CO2 which has migrated through the caprock by various mechanisms. A new marine model having a depleted gas reservoir is currently under construction and will involve similar simulations as were done on the onshore pilot model.

Simulations: Reservoir modeling has provided good information about the containment and/or migration of CO2 within the reservoir and through the leakage pathways. This information has led to a refinement of the model to make it more appropriate for participants’ interests.

  • Coupled reservoir flow/geomechanical simulations provide the most realistic model for the distribution of CO2 within the model.
  • Several scenarios have been tested and include one in which CO2 is fully contained within the main reservoir and others where CO2 leaks into the upper siliciclastic reservoirs by passing through the reservoir caprock and along a fault.



Geophysical simulations are being conducted on 4 reservoir models:

  • Model 1: Baseline model prior to injection of CO2.
  • Model 2: A scenario where all CO2 is contained at 30 years after the initiation of injection.
  • Model 3: A scenario where CO2 migrates* above the caprock- simulation at 9 years after the start of injection.
  • Model 4: A scenario where CO2 migrates* above the caprock- simulation at 30 years after the start of injection.


*CO2 migration through the shale caprock into a middle reservoir immediately above the caprock and along a fault that penetrates the reservoir and has continuity up to a shallow reservoir at 500 m where CO2 migrates.

*On the same models as used for 2D seismic

3D migration imaging will be conducted on 3D seismic datasets, 2D imaging will be conducted on the 2D datasets and on the VSP data (approach TBD).
We define 2D seismic to be 3D simulations where sources and receivers all fall along lines passing through one or two wellbores. These data will be processed using 2D imaging algorithms.

4D Controlled-source EM simulations will be conducted on the baseline and at least one monitor model. 4D gravity simulations have been conducted on 3 monitor models.