Well Control Strategies for Effective CO2 Subsurface Storage: Optimization and Policies †
Abstract
:1. Introduction
2. Key Subsurface Policies in CO2 Geological Storage: Outline and Application
2.1. Pressure Management: Controlling Pressure Build-Up and Geomechanical Complications
- (1)
- Closed systems are characterized by impervious boundaries surrounding the storage formation and vertical obstruction by impermeable sealing units. These systems lack pressure bleed-off mechanisms and therefore experience a more significant impact from pressure build-up. While closed systems mitigate the risk of brine leakage during CO2 injection, it is essential to maintain pressure below the maximum threshold tolerated by the formation. This is necessary to ensure the mechanical integrity of the storage site, preventing failures in the caprock and reactivation of fractures and faults.
- (2)
- Semi-closed systems have lateral impervious boundaries and are partially sealed above and/or below by semi-permeable sealing units. These systems can effectively reduce reservoir pressurization through pressure bleed-off mechanisms. For example, brine migration into semi-sealing units and lateral displacement of brine help mitigate pressure. However, elevated pressure levels in semi-closed systems may result in brine displacement into freshwater aquifers through leaky faults and wells, posing environmental risks.
- (3)
- Open systems have lateral boundaries located at such a distance that they remain unaffected by pressure disturbances. They naturally experience less pressure build-up compared to closed and semi-closed systems [19].
2.2. Geological Storage Security: Improving Residual and Solubility Trapping
- (1)
- Residual gas trapping: encountered when formation water encroaches or invades the CO2 plume, leaving a portion of the CO2 trapped as residual gas within the pore spaces of the rock formation.
- (2)
- Solubility trapping: Achieved when CO2 partially dissolves into the aqueous phase present in the formation, leading to solubility trapping. This dissolved CO2 is unlikely to leave the solution unless there is a significant decrease in pressure.
- (3)
- Mineral trapping: Anticipated when CO2 reacts with native minerals in the rock formation, resulting in the precipitation of carbonate minerals. This process helps to immobilize CO2 in a more secure manner.
3. The Optimization of Well Control Strategies for Effective CO2 Sequestration in Saline Aquifers
4. Conclusions
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Conflicts of Interest
References
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Ismail, I.; Gaganis, V. Well Control Strategies for Effective CO2 Subsurface Storage: Optimization and Policies. Mater. Proc. 2023, 15, 74. https://doi.org/10.3390/materproc2023015074
Ismail I, Gaganis V. Well Control Strategies for Effective CO2 Subsurface Storage: Optimization and Policies. Materials Proceedings. 2023; 15(1):74. https://doi.org/10.3390/materproc2023015074
Chicago/Turabian StyleIsmail, Ismail, and Vassilis Gaganis. 2023. "Well Control Strategies for Effective CO2 Subsurface Storage: Optimization and Policies" Materials Proceedings 15, no. 1: 74. https://doi.org/10.3390/materproc2023015074
APA StyleIsmail, I., & Gaganis, V. (2023). Well Control Strategies for Effective CO2 Subsurface Storage: Optimization and Policies. Materials Proceedings, 15(1), 74. https://doi.org/10.3390/materproc2023015074