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Two-Phase Flow Mechanisms Controlling CO2 Intrusion into Shaly Caprock
Abstract Geologic carbon storage in deep saline aquifers has emerged as a promising technique to mitigate climate change. CO 2 is buoyant at the storage conditions and tends to float over the resident brine jeopardizing long-term containment goals. Therefore, the caprock sealing capacity is of great importance and requires detailed assessment. We perform supercritical CO 2 injection experiments on shaly caprock samples (intact caprock and fault zone) under representative subsurface conditions. We numerically simulate the experiments, satisfactorily reproducing the observed evolution trends. Simulation results highlight the dynamics of CO 2 flow through the specimens with implications to CO 2 leakage risk assessment in field practices. The large injection-induced overpressure drives CO 2 in free phase into the caprock specimens. However, the relative permeability increase following the drainage path is insufficient to provoke an effective advancement of the free-phase CO 2 . As a result, the bulk CO 2 front becomes almost immobile. This implies that the caprock sealing capacity is unlikely to be compromised by a rapid capillary breakthrough and the injected CO 2 does not penetrate deep into the caprock. In the long term, the intrinsically slow molecular diffusion appears to dominate the migration of CO 2 dissolved into brine. Nonetheless, the inherently tortuous nature of shaly caprock further holds back the diffusive flow, favoring safe underground storage of CO 2 over geological time scales.
Effect of CO2 Injection on the Multiphase Flow Properties of Reservoir Rock
Not provided.
CO2-Utilization Facilitated by Solid Reaction Mediums—A Review
Abstract This short review examines solid reaction mediums—specifically oxygen, CO 2 , and carbon carriers—within the framework of Chemical Looping (CL) to illuminate various CO 2 utilization pathways. The thermodynamic consideration for carrier selection is first discussed. This is followed by a summary of the key carrier types investigated to date, with an emphasis on elucidating the roles of compositional, structural, and surface properties of the various carriers toward their reactive performances. Besides assessing the performances of various oxygen carriers, their long-term performance, potential deactivation mechanism in the presence of CO 2, and strategies for their reactivation are also discussed in the context of chemical looping dry reforming of methane (CLDRM). While relatively underexplored, the current status of development, advantages, and potential limitations of CO 2 carriers in sorbent looping dry reforming of methane (SLDRM) and carbon carriers in chemical looping methane cracking (CLMC) are also reviewed and discussed. Emerging topics such as combined carriers are also covered along with a perspective for future research directions. Overall, this review aims to offer insights into the sustainable use of CO 2 through chemical looping, emphasizing the potential of solid reaction mediums across different carriers and the challenges associated with these solid reaction mediums.
Permeability prediction in the South Georgia rift basin–applications to CO2 storage and regional tectonics
Not provided.
Correction: Generating H2 during the CO2 sequestration in basalt formations
In this article [1], the author’s name Carl Steefel was incorrectly written as Carl Stefeel. The original article has been corrected.
Natural basalt reactivity towards CO2: implication for geologic storage in mafic rocks
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Characterization of multiphase flow in shaly caprock for geologic CO2 storage
Not provided.
Oxidative coupling of methane using oxidant mixtures of CO2 and O2 over Sr/La2O3
Not provided.
Highly stable two-dimensional bismuth metal-organic frameworks for efficient electrochemical reduction of CO2
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Highly active Ni/CeO2 catalyst for CO2 methanation: Preparation and characterization
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