Review on in-situ CO2 mineralization sequestration: mechanistic understanding and research frontiers

Abstract The substantial emissions of greenhouse gases, particularly CO 2 , constitute a primary driver of global warming. CCUS is proposed as an effective mitigation strategy which is often estimated to account for about 15% of cumulative carbon emission reduction. In-situ CO 2 mineralization sequestration, compared to conventional geological storage methods such as depleted oil and gas reservoirs, unmineable coal seams, and deep saline aquifers, offers the advantage of permanent immobilization of injected carbon. However, uncertainties persist regarding the characteristics of geochemical interactions under reservoir pore conditions, as well as the kinetic mechanisms of mineralization reactions. Additionally, geochemical reactions may lead to solid particle transport and deposition, potentially causing pore throat occlusion. Pilot projects in Iceland and the United States have demonstrated the feasibility of this technology, but the field remains in the early deployment stage. In this review, the mechanisms of in-situ mineralization have been elucidated, the primary factors influencing the reaction kinetics have been discussed, and the current research status in this field has been summarized. It is emphasized that establishing a reliable system for evaluating storage capacity and understanding the kinetic mechanisms governing CO 2 conversion into minerals at multi-phase interfaces are key priorities for future work.

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Publication Details

Journal
International Journal of Coal Science & Technology
Published
2025-02-18
DOI
https://doi.org/10.1007/s40789-025-00755-8
Citations
37
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
29.57

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article

Review on in-situ CO2 mineralization sequestration: mechanistic understanding and research frontiers

Michelle Ma, Wentao Zhao, Yanjun Xie, Zhanpeng Wang et al.
37 citations
International Journal of Coal Science & Technology
CO2 Sequestration and Geologic Interactions
29.57
article

Review on in-situ CO2 mineralization sequestration: mechanistic understanding and research frontiers

Michelle Ma, Wentao Zhao, Yanjun Xie, Zhanpeng Wang, Qi Liu, Chenggang Xian, Hang Ye, Qi Bao
article en
37 citations

Abstract

Abstract The substantial emissions of greenhouse gases, particularly CO 2 , constitute a primary driver of global warming. CCUS is proposed as an effective mitigation strategy which is often estimated to account for about 15% of cumulative carbon emission reduction. In-situ CO 2 mineralization sequestration, compared to conventional geological storage methods such as depleted oil and gas reservoirs, unmineable coal seams, and deep saline aquifers, offers the advantage of permanent immobilization of injected carbon. However, uncertainties persist regarding the characteristics of geochemical interactions under reservoir pore conditions, as well as the kinetic mechanisms of mineralization reactions. Additionally, geochemical reactions may lead to solid particle transport and deposition, potentially causing pore throat occlusion. Pilot projects in Iceland and the United States have demonstrated the feasibility of this technology, but the field remains in the early deployment stage. In this review, the mechanisms of in-situ mineralization have been elucidated, the primary factors influencing the reaction kinetics have been discussed, and the current research status in this field has been summarized. It is emphasized that establishing a reliable system for evaluating storage capacity and understanding the kinetic mechanisms governing CO 2 conversion into minerals at multi-phase interfaces are key priorities for future work.

International Journal of Coal Science & TechnologyVol. 12(1)
China University of Petroleum, Beijing (CN), Huaneng Clean Energy Research Institute (CN)
National Natural Science Foundation of China, Science Foundation of China University of Petroleum, Beijing
Openalex Percentile: Top 0%
CO2 Sequestration and Geologic Interactions
29.57
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