{"title":"Reaction mechanisms and evolution of pore structure and wettability in the CO2-shale system: A systematic review","authors":"Yaxiong Zhang , Qihong Feng , Sen Wang","doi":"10.1016/j.earscirev.2025.105262","DOIUrl":null,"url":null,"abstract":"<div><div>The geochemical reactions involving CO<sub>2</sub>-water-shale induce significant alterations in reservoir pore permeability characteristics and physical properties through mineral dissolution, clay swelling, and micropore structure evolution, exerting a crucial influence on CO<sub>2</sub>-enhanced shale recovery and its geological storage. This review systematically summarizes the patterns and mechanisms of CO<sub>2</sub>-water-shale geochemical reactions, examines the processes and recent advances in CO<sub>2</sub>-shale geochemical interactions, and clarifies the impact of geochemical reactions on shale properties, including shale mineral dissolution, swelling, erosion, and precipitation triggered by CO<sub>2</sub> injection, and integrates the chemo-mechanical coupling mechanisms as well as multi-scale evolution mechanisms from the perspectives of mineral composition, microstructure, mechanical properties, and wettability. Studies indicate that the spatiotemporal coupling of geochemical reactions (e.g., dissolution and precipitation) and physical processes (e.g., swelling) fundamentally alters shale's pore structure, micro-morphology, and mechanical properties. Meanwhile, this process is jointly regulated by temperature, pressure, and the content and composition of minerals such as clay and carbonate. Furthermore, the review prospects challenges and future development trends concerning CO<sub>2</sub>-shale interactions, providing a detailed theoretical foundation and scientific basis for research on injecting CO<sub>2</sub> into shale reservoirs for enhanced oil recovery.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"271 ","pages":"Article 105262"},"PeriodicalIF":10.0000,"publicationDate":"2025-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth-Science Reviews","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0012825225002235","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
The geochemical reactions involving CO2-water-shale induce significant alterations in reservoir pore permeability characteristics and physical properties through mineral dissolution, clay swelling, and micropore structure evolution, exerting a crucial influence on CO2-enhanced shale recovery and its geological storage. This review systematically summarizes the patterns and mechanisms of CO2-water-shale geochemical reactions, examines the processes and recent advances in CO2-shale geochemical interactions, and clarifies the impact of geochemical reactions on shale properties, including shale mineral dissolution, swelling, erosion, and precipitation triggered by CO2 injection, and integrates the chemo-mechanical coupling mechanisms as well as multi-scale evolution mechanisms from the perspectives of mineral composition, microstructure, mechanical properties, and wettability. Studies indicate that the spatiotemporal coupling of geochemical reactions (e.g., dissolution and precipitation) and physical processes (e.g., swelling) fundamentally alters shale's pore structure, micro-morphology, and mechanical properties. Meanwhile, this process is jointly regulated by temperature, pressure, and the content and composition of minerals such as clay and carbonate. Furthermore, the review prospects challenges and future development trends concerning CO2-shale interactions, providing a detailed theoretical foundation and scientific basis for research on injecting CO2 into shale reservoirs for enhanced oil recovery.
co2 -水-页岩地球化学反应通过矿物溶蚀、粘土溶胀、微孔结构演化等导致储层孔隙渗透率特征和物性发生显著变化,对co2增强页岩采收率及其地质储层具有重要影响。本文系统总结了CO2-水-页岩地球化学反应的模式和机制,综述了CO2-页岩地球化学相互作用的过程和最新进展,阐明了地球化学反应对页岩性质的影响,包括CO2注入引发的页岩矿物溶解、溶胀、侵蚀和降水等。从矿物组成、微观结构、力学性能和润湿性等方面综合了化学-力学耦合机制和多尺度演化机制。研究表明,地球化学反应(如溶解、沉淀)和物理过程(如溶胀)的时空耦合作用从根本上改变了页岩的孔隙结构、微观形态和力学性能。同时,这一过程受温度、压力以及粘土、碳酸盐等矿物的含量和组成的共同调节。展望了CO2-页岩相互作用研究面临的挑战和未来发展趋势,为页岩储层注CO2提高采收率的研究提供了详细的理论基础和科学依据。
期刊介绍:
Covering a much wider field than the usual specialist journals, Earth Science Reviews publishes review articles dealing with all aspects of Earth Sciences, and is an important vehicle for allowing readers to see their particular interest related to the Earth Sciences as a whole.