首页|玄武岩矿化封存CO2机理及储层演化特征研究进展

玄武岩矿化封存CO2机理及储层演化特征研究进展

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随着全球气候变暖的不断加剧,以及中国"双碳"目标的提出,降低CO2排放迫在眉睫.作为最有前景的CO2地质封存技术之一,玄武岩矿化封存研究备受关注.为掌握该技术最新进展,推动中国在该领域的发展,拟从玄武岩地质特征、玄武岩-CO2矿化机理、储层物性演化等方面开展现状调研,并对中国部分玄武岩分布地区进行了封存潜力初步估算.研究指出,玄武岩原始矿物组分、孔渗特性等地质差异特征对矿化封存过程具有重要影响,但目前针对该过程中储层物性演化特征还不清晰,CO2注入后矿化封存机理及多尺度流体运移规律表征理论模型、手段和技术尚待进一步完善.估算结果表明,中国玄武岩分布广泛,尤其以具有良好源储配置和巨量体积的峨眉山玄武岩具有最大区域封存潜力.
Research progress on the CO2 mineralization mechanism and evolution of the physical properties of basalt
With the increase of global warming and China's"double carbon"goal,there is urgent need to reduce CO2 emissions.As one of the most promising CO2 geological storage technologies,basalt mineralization storage has attracted considerable research attention.In order to understand the latest progress of this technology and promote the development of this field in China,we have carried out a status quo study of the geological characteristics of basalt,basalt-CO2 mineralization mechanism,and the physical properties of basalt reservoirs,and have made a preliminary estimation of sequestration potential in some basalt-distributed areas in China.It is pointed out in this study that the original mineral components of basaltic rocks,the pore-permeability characteristics of the endowment,and other geological properties each have an important influence on the mineralization and storage process.However,the evolutionary characteristics of this process and the physical properties of basalt reservoirs are still unclear,and the theoretical models,tools,and techniques used to characterize the mineralization and storage mechanism,including the multiscale fluid transport law after CO2 injection,need to be further improved.The results of this study reveal that basalts in China are extensively distributed,with Emeishan basalts particularly prevalent.These basalts exhibit favorable source-reservoir configurations and significant volumes,making them highly promising for regional CO2 storage.

carbon dioxidebasaltmechanism of mineralization storagereservoir evolutionpotential estimation

刘云乾、廖志伟、丁海、甘泉、方惠京、罗永江、陈强

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重庆大学资源与安全学院,重庆 400044

安徽省煤田地质局勘查研究院,合肥 230088

二氧化碳 玄武岩 矿化封存机理 储层演化 潜力估算

2024

成都理工大学学报(自然科学版)
成都理工大学

成都理工大学学报(自然科学版)

CSTPCD北大核心
影响因子:1.596
ISSN:1671-9727
年,卷(期):2024.51(6)