通过注入CO2和水到玄武岩中进行in-situ碳矿化:对孔隙网络的影响
Seyi Philemon Akanji1, Lionel Esteban2, Ausama Giwelli3
1Edith Cowan University School of Engineering, 270 Joondalup Drive, Perth, Western Australia 6027, Australia; CSIRO Energy, 26 Dick Perry Ave, Kensington, Perth, Western Australia 6151, Australia.
Advances in colloid and interface science
|November 28, 2025
概括
在玄武岩中碳捕获和储存 (CCS) 通过矿化提供安全,永久的二氧化碳储存. 这种方法注入二氧化碳和水,形成固体碳酸盐,并可能改变岩石的多孔性和透性.
科学领域:
- 地球科学 地球科学 地球科学
- 地质化学 地质化学
- 环境科学 环境科学
背景情况:
- 碳捕获和储存 (CCS) 对于减轻全球变暖至关重要.
- 传统的地质储存依赖于盖封和地下水溶解.
- 在玄武岩中矿化是一种低风险的二氧化碳封存替代方案.
研究的目的:
- 审查基岩岩石中二氧化碳矿物化的实地和实验室研究.
- 分析二氧化碳矿化对岩石微观结构,毛孔网络,透性和多孔性的影响.
- 评估玄武岩形成的可行性,以永久存储二氧化碳.
主要方法:
- 综合现有的实地和实验室研究基岩中二氧化碳矿化.
- 溶解-沉反应及其对岩石性能的影响的分析.
- 评估影响矿化效率的因素,包括流体停留时间,反应表面积和现场岩石特性.
主要成果:
- 玄武岩中的二氧化碳矿化显著改变了岩石的微观结构.
- 流体停留时间,反应表面积和岩石透性/多孔性是影响的关键因素.
- 溶解可以增强孔隙连接性,而降水可能堵塞通道,尽管骨折可以减轻这一点.
结论:
- 玄武岩的形成是有希望的,安全的,可扩展的存储库,用于永久的二氧化碳储存.
- 连续溶解CO2注入策略,如CarbFix中的策略,可以通过管理溶解和降水区来优化存储.
- 需要进一步的研究来完善孔尺度过程的理解,并优化注入策略,以增强二氧化碳封存.
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