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GEOCHEMICAL INTERACTIONS BETWEEN CO_2, PORE-WATERS AND RESERVOIR ROCKS

机译:CO_2,孔隙水和水库岩石之间的地球化学相互作用

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摘要

The degree of reactivity between COj, pore-waters and minerals may have significant consequences on CO2 storage capacity, the injection process, and long-term safety and stability. Geochemical reactions are highly site-specific and time-dependent. They need to be assessed on a site-to-site basis according to best practises by combining numerical modelling and observations from laboratory experiments, field monitoring, and natural analogues. A selection of lessons learned from three European projects about the reactivity of CO2 with reservoir rocks and cap rocks is presented here for three sites: Sleipner (Norway) and Weyburn (Canada) where more than 1 Mt of CO2 per year has been injected underground since 1996 and 2000 respectively, and Montmiral, a natural CO2 field in France.
机译:COJ,孔隙水和矿物质之间的反应性可能对二氧化碳储存能力,注射过程和长期安全性和稳定性产生重大影响。地球化学反应是高度特异性和时间依赖性的。通过将数值建模和观察结果从实验室实验,现场监测和自然类似物组合,需要根据最佳实践进行评估。从三个欧洲关于CO2的反应性的一项经验教训,其中包括水库岩石和帽岩石的三个地点:Sleipner(挪威)和Weyburn(加拿大),每年超过1公吨二氧化碳的二氧化碳1996年和2000年,分别在法国的自然二氧化碳领域蒙疹。

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