$Influence of heterogeneity on dissolved CO2 migration in a fractured reservoir$

Influence of heterogeneity on dissolved CO2 migration in a fractured reservoir

Dissolution trapping CO 2 is thought to be a permanent storage mechanism in deep saline aquifers. Brine saturated with CO 2 sinks to the bottom of the aquifer due to density-driven flow and is replaced by fresh brine with the remaining dissolution potential. This convective process persists and can...

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Veröffentlicht in:	Environmental earth sciences 2024-08, Vol.83 (16), p.463, Article 463
Hauptverfasser:	Chen, Ruiqi, Xu, Wenjie, Chen, Yunmin, Nagel, Thomas, Chen, Chaofan, Hu, Yingtao, Li, Jinlong, Zhuang, Duanyang
Format:	Artikel
Sprache:	eng
Schlagworte:	Apertures Aquifers Biogeosciences Brines Carbon dioxide Carbon sequestration Channels Convection Density Dissolution Dissolving Earth and Environmental Science Earth Sciences Environmental Science and Engineering Fractured reservoirs Fractures Geochemistry Geology Heterogeneity Hydrology/Water Resources Original Article Permeability Reservoirs Risk reduction Terrestrial Pollution Three dimensional analysis Trapping
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