Evaporite Caprock Integrity. An experimental study of reactive mineralogy and pore-scale heterogeneity during brine-CO2 exposure
- Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Characterization and geochemical data are presented from a core-flooding experiment on a sample from the Three Fingers evaporite unit forming the lower extent of caprock at the Weyburn-Midale reservoir, Canada. This low-permeability sample was characterized in detail using X-ray computed microtomography before and after exposure to CO 2-acidified brine, allowing mineral phase and voidspace distributions to be quantified in three dimensions. Solution chemistry indicated that CO 2-acidified brine preferentially dissolved dolomite until saturation was attained, while anhydrite remained unreactive. Dolomite dissolution contributed to increases in bulk permeability through the formation of a localized channel, guided by microfractures as well as porosity and reactive phase distributions aligned with depositional bedding. An indirect effect of carbonate mineral reactivity with CO 2-acidified solution is voidspace generation through physical transport of anhydrite freed from the rock matrix following dissolution of dolomite. The development of high permeability fast pathways in this experiment highlights the role of carbonate content and potential fracture orientations in evaporite caprock formations considered for both geologic carbon sequestration and CO 2-enhanced oil recovery operations.
- Research Organization:
- Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
- Sponsoring Organization:
- USDOE
- Grant/Contract Number:
- AC52-07NA27344
- OSTI ID:
- 1237526
- Report Number(s):
- LLNL-JRNL-544136
- Journal Information:
- Environmental Science and Technology, Vol. 47, Issue 1; ISSN 0013-936X
- Publisher:
- American Chemical Society (ACS)Copyright Statement
- Country of Publication:
- United States
- Language:
- English
Web of Science
Permeability impairment of a limestone reservoir triggered by heterogeneous dissolution and particles migration during CO 2 -rich injection: DISSOLUTION-INDUCED PARTICLE MIGRATION
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journal | September 2013 |
Permeability of Wellbore-Cement Fractures Following Degradation by Carbonated Brine
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journal | December 2012 |
Reactive Transport Simulation of Fracture Channelization and Transmissivity Evolution
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journal | January 2019 |
A review of geochemical–mechanical impacts in geological carbon storage reservoirs
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journal | May 2019 |
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