2020
DOI: 10.3390/en13051167
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Micro- and Macroscale Consequences of Interactions between CO2 and Shale Rocks

Abstract: In carbon storage activities, and in shale oil and gas extraction (SOGE) with carbon dioxide (CO2) as stimulation fluid, CO2 comes into contact with shale rock and its pore fluid. As a reactive fluid, the injected CO2 displays a large potential to modify the shale’s chemical, physical, and mechanical properties, which need to be well studied and documented. The state of the art on shale–CO2 interactions published in several review articles does not exhaust all aspects of these interactions, such as changes in … Show more

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Cited by 35 publications
(22 citation statements)
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“…Mixing of the shale pore fluid with the exposure fluid will thus cause the system to undergo changes toward a new equilibrium state. These changes may thus include: (1) ion exchange between clays and the new pore fluid followed by volumetric response of swelling clays (swelling, Energies 2021, 14, 2342 6 of 14 shrinkage), (2) changes in the interparticle interactions, (3) dissolution of some minerals due to contact with undersaturated solution [16,20]. minerals due to contact with undersaturated solution [16,20].…”
Section: Resultsmentioning
confidence: 99%
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“…Mixing of the shale pore fluid with the exposure fluid will thus cause the system to undergo changes toward a new equilibrium state. These changes may thus include: (1) ion exchange between clays and the new pore fluid followed by volumetric response of swelling clays (swelling, Energies 2021, 14, 2342 6 of 14 shrinkage), (2) changes in the interparticle interactions, (3) dissolution of some minerals due to contact with undersaturated solution [16,20]. minerals due to contact with undersaturated solution [16,20].…”
Section: Resultsmentioning
confidence: 99%
“…Indeed, an X-ray tomography cross-section image through sample The observed significant difference between the maximum peak force after exposure to HCl compared to NaCl is most likely due to leaching out of some cementing material at acidic conditions. It has been shown that exposure of some shale rocks to acidic environment leads to significant deterioration of shale mechanical properties [16,17,[22][23][24]. The loss of mechanical strength of shales upon exposure to acidic fluids was ascribed to dissolution of such minerals as: carbonates like calcite, dolomite, magnesite, and siderite; phyllosilicates like e.g., chlorite and K-feldspar [16,25].…”
Section: Resultsmentioning
confidence: 99%
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