2022
DOI: 10.1016/j.chemgeo.2022.120742
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Geochemical modelling of CO2 interactions with shale: Kinetics of mineral dissolution and precipitation on geological time scales

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Cited by 38 publications
(42 citation statements)
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“…The dissolution of potassium feldspar (KAlSi 3 O 8 ) and plagioclase in carbonic acid (H 2 CO 3 ) produces quartz as the primary byproduct. Consequently, it is expected that the samples will experience an increase in the amount of quartz and subsequent precipitation of this mineral KAlSi 3 O 8 + 2 H + + H 2 O 2 K + + Al 2 Si 2 O 5 false( normalOH false) 4 + 4 SiO 2 NaAlSi 3 O 8 + H 2 CO 3 + H 2 O Na + HCO 3 + Al 2 Si 2 O 5 ( OH ) 4 + H 4 SiO 4 ...…”
Section: Interaction Of Sc-co2 With Shalementioning
confidence: 99%
“…The dissolution of potassium feldspar (KAlSi 3 O 8 ) and plagioclase in carbonic acid (H 2 CO 3 ) produces quartz as the primary byproduct. Consequently, it is expected that the samples will experience an increase in the amount of quartz and subsequent precipitation of this mineral KAlSi 3 O 8 + 2 H + + H 2 O 2 K + + Al 2 Si 2 O 5 false( normalOH false) 4 + 4 SiO 2 NaAlSi 3 O 8 + H 2 CO 3 + H 2 O Na + HCO 3 + Al 2 Si 2 O 5 ( OH ) 4 + H 4 SiO 4 ...…”
Section: Interaction Of Sc-co2 With Shalementioning
confidence: 99%
“…The alterations of minerals in shale are also influenced by the reaction kinetics of different minerals in shale. Carbonate has the largest reaction rate with CO 2 ; clay minerals and feldspars react more slowly with CO 2 than carbonates, which may last for decades, centuries, or millennia. Thus, for different minerals, the dissolution and precipitation kinetics of the mineral associated with CO 2 /brine–shale interaction covers multiple time scales. In addition, the spatial heterogeneity in the distribution of pore structure and mineral also affects CO 2 –shale reaction rates.…”
Section: Alterations In Physical and Chemical Properties Of Shalementioning
confidence: 99%
“…Numerous studies have reported that injecting CO 2 into geological formations can disrupt the geochemical equilibrium through dissolution and precipitation processes, which affect the reservoir mineral phases. , However, it has been mentioned that, by having a small number of secondary minerals present in the formation after CO 2 injection, considerable changes in permeability and porosity can be seen through precipitation. , Similarly, Shao et al reported that the permeability could decrease when the precipitation size is nearly equal to the size of the pore throats in the porous system of the formation …”
Section: Introductionmentioning
confidence: 99%