2021
DOI: 10.1016/j.cej.2020.127626
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CO2 solubility in brine in silica nanopores in relation to geological CO2 sequestration in tight formations: Effect of salinity and pH

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Cited by 50 publications
(45 citation statements)
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“…After the discussion of the effect of kerogen maturity and pore size on water and CO 2 distributions and CO 2 storage mechanisms, we evaluate the CO 2 storage capacity S cap in various kerogen nanopores, which is defined as where m CO 2 is the molar number of CO 2 molecules in the analysis region within nanopores (see Figure a) and V pore is the effective pore volume obtained from helium uptake method. , More details can be found in the “Effective Pore Volume” part in the Supporting Information.…”
Section: Resultsmentioning
confidence: 99%
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“…After the discussion of the effect of kerogen maturity and pore size on water and CO 2 distributions and CO 2 storage mechanisms, we evaluate the CO 2 storage capacity S cap in various kerogen nanopores, which is defined as where m CO 2 is the molar number of CO 2 molecules in the analysis region within nanopores (see Figure a) and V pore is the effective pore volume obtained from helium uptake method. , More details can be found in the “Effective Pore Volume” part in the Supporting Information.…”
Section: Resultsmentioning
confidence: 99%
“…Three pore sizes (1, 2, and 4 nm) are designed to represent the kerogen nanopores, which are within the dominant pore size distribution in kerogen. , CO 2 and water molecules can freely move in the system via molecular diffusion. Once the system reaches equilibrium (chemical potentials of water and CO 2 in the nanopore and bulk water reservoirs are equal ,, ), the distributions of CO 2 and water in the nanopore and bulk water reservoirs can be obtained in the corresponding regions. To minimize the pore end effect, we only use the center region of the kerogen nanopore (6 nm in the center in the x -direction, marked as “analysis region” in Figure a) for analysis.…”
Section: Methodsmentioning
confidence: 99%
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