2020
DOI: 10.1016/j.cej.2020.125449
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Hydrophilicity/hydrophobicity driven CO2 solubility in kaolinite nanopores in relation to carbon sequestration

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Cited by 45 publications
(35 citation statements)
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“…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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“…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%
“…The detailed review of the above works can be found in our recent work and a recent review paper . According to our recent works, , CO 2 solubility in water/brine in the kaolinite and silica nanopores strongly depends on the confinement surface chemistry. Therefore, CO 2 solubility in water in kerogen nanopores might be dependent on its maturity.…”
Section: Introductionmentioning
confidence: 98%
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“…The phase of these samples is characterized by XRD. As shown in Figures 2(a)-2(f), by comparing the diffraction peaks with the standard cards, it is confirmed that the materials are correspondingly attapulgite, halloysite, sepiolite, montmorillonite, kaolinite, and diatomite, respectively [50][51][52][53][54][55].…”
Section: Resultsmentioning
confidence: 58%