2011
DOI: 10.1016/j.egypro.2011.02.475
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Importance of dissolution and precipitation kinetics for mineral carbonation

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Cited by 22 publications
(13 citation statements)
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“…However, MgCO 3 formation could be observed when natural ores (e.g., serpentine, olivine, etc) were selected as the feedstock for carbonation (Alexander et al, 2007;Krevor and Lackner, 2011). Furthermore, the study reported by Haug et al (2011) indicated that the mineral carbonation of olivine (generally rich in Mg contents) at 115 bar and 185°C is limited by MgCO 3 (magnesite) precipitation and not the olivine dissolution rate. O'Connor et al (2002) also found that conversion of the silicate to carbonate does not occur in the solid state but appears to require mineral dissolution in the aqueous phase.…”
Section: Rate Of Carbonate Precipitationmentioning
confidence: 99%
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“…However, MgCO 3 formation could be observed when natural ores (e.g., serpentine, olivine, etc) were selected as the feedstock for carbonation (Alexander et al, 2007;Krevor and Lackner, 2011). Furthermore, the study reported by Haug et al (2011) indicated that the mineral carbonation of olivine (generally rich in Mg contents) at 115 bar and 185°C is limited by MgCO 3 (magnesite) precipitation and not the olivine dissolution rate. O'Connor et al (2002) also found that conversion of the silicate to carbonate does not occur in the solid state but appears to require mineral dissolution in the aqueous phase.…”
Section: Rate Of Carbonate Precipitationmentioning
confidence: 99%
“…Various studies have addressed methods to speed up the kinetics of direct aqueous carbonation including physical and chemical pretreatment (Maroto-Valer et al, 2005a, b), electrolysis and heat pretreatment , and mechanical activation methods (McKelvy et al, 2004;Park and Fan, 2004;Haug et al, 2010;Haug et al, 2011). O'Connor et al (2002) investigated approaches to reduce particle size, and increase surface area, and elevate process temperature and pressure by thermal treatment or steam activation.…”
Section: Performance Evaluationmentioning
confidence: 99%
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“…Mineral carbonation transform carbon dioxide into the form of geologically and thermodynamically stable magnesium carbonate. This process can be considered as a result of two steps: (1) dissolution of silicate minerals and (2) the reaction between either calcium or magnesium cations and CO 2 to create carbonates [1][2][3][4][5][6]. For aqueous carbonation, magnesium silicate minerals such as serpentinite and olivine are frequently used [7][8][9].…”
Section: Introductionmentioning
confidence: 99%