2009
DOI: 10.1016/j.chemgeo.2009.01.022
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Carbonation of Ca-bearing silicates, the case of wollastonite: Experimental investigations and kinetic modeling

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Cited by 231 publications
(168 citation statements)
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“…Compared with other CCS technologies, it has the advantage of safely storing CO 2 for a very long, if not infinite, time, by converting CO 2 into a solid phase. Through a reaction between rich calcium and magnesium ions in natural alkaline ores [8][9][10][11][12][13][14][15][16][17][18] and alkaline wastes [19][20][21][22][23], CO 2 could be converted into stable solid carbonates, such as magnesium carbonate and calcium carbonate. Forsterite, with a high CO 2 conversion rate, is the main mineralization material.…”
mentioning
confidence: 99%
“…Compared with other CCS technologies, it has the advantage of safely storing CO 2 for a very long, if not infinite, time, by converting CO 2 into a solid phase. Through a reaction between rich calcium and magnesium ions in natural alkaline ores [8][9][10][11][12][13][14][15][16][17][18] and alkaline wastes [19][20][21][22][23], CO 2 could be converted into stable solid carbonates, such as magnesium carbonate and calcium carbonate. Forsterite, with a high CO 2 conversion rate, is the main mineralization material.…”
mentioning
confidence: 99%
“…These divalent cations, in addition to the alkalinity required for CO 2 conversion to carbonate ions can be considered as the main rawmaterials for the mineral CO 2 sequestration process (reaction 2.1). Alkaline silicate minerals such as wollastonite can potentially provide the divalent cation and alkalinity needed for the capture and sequestration of CO 2 at ambient environmental conditions (reaction 2.2) (Daval et al, 2009). There are far more than sufficient alkaline silicate materials available to sequester the equivalent CO 2 of the total known amount of fossil fuels (Graves et al, 2006;Kelemen & Matter, 2008;Lackner et al, 1995).…”
Section: Challenges For Application Of Mineral Co 2 Sequestrationmentioning
confidence: 99%
“…Despite studies highlighting the mineralogical variation between ISM facilities, 14) the typical reported information is limited to the slag source (e.g., BF, BOF, EAF) and the elemental composition as simple oxides. Work from the silicate rock-based CO 2 mineralization field has shown that the ostensibly similar Mg 2 SiO 4 and CaSiO 3 differ in CO 2 mineralization depth by ~4 orders of magnitude (≤40 nm 16) and ≥ 125 μm, 17) respectively), despite comparable thermodynamic driving forces (ΔG r = − 34.7 kJ/mol and − 39.5 kJ/mol, respectively) and dissolution rates. 18) Though thermodynamics determines the initial surface reactions, the activation energy is structurally-dependent, 19) and the mineralogy determines the PL characteristics which are the primary inhibitory feedback on CO 2 mineralization reactions.…”
Section: Mineralogy and Crystallinitymentioning
confidence: 99%