2009
DOI: 10.1016/j.egypro.2009.02.319
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A continuous process for manufacture of magnesite and silica from olivine, CO2 and H2O

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Cited by 29 publications
(11 citation statements)
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“…Also, calcitization and Mg-depletion of ultramafic rocks are commonly observed, but again, no attempts have been made to study these processes in experiments. Most of the recent experimental studies that were conducted to evaluate the efficiency of potential CO 2 mineral sequestration technologies have focused on the formation of magnesite from pure olivine or fresh peridotite (e.g., O' Connor et al, 2004;Giammar et al, 2005;Chizmeshya et al, 2007;Gerdemann et al, 2007;Andreani et al, 2009;Dufaud et al, 2009;Munz et al, 2009;Garcia et al, 2010). However, several difficulties that could drastically limit the efficiency of such processes exist, including the high supersaturation needed for magnesite nucleation and growth (e.g., Giammar et al, 2005;Saldi et al, 2009) and the uptake of Mg by secondary hydrous Mg-silicates (King et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…Also, calcitization and Mg-depletion of ultramafic rocks are commonly observed, but again, no attempts have been made to study these processes in experiments. Most of the recent experimental studies that were conducted to evaluate the efficiency of potential CO 2 mineral sequestration technologies have focused on the formation of magnesite from pure olivine or fresh peridotite (e.g., O' Connor et al, 2004;Giammar et al, 2005;Chizmeshya et al, 2007;Gerdemann et al, 2007;Andreani et al, 2009;Dufaud et al, 2009;Munz et al, 2009;Garcia et al, 2010). However, several difficulties that could drastically limit the efficiency of such processes exist, including the high supersaturation needed for magnesite nucleation and growth (e.g., Giammar et al, 2005;Saldi et al, 2009) and the uptake of Mg by secondary hydrous Mg-silicates (King et al, 2010).…”
Section: Introductionmentioning
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%
“…Work on a three-step process of olivine carbonation, involving (i) dissolution of olivine, (ii) precipitation of magnesite and (iii) precipitation of silica in an aqueous solution was recently reported from norway (Munz et al, 2009), where the process proceeds without chemical additives at 100-150 bar and 130-250 °C. no reaction rates were, however, reported.…”
Section: Recent Developments (2005-today)mentioning
confidence: 98%