2010
DOI: 10.1016/j.apgeochem.2010.08.005
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Investigating dissolution of mechanically activated olivine for carbonation purposes

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Cited by 78 publications
(62 citation statements)
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“…CO 2 has a critical point at 31.06°C and 73.8 bars (1,070 lb/in 2 ) and a critical density of 0.469 g/cm 3 . It could be dissolved from the atmosphere in available water, and carbonic acid can be created with a pH around 5.6 (Haug et al, 2010). In addition, diffusion of CO 2 in water is approximately 10000 times lower than in air.…”
Section: Ion Equilibrium In Solutionmentioning
confidence: 99%
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“…CO 2 has a critical point at 31.06°C and 73.8 bars (1,070 lb/in 2 ) and a critical density of 0.469 g/cm 3 . It could be dissolved from the atmosphere in available water, and carbonic acid can be created with a pH around 5.6 (Haug et al, 2010). In addition, diffusion of CO 2 in water is approximately 10000 times lower than in air.…”
Section: Ion Equilibrium In Solutionmentioning
confidence: 99%
“…However, the kinetics of natural carbonation is extremely slow due to the relatively low CO 2 concentration, about 0.03-0.06% (Lackner, 2002;Costa et al, 2007). According to an investigation by Haug et al (2010), the weathering rate of olivine is estimated to be 10 −8.5 mol/(m 2 s) using the average ground temperature in Norway of 6°C and a pH of 5.6, which corresponds to the acidity of rainwater.…”
Section: Natural Carbonationmentioning
confidence: 99%
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