Enhancing magnesite formation at low temperature and high CO2 pressure: The impact of seed crystals and minor components

• Published in: Chemical geology 2015-02, Vol.395, p.119-125
• Main Authors: Felmy, Andrew R., Qafoku, Odeta, Arey, Bruce W., Kovarik, Libor, Liu, Jia, Perea, Daniel, Ilton, Eugene S.
• Format: Article
• Language: English
• Subjects: Bicarbonates; Carbon dioxide; Carbonates; Formations; Magnesite; Magnesium carbonate; Mathematical models; Nucleation; Scanning electron microscopy; Seed crystals
• ISSN: 0009-2541; 1872-6836
• DOI: 10.1016/j.chemgeo.2014.12.003

The formation of magnesite was followed in aqueous solution containing initially added Mg(OH)2 equilibrated with supercritical carbon dioxide (90atm pressure, 50°C) in the presence of introduced magnesite particles and minor components, Co(II). As expected, the introduction of magnesite particles accelerated the formation of magnesite from solution. However, the formation rate of magnesite was even greater when small concentrations of Co(II) were introduced, indicating that the increased rate of magnesite formation in the presence of Co(II) was not solely due to the addition of a growth promoting surface. Detailed analysis of the magnesite particles by scanning electron microscopy (SEM), transmission electron microscopy (TEM), energy dispersive spectroscopy (EDS), and atom probe tomography (APT) revealed that the originally added Co(II) was concentrated in the center but also present throughout the growing magnesite particles. Addition of the Co(II) in different chemical forms (i.e. as solid phase CoCO3 or Co(OH)2) could alter the growth rate of magnesite depending upon the addition of bicarbonate to the starting solution. Geochemical modeling calculations indicate that this difference is related to the thermodynamic stability of these different phases in the initial solutions. More broadly, these results indicate that the presence of even small concentrations of foreign ions that form carbonate compounds with a similar structure as magnesite can be incorporated into the magnesite lattice, accelerating the formation of anhydrous carbonates in natural environments. •Substitution of minor components (Co) accelerates magnesite formation.•The minor components (Co) are distributed throughout the formed magnesite•Magnesite can form at low temperature (50°C) in supercritical CO2.•Geochemical modeling indicates different solid forms of the minor components can yield different magnesite formation rates.