Influence of amorphous silica layer formation on the dissolution rate of olivine at 90°C and elevated pCO2

For mitigating against rising levels of atmospheric CO2, carbonation of M2+-bearing silicates has been proposed as a possible option for sequestering CO2 over long time spans. Due to its rapid far-from-equilibrium dissolution rate and its widespread occurrence in mafic and ultramafic rocks, olivine...

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Veröffentlicht in:	Chemical geology 2011-05, Vol.284 (1-2), p.193-209
Hauptverfasser:	Daval, Damien, Sissmann, Olivier, Menguy, Nicolas, Saldi, Giuseppe D., Guyot, François, Martinez, Isabelle, Corvisier, Jérôme, Garcia, Bruno, Machouk, Imène, Knauss, Kevin G., Hellmann, Roland
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth Sciences Environmental Sciences Geochemistry Global Changes Sciences of the Universe
Online-Zugang:	Volltext
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