Influence of amorphous silica layer formation on the dissolution rate of olivine at 90°C and elevated pCO2-Reference-Cited by-同舟云学术

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

Published:2011-05 Issue:1-2 Volume:284 Page:193-209
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Daval Damien,Sissmann Olivier,Menguy Nicolas,Saldi Giuseppe D.,Guyot François,Martinez Isabelle,Corvisier Jérôme,Garcia Bruno,Machouk Imène,Knauss Kevin G.,Hellmann Roland

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference80 articles.

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4. The thermal behaviour and structural stability of nesquehonite, MgCO3 center dot 3H(2)O, evaluated by in situ laboratory parallel-beam X-ray powder diffraction: new constraints on CO2 sequestration within minerals;Ballirano;Journal of Hazardous Materials,2010

5. Carbon sequestration via aqueous olivine mineral carbonation: role of passivating layer formation;Bearat;Environmental Science & Technology,2006

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