Dissolution of basalts and peridotite in seawater, in the presence of ligands, and CO2: Implications for mineral sequestration of carbon dioxide

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Dissolution of basalts and peridotite in seawater, in the presence of ligands, and CO2: Implications for mineral sequestration of carbon dioxide

Steady-state silica release rates (rSi) from basaltic glass and crystalline basalt of similar chemical composition as well as dunitic peridotite have been determined in far-from-equilibrium dissolution experiments at 25 °C and pH 3.6 in (a) artificial seawater solutions under 4 bar pCO2, (b) varying...

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Bibliographic Details
Main Authors:	Wolff-Boenisch, Domenik, Wenau, S., Gislason, S., Oelkers, E.
Format:	Journal Article
Published:	Pergamon-Elsevier Science Ltd 2011
Online Access:	http://hdl.handle.net/20.500.11937/33562

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