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    Experimental studies of basalt-H2O-CO2 interaction with a high pressure column flow reactor: the mobility of metals

    Access Status
    Fulltext not available
    Authors
    Galeczka, I.
    Wolff-Boenisch, Domenik
    Gislason, S.
    Date
    2013
    Type
    Conference Paper
    
    Metadata
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    Citation
    Galeczka, I. and Wolff-Boenisch, D. and Gislason, S. 2013. Experimental studies of basalt-H2O-CO2 interaction with a high pressure column flow reactor: the mobility of metals, in Unknown (ed), 11th International Conference on Greenhouse Gas Control Technologies, GHGT-11, Nov 18 2012, pp. 5823-5833. Kyoto, Japan: Elsevier.
    Source Title
    Energy Procedia 37
    Source Conference
    11th International Conference on Greenhouse Gas Control Technologies, GHGT-11
    Additional URLs
    http://www.sciencedirect.com/science/article/pii/S1876610213007480/pdf?md5=0f77c5ff85d7cec6824ae7cac596df63&pid=1-s2.0-S1876610213007480-main.pdf
    ISSN
    1876-6102
    URI
    http://hdl.handle.net/20.500.11937/18567
    Collection
    • Curtin Research Publications
    Abstract

    Here, we report on the mobility of metals at the early stage of CO2 injection into basalt, before significant precipitation of secondary minerals. Short-lived pulses (50-100 hours) of CO2-charged water were injected into a high pressure column flow reactor filled with basaltic glass grains at 22°C, 8 MPa of total pressure and a velocity of 0.4 cm/min. The residence time of the water within the column ranged from 8 to 10 hours. The column was conditioned with pure water, resulting in alkaline outflow (pH ~9). The pH of the inlet CO2-charged water was ~3.2, and the lowest pH measured in the column was 4.5, after less than 10 hours of water/rock interaction. The dissolved metal concentrations and metals relative mobility increased dramatically during the CO2-pulses; more than 100 times for Sr, Fe, Al, Ca, Ba, Mn, and Mg. Of these elements, all but Al can bind with CO2 to form carbonate minerals. Only the dissolved Al, Fe, Mn and Cr concentrations exceeded allowable drinking water limits. After the CO2-pulses, all of the elemental concentrations decreased close-to or even below what was measured during the conditioning of the column. The pH never reached ~9 which was the initial pH before CO2-pulses.

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