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    中国百强科技报刊

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    Volume 37 Issue 1
    Jan.  2012
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    Article Contents
    ZHANG Zhou, ZHANG Hong-fu, 2012. Carbonation of Mafic-Ultramafic Rocks: A New Approach to Carbon Dioxide Geological Sequestration. Earth Science, 37(1): 156-162. doi: 10.3799/dqkx.2012.015
    Citation: ZHANG Zhou, ZHANG Hong-fu, 2012. Carbonation of Mafic-Ultramafic Rocks: A New Approach to Carbon Dioxide Geological Sequestration. Earth Science, 37(1): 156-162. doi: 10.3799/dqkx.2012.015

    Carbonation of Mafic-Ultramafic Rocks: A New Approach to Carbon Dioxide Geological Sequestration

    doi: 10.3799/dqkx.2012.015
    • Received Date: 2011-05-19
    • Publish Date: 2012-01-15
    • Geological sequestration is an effective way to enhance the net reduction of global CO2 emission. In nature, there is vast amount of carbonation of mafic-ultramafic rocks, reacting with CO2 to produce stable carbonate minerals. Factors that affect carbonation reaction rates of mafic-ultramafic rocks with CO2 include temperature, pressure, pH values, fluid flow rate, and contact surface area, etc.. Exothermic mineral reactions can drive the carbonation system into a self-heating regime. Meanwhile, controlling fluid flow rates can maintain the optimal temperature for reaction rate. Peridotites in ophiolite, continental flood basalt and deep-sea basalt are widespread on the shallow surface of the earth, providing an alternative for CO2 storage. Current research demonstrates that both technology and economic cost are available. Therefore, mafic-ultramafic rocks have huge potential for CO2 sequestration and it is a new approach to CO2 geological sequestration.

       

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