Description

Carbon can be a major constituent of crustal and mantle uids, occurring both as dissolved ionic species (e.g., carbonate ions or organic acids) and molecular species (e.g., CO[subscript 2],

Carbon can be a major constituent of crustal and mantle uids, occurring both as dissolved ionic species (e.g., carbonate ions or organic acids) and molecular species (e.g., CO[subscript 2], CO, CH[subscript 4], and more complex organic compounds). The chemistry of dissolved carbon changes dramatically with pressure (P) and temperature (T). In aqueous uids at low P and T, molecular carbon gas species such as CO[subscript 2] and CH[subscript 4] saturate at low concentration to form a separate phase.

Reuse Permissions
  • application/pdf

    Download count: 0

    Details

    Contributors
    Date Created
    • 2013
    Resource Type
  • Text
  • Collections this item is in
    Identifier
    • Digital object identifier: 10.2138/rmg.2013.75.5
    • Identifier Type
      International standard serial number
      Identifier Value
      1529-6466

    Citation and reuse

    Cite this item

    This is a suggested citation. Consult the appropriate style guide for specific citation guidelines.

    Manning, C. E., Shock, E. L., & Sverjensky, D. A. (2013). The Chemistry of Carbon in Aqueous Fluids at Crustal and Upper-Mantle Conditions: Experimental and Theoretical Constraints. Reviews in Mineralogy and Geochemistry, 75(1), 109–148. doi:10.2138/rmg.2013.75.5

    Machine-readable links