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    In:  Other Sources
    Publication Date: 2011-08-16
    Description: Consideration of theoretical limits and experimental data for the kinetics of the reaction quartz plus calcite yields wollastonite plus CO2 supports the concept of a short-term quasi-equilibrium state for the atmosphere of Venus. These data indicate that the time scale of this reaction and of any competing CO2 producing reaction may be as short as several hundred years or less at the inferred Venus surface temperatures.
    Keywords: SPACE SCIENCES
    Type: Icarus; 19; Aug. 197
    Format: text
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