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    Application of MELTS to kinetic evaporation models of FeO-bearing silicate melts

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    Author
    Alexander, C. M. O'D.
    Issue Date
    2002-01-01
    Keywords
    Elemental fractionations
    chondrules
    
    Metadata
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    Citation
    Alexander, C. M. O'D. (2002). Application of MELTS to kinetic evaporation models of FeO‐bearing silicate melts. Meteoritics & Planetary Science, 37(2), 245-256.
    Publisher
    The Meteoritical Society
    Journal
    Meteoritics & Planetary Science
    URI
    http://hdl.handle.net/10150/655472
    DOI
    10.1111/j.1945-5100.2002.tb01107.x
    Additional Links
    https://meteoritical.org/
    Abstract
    Incorporation of the MELTS silicate melt solution model into models of evaporation successfully reproduces the evaporation behavior of alkali-free, FeO-bearing (greater than or equal to 2 mol%) chondritic melts at temperatures between 1700 and 2000 degrees C. In conjunction with the Berman CMAS melt solution model for FeO-poor melts, evaporation of alkali-free melts can now be modeled over a very wide range of conditions. MELTS-based evaporation models can also quite successfully reproduce the evaporation behavior of K when Al/(Na + K) > 1. However, reproduction of Na evaporation experiments is much poorer.
    Type
    Article
    text
    Language
    en
    ISSN
    1945-5100
    ae974a485f413a2113503eed53cd6c53
    10.1111/j.1945-5100.2002.tb01107.x
    Scopus Count
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    Meteoritics & Planetary Science, Volume 37, Number 2 (2002)

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