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

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

Feb 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002m%26ps...37..245a&link_type=abstract

Meteoritics & Planetary Science, vol. 37, no. 2, pp. 245-256 (2002)

Physics

8

Scientific paper

Incorporation of the MELTS silicate melt solution model into models of evaporation successfully reproduces the evaporation behavior of alkali-free, FeO-bearing (?2 mol%) chondritic melts at temperatures between 1700 and 2000 ?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.

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