Oxygen Solubility in Iron Melts at High Pressures and Temperatures: Experimental Constraints on Terrestrial Planetary Core Formation

Details Oxygen Solubility in Iron Melts at High Pressures and Temperatures: Experimental Constraints on Terrestrial Planetary Core Formation Oxygen Solubility in Iron Melts at High Pressures and Temperatures: Experimental Constraints on Terrestrial Planetary Core Formation

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1872l&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Physics

Scientific paper

Solubility of oxygen was investigated experimentally in Fe-rich portions
of Fe-FeO and Fe-O-S systems at HP and HT (15 and 23 GPa,
1500°-2000°C). Our results indicate an increase of oxygen
solubility with increasing pressure at eutectic conditions.

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