The Role of Hydrogen and Oxygen Fugacity on the Incorporation of Nitrogen in Reduced Magmas of the Early Earth's Mantle

Details The Role of Hydrogen and Oxygen Fugacity on the Incorporation of Nitrogen in Reduced Magmas of the Early Earth's Mantle The Role of Hydrogen and Oxygen Fugacity on the Incorporation of Nitrogen in Reduced Magmas of the Early Earth's Mantle

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1037k&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

According to experiments at 4 GPa, 1550°C, significant amounts of
nitrogen (NH3, NH4) could have been incorporated
in the early Earth by dissolution in a magma ocean, under fO2
conditions relevant to those prevailing during metal segregation.

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