Phase relations in the Fe-Fe3C-Fe3N system at 7.8 GPa and 1150°C: implications for C and N hosts in metal-saturated mantle. Issue 4 (2nd October 2021)

• Record Type: Journal Article
• Authors: Kruk, Alexey N.; Korablin, Alexander A.; Sokol, Alexander G.; Palyanov, Yury N.
• Is Part Of: High pressure research. Volume 41:Issue 4(2021)
• Page Start: 392
• Page End: 404
• Publication Date: 2021-10-02
• Subjects: Mantle -- experiment -- native iron -- carbon and nitrogen hosts -- diamond; High pressure (Science) -- Periodicals; High pressure (Technology) -- Periodicals; 536.41
• DOI: 10.1080/08957959.2021.1998479
• Languages: English
• ISSNs: 0895-7959

Abstract

ABSTRACT: The isothermal section of the Fe-Fe3 C-Fe3 N phase diagram at 7.8 GPa and 1150°С comprises a three-phase field of γ-Fe + Fe3 C + ϵ-Fe3 (С/N) in the central part and three two-phase fields (γ-Fe + Fe3 C, γ-Fe + ϵ-Fe3 (С/N) and Fe3 C + ϵ-Fe3 (С/N)) bounded by three single-phase fields of γ-Fe, Fe3 C and ϵ-Fe3 (С/N) solid solutions along the triangle sides. Thus, native iron can host carbon and nitrogen in the γ-Fe + Fe3 C or γ-Fe phases in the mantle depleted in volatiles (20 ppm C and 1 ppm N) at temperatures corresponding to the ∼35 mW/m 2 heat flux, and in the Fe3 C or ϵ-Fe3 (С/N) phases if the contents of volatiles in the mantle reach 250 ppm C and 100 ppm N. Iron carbonitride has quite a large stability field even at low nitrogen concentrations in the system simulating native iron.