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Systematics of the post-spinel tranisition in Fe-bearing compositions

Fachliche Zuordnung Mineralogie, Petrologie und Geochemie
Förderung Förderung von 2006 bis 2010
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 24942365
 
Erstellungsjahr 2011

Zusammenfassung der Projektergebnisse

The experimental results from this project are 1) that FeAl2O4 (hercynite) breaks down into its constituent oxides at high pressures and apparently does not have a high-P polymorph (unlike MgAl2O4), 2) the thermodynamic properties of FeAl2O4 are consistent with the earlier values listed by Holland & Powell (1990) with a relatively high S°298 rather than the newer Holland & Powell (1998) formulation, 3) in situ resistivity and diffraction measurements reveal that Fe3O4, magnetite, undergoes a transition to a post-spinel phase with the phase boundary being nearly isobaric at 9.5-10 GPa, 4) the post-spinel phase has a different structure from that previously proposed, 5) a new post-spinel phase is consistent with resistivity measurements, which reveals semiconductor-like behaviour rather than the metallic-like behaviour previously observed for a CaTi2O4-structured polymorph, and 5) the post-spinel phase also occurs in Fe3O4-bearing binary solid solutions with Fe2SiO4 or FeCr2O4, however, the phase relations are more complicated than expected. Determination of the structure of the post-spinel "mystery phase" of Fe3O4 is the subject of continuing study.

Projektbezogene Publikationen (Auswahl)

 
 

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