Equation of state of the high-pressure Fe3O4 phase and a new structural transition at 70 GPa

Angèle Ricolleau (1) , Yingwei Fei (2)

1 CINaM - Centre Interdisciplinaire de Nanoscience de Marseille
2 Geophysical Laboratory [Carnegie Institution]

We have investigated the high-pressure behavior of Fe3O4 by in situ X-ray diffraction measurements from 11 to 103 GPa. Up to 70 GPa, the previous observed high-pressure Fe3O4 phase (h-Fe3O4) is stable, with a CaTi2O4-type structure. The compression curve shows an abnormal volume contraction at about 50 GPa, likely associated with the magnetic moment collapse observed at that pressure. Fitting the compression data up to 45 GPa to the Birch-Murnaghan equation of state yields a bulk modulus, K-T0 = 172 GPa, and V-0 = 277 angstrom(3), with fixed K' = 4. At a pressure between 64 and 73 GPa, a new structural transition was observed in Fe3O4, which can be attributed to a martensitic transformation as described by Yamanaka et al. (2008) for post-spinel structural transition. The diffraction data can be best fitted with a Pnma space group. No breakdown of Fe3O4 was observed up to at least 103 GPa. The new high-pressure polymorph is about 6% denser than the h-Fe3O4 phase at 75 GPa.

Domaines: Minéralogie

Angèle Ricolleau, Yingwei Fei. Equation of state of the high-pressure Fe3O4 phase and a new structural transition at 70 GPa. The American Mineralogist, 2016, 101 (3-4), pp.719-725. ⟨10.2138/am-2016-5409⟩. ⟨hal-01452048⟩