Author
Listed:
- J. A. Sans
(Universitat Politècnica de València)
- V. Monteseguro
(European Radiation Synchrotron Facility
Universitat de València)
- G. Garbarino
(European Radiation Synchrotron Facility)
- M. Gich
(Institut de Ciència de Materials de Barcelona (ICMAB-CSIC))
- V. Cerantola
(European Radiation Synchrotron Facility)
- V. Cuartero
(European Radiation Synchrotron Facility
Centro Universitario de la Defensa de Zaragoza)
- M. Monte
(European Radiation Synchrotron Facility)
- T. Irifune
(Ehime University, 2–5 Bunkyo-cho
Earth-Life Science Institute, Tokyo Institute of Technology)
- A. Muñoz
(MALTA Consolider Team, Universidad de La Laguna)
- C. Popescu
(ALBA-CELLS)
Abstract
Iron oxides are among the major constituents of the deep Earth’s interior. Among them, the epsilon phase of Fe2O3 is one of the less studied polymorphs and there is a lack of information about its structural, electronic and magnetic transformations at extreme conditions. Here we report the precise determination of its equation of state and a deep analysis of the evolution of the polyhedral units under compression, thanks to the agreement between our experiments and ab-initio simulations. Our results indicate that this material, with remarkable magnetic properties, is stable at pressures up to 27 GPa. Above 27 GPa, a volume collapse has been observed and ascribed to a change of the local environment of the tetrahedrally coordinated iron towards an octahedral coordination, finding evidence for a different iron oxide polymorph.
Suggested Citation
J. A. Sans & V. Monteseguro & G. Garbarino & M. Gich & V. Cerantola & V. Cuartero & M. Monte & T. Irifune & A. Muñoz & C. Popescu, 2018.
"Stability and nature of the volume collapse of ε-Fe2O3 under extreme conditions,"
Nature Communications, Nature, vol. 9(1), pages 1-11, December.
Handle:
RePEc:nat:natcom:v:9:y:2018:i:1:d:10.1038_s41467-018-06966-9
DOI: 10.1038/s41467-018-06966-9
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