High-pressure magnetic, electronic, and structural properties of MFe2O4 (M=Mg,Zn,Fe) ferric spinels

E. Greenberg, W. M. Xu, M. Nikolaevsky, E. Bykova, G. Garbarino, K. Glazyrin, D. G. Merkel, L. Dubrovinsky, M. P. Pasternak, and G. Kh. Rozenberg
Phys. Rev. B 95, 195150 – Published 23 May 2017
PDFHTMLExport Citation

Abstract

Magnetic, electronic, and structural properties of MFe2O4 (M=Mg,Zn,Fe) ferric spinels have been studied by Fe57 Mössbauer spectroscopy, electrical conductivity, and powder and single-crystal x-ray diffraction (XRD) to a pressure of 120 GPa and in the 2.4–300 K temperature range. These studies reveal for all materials, at the pressure range 25–40 GPa, an irreversible first-order structural transition to the postspinel CaTi2O4 type structure (Bbmm) in which the HS Fe3+ occupies two different crystallographic sites characterized by six- and eightfold coordination polyhedra, respectively. Above 40 GPa, an onset of a sluggish second-order high-to-low spin (HS-LS) transition is observed on the octahedral Fe3+ sites while Fe3+ occupying bicapped trigonal prism sites remain in the HS state. Despite an appreciable resistance decrease, corroborating with the transition to the LS state, MgFe2O4 and ZnFe2O4 remain semiconductors at this pressure range. However, in the case of Fe3O4, the second-order HS-LS transition on the Fe3+ octahedral sites corroborates with a clear trend to a gap closure and formation of a semimetal state above 50 GPa. Above 65 GPa, another structural phase transition is observed in Fe3O4 to a new Pmma structure. This transition coincides with the onset of nonmagnetic Fe2+, signifying further propagation of the gradual collapse of magnetism corroborating with a sluggish metallization process. With this, half of Fe3+ sites remain in the HS state. Thus, this paper demonstrates that, in a material with a complex crystal structure containing transition metal cation(s) in different environments, a HS-LS transition and delocalization/metallization of the 3d electrons does not necessarily occur simultaneously and may propagate through different crystallographic sites at different degrees of compression.

  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
5 More
  • Received 21 March 2017
  • Revised 27 April 2017

DOI:https://doi.org/10.1103/PhysRevB.95.195150

©2017 American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

E. Greenberg1,†, W. M. Xu1, M. Nikolaevsky1,2, E. Bykova3, G. Garbarino4, K. Glazyrin5, D. G. Merkel4,‡, L. Dubrovinsky3, M. P. Pasternak1, and G. Kh. Rozenberg1

  • 1School of Physics and Astronomy, Tel Aviv University, 69978, Tel Aviv, Israel
  • 2Physics Department, Nuclear Research Center Negev, Beer-Sheva 84190, Israel
  • 3Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany
  • 4European Synchrotron Radiation Facility, F-38043 Grenoble Cedex, France
  • 5DESY, Photon Sciences, PETRA-III, P02, Notkestr. 85, Bldg. 47c, Hamburg, Germany

  • *erangre@gmail.com
  • Present address: Center for Advanced Radiation Sources, University of Chicago, Argonne Illinois 60439, USA.
  • On leave from Institute for Particle and Nuclear Physics, Wigner Research Centre for Physics, Hungarian Academy of Sciences, H-1525 Budapest, Hungary.

Article Text (Subscription Required)

Click to Expand

Supplemental Material (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 95, Iss. 19 — 15 May 2017

Reuse & Permissions
Access Options
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review B

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×