Pressure-induced FeCu cationic valence exchange and its structural consequences: High-pressure studies of delafossite CuFeO2

W. M. Xu, G. Kh. Rozenberg, M. P. Pasternak, M. Kertzer, A. Kurnosov, L. S. Dubrovinsky, S. Pascarelli, M. Munoz, M. Vaccari, M. Hanfland, and R. Jeanloz
Phys. Rev. B 81, 104110 – Published 17 March 2010

Abstract

The present high-pressure studies of CuFeO2 to 30 GPa using x-ray diffraction, along with F57e Mössbauer and Fe and CuK-edge x-ray absorption spectroscopy methods, reveal a sequence of intricate structural/electronic-magnetic pressure-induced transitions. The low-pressure R3¯m structure (0–18 GPa) is composed of sheets of FeS=5/23+ ions alternating with layers of O-CuS=01+-O dumbbells, the latter oriented along the c axis. This structure is characterized by an unusual positive d(c/a)/dP. At 18 GPa a structural transition takes place to a more isotropic C2/c structure with the O-CuS=01+-O axis tilted 28° from the c axis and with negative d(c/a)/dP. This transition corroborates with the onset of long-range antiferromagnetic order. Starting at 23GPa, with an initial volume reduction in |ΔV/V0|=0.16, the Cu-Fe bands overlap and this leads to a (CuS=01+FeS=5/23+)(CuS=1/22+FeS=22+) interionic valence exchange in about 1/3 of the C2/c-CuFeO2 at 27 GPa. As a result: (i) the Cu2+-O becomes fourfold coordinated and is in a new crystallographic structure with space group P3¯m, and (ii) the Néel temperature increases above twofold [TN(CuS=1/22+FeS=22+)2.2TN(CuS=01+FeS=5/23+)]. This sequence of transitions is reversible with minimal hysteresis.

  • Figure
  • Figure
  • Figure
  • Figure
  • Received 20 August 2009

DOI:https://doi.org/10.1103/PhysRevB.81.104110

©2010 American Physical Society

Authors & Affiliations

W. M. Xu1, G. Kh. Rozenberg1, M. P. Pasternak1, M. Kertzer1, A. Kurnosov2, L. S. Dubrovinsky2, S. Pascarelli3, M. Munoz3, M. Vaccari3, M. Hanfland3, and R. Jeanloz4

  • 1School of Physics and Astronomy, Tel-Aviv University, Ramat-Aviv, 69997 Tel Aviv, Israel
  • 2Bayerisches Geoinstitut, University Bayreuth, D-95440 Bayreuth, Germany
  • 3European Synchrotron Radiation Facility, BP 220, 38043 Grenoble, France
  • 4Department of Earth and Planetary Science, University of California, Berkeley, California 94720, USA

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 81, Iss. 10 — 1 March 2010

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
×