X-ray scattering study of the order parameters in multiferroic TbMnO3

D. Mannix, D. F. McMorrow, R. A. Ewings, A. T. Boothroyd, D. Prabhakaran, Y. Joly, B. Janousova, C. Mazzoli, L. Paolasini, and S. B. Wilkins
Phys. Rev. B 76, 184420 – Published 16 November 2007

Abstract

We report on an extensive investigation of the multiferroic compound TbMnO3 using x-ray scattering techniques. Nonresonant x-ray magnetic scattering (NRXMS) was used to characterize the domain population of the single crystal used in our experiments. This revealed that the dominant domain is overwhelmingly A type. The temperature dependence of the intensity and wave vector associated with the incommensurate magnetic order was found to be in good agreement with neutron scattering data. X-ray resonant scattering experiments were performed in the vicinity of the Mn K and Tb L3 edges in the high-temperature collinear phase, the intermediate temperature cycloidal and ferroelectric phase, and the low-temperature phase. In the collinear phase, where according to neutron diffraction only the Mn sublattice is ordered, resonant E1E1 satellites were found at the Mn K edge associated with A-type but also F-type peaks. Detailed measurements of the azimuthal dependence of the F-type satellites (and their absence in the NRXMS experiments) leads us to conclude that they are most likely nonmagnetic in origin. We suggest instead that they may be associated with an induced charge multipole. At the Tb L3 edge, resonant A- and F-type satellites were observed in the collinear phase again associated with E1E1 events. We attribute these to a polarization of the Tb5d states by the ordering of the Mn sublattice. On cooling into the cycloidal and ferroelectric phase, a new set of resonant satellites appear corresponding to C-type order. These appear at the Tb L3 edge only. In addition to a dominant E1E1 component in the σπ channel, a weaker component is found in the preedge with σσ polarization and displaced by 7eV with respect to the E1E1 component. Comprehensive calculations of the x-ray scattering cross section were performed using the FDMNES code. These calculations show that the unrotated σσ component of the Tb L3 C-type peaks appearing in the ferroelectric phase contains a contribution from a multipole that is odd with respect to both space and time, known in various contexts as the anapole. Our experiments thus provide tentative evidence for the existence of a type of anapolar order parameter in the rare-earth manganite class of mulitferroic compounds.

  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
13 More
  • Received 18 May 2007

DOI:https://doi.org/10.1103/PhysRevB.76.184420

©2007 American Physical Society

Authors & Affiliations

D. Mannix1, D. F. McMorrow2,3, R. A. Ewings4, A. T. Boothroyd4, D. Prabhakaran4, Y. Joly5, B. Janousova6, C. Mazzoli6, L. Paolasini6, and S. B. Wilkins6

  • 1XMaS CRG Beamline, European Synchrotron Radiation Facility, F-38043 Grenoble, France
  • 2London Centre for Nanotechnology and Department of Physics and Astronomy, University College London, United Kingdom
  • 3ISIS Facility, Rutherford Appleton Laboratory, Chilton, Didcot OX11 0QX, United Kingdom
  • 4Department of Physics, Clarendon Laboratory, University of Oxford, Oxford, United Kingdom
  • 5CNRS-Grenoble, Grenoble, France
  • 6European Synchrotron Radiation Facility, F-38043 Grenoble, France

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 76, Iss. 18 — 1 November 2007

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
×