Electronic and magnetic properties of multiferroic ScFeO available from diffraction experiments.

J Phys Condens Matter

ISIS Facility, STFC Oxfordshire, OX11 0QX, United Kingdom. Diamond Light Source Ltd, Oxfordshire, OX11 0DE, United Kingdom.

Published: November 2017

AI Article Synopsis

  • The electronic and magnetic properties of ferric ions in ScFeO differ significantly from BiFeO, raising important questions about their behavior in multiferroics.
  • Studies on resonant x-ray diffraction can help clarify the nature of ferric ions, particularly whether they are in a high-spin state, which would influence their magnetic properties.
  • Additionally, the analysis of magnetic neutron diffraction suggests that conventional interpretations may be insufficient if ferric ions are not in a high-spin state, revealing more complex scattering behaviors than just dipole moments.

Article Abstract

Electronic and magnetic properties of ferric ions (3d ) in multiferroic ScFeO are puzzling, in part because they are different from the only other multiferroic known to possess the same polar chemical structure, BiFeO. Open questions about ScFeO can be addressed by confronting observations with results for G-type antiferromagnetism allowed by the lithium niobate (LiNbO)-like parent R3c structure. Calculated structure factors for resonant x-ray diffraction include all charge-like quadrupoles allowed by symmetry, and if experimental results for ScFeO subsequently imply they are different from zero then ferric ions cannot be in the high-spin S state. The same type of experiment can reveal the moment direction in the G-type antiferromagnetism, according to our calculations, and thereby contribute to understanding magnetic anisotropy. Furthermore, structure factors for magnetic neutron diffraction by ScFeO include Dirac multipoles that are time-odd and parity-odd, e.g. dipoles that are often called anapoles or toroidal moments. Apart from Dirac multipoles, the conventional approach to the interpretation of neutron Bragg diffraction data will be inadequate if ferric ions (Fe) are not in the high-spin S state, because the scattering amplitude includes more than simple dipole moments in the general case.

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http://dx.doi.org/10.1088/1361-648X/aa860fDOI Listing

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