Noncollinear ordering of the orbital magnetic moments in magnetite

The magnitude of the orbital magnetic moment and its role as a trigger of the Verwey transition in the prototypical Mott insulator, magnetite, remain contentious. Using 1s2p resonant inelastic x-ray scattering angle distribution (RIXS-AD), we prove the existence of noncollinear orbital magnetic orde...

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Main Authors: Elnaggar, Hebatalla (Author) , Haverkort, Maurits W. (Author)
Format: Article (Journal)
Language:English
Published: 12 November 2019
In: Physical review letters
Year: 2019, Volume: 123, Issue: 20
ISSN:1079-7114
DOI:10.1103/PhysRevLett.123.207201
Online Access:Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1103/PhysRevLett.123.207201
Verlag, lizenzpflichtig, Volltext: https://link.aps.org/doi/10.1103/PhysRevLett.123.207201
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Author Notes:H. Elnaggar, Ph. Sainctavit, A. Juhin, S. Lafuerza, F. Wilhelm, A. Rogalev, M.-A. Arrio, Ch. Brouder, M. van der Linden, Z. Kakol, M. Sikora, M.W. Haverkort, P. Glatzel, and F.M.F. de Groot

MARC

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520 |a The magnitude of the orbital magnetic moment and its role as a trigger of the Verwey transition in the prototypical Mott insulator, magnetite, remain contentious. Using 1s2p resonant inelastic x-ray scattering angle distribution (RIXS-AD), we prove the existence of noncollinear orbital magnetic ordering and infer the presence of dynamical distortion creating a polaronic precursor for the metal to insulator transition. These conclusions are based on a subtle angular shift of the RIXS-AD spectral intensity as a function of the magnetic field orientation. Theoretical simulations show that these results are only consistent with noncollinear magnetic orbital ordering. To further support these claims we perform Fe K-edge x-ray magnetic circular dichroism in order to quantify the Fe average orbital magnetic moment. 
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