A critical re-examination of resonant soft x-ray Bragg forbidden reflections in magnetite
S.B. Wilkins, S. Di Matteo, T.A.W. Beale, Y. Joly, C. Mazzoli, P.D., Hatton, P. Bencok, F. Yakhou, V.A.M. Brabers

TL;DR
This study re-examines resonant soft x-ray diffraction in magnetite, demonstrating that observed forbidden reflections are due to structural displacements, challenging previous claims of charge and orbital ordering.
Contribution
The paper provides a critical re-analysis showing that forbidden reflections can be explained without invoking charge or orbital order, questioning prior interpretations.
Findings
Forbidden reflection intensity explained by structural displacements
Resonant soft x-ray sensitivity insufficient to confirm charge/orbital order
Challenges previous claims of ordering based on diffraction data
Abstract
Magnetite, FeO, displays a highly complex low temperature crystal structure that may be charge and orbitally ordered. Many of the recent experimental claims of such ordering rely on resonant soft x-ray diffraction at the oxygen K and iron L edges. We have re-examined this system and undertaken soft x-ray diffraction experiments on a high-quality single crystal. Contrary to previous claims in the literature, we show that the intensity observed at the Bragg forbidden (001/2) reflection can be explained purely in terms of the low-temperature structural displacements around the resonant atoms. This does not necessarily mean that magnetite is not charge or orbitally ordered, but rather that the present sensitivity of resonant soft x-ray experiments does not allow conclusive demonstration of such ordering.
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