Parity-odd multipoles, magnetic charges and chirality in haematite (alfa-Fe2O3)
S. W. Lovesey, A. Rodriguez-Fernandez, J. A. Blanco

TL;DR
This paper revises the analysis of magnetic diffraction in haematite, emphasizing the importance of parity-odd multipoles and demonstrating the presence of chiral states and magnetic charges through resonant x-ray diffraction.
Contribution
It introduces a new formulation for analyzing magnetic x-ray diffraction that incorporates parity-odd multipoles, challenging previous analyses and providing clearer insights into haematite's magnetic structure.
Findings
Parity-odd multipoles are essential for accurate diffraction analysis.
Data indicate the presence of chiral states and magnetic charges in haematite.
Analysis shows inconsistency with only parity-even events in previous models.
Abstract
Collinear and canted magnetic motifs in haematite were investigated by Kokubun et al. (2008) using x-ray Bragg diffraction magnified at the iron K-edge, and analyses of observations led to various potentially interesting conclusions. We demonstrate that the reported analyses for both non-resonant and resonant magnetic diffraction at low energies near the absorption K-edge are not appropriate. In its place, we apply a radically different formulation, thoroughly tried and tested, that incorporates all magnetic contributions to resonant x-ray diffraction allowed by the established chemical and magnetic structures. Essential to a correct formulation of diffraction by a magnetic crystal with resonant ions at sites that are not centres of inversion symmetry are parity-odd atomic multipoles, time-even (polar) and time-odd (magneto-electric), that arise from enhancement by the electric-dipole…
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