Abstract
Collinear and canted magnetic motifs in hematite were investigated by J. Kokubun et al. [Phys. Rev. B 78, 115112 (2008)] using x-ray Bragg diffraction magnified at the iron -edge, and analyses of observations led to various potentially interesting conclusions. We demonstrate that the reported analyses for both nonresonant and resonant magnetic diffraction at low energies near the absorption -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 centers of inversion symmetry are parity-odd atomic multipoles, time-even (polar) and time-odd (magneto-electric), that arise from enhancement by the electric-dipole ()–electric-quadrupole () event. Analyses of azimuthal-angle scans on two space-group forbidden reflections, hexagonal and , collected by Kokubun [Phys. Rev. B 78, 115112 (2008)] above and below the Morin temperature K), allow us to obtain good estimates of contributing polar and magnetoelectric multipoles, including the iron anapole. We show, beyond reasonable doubt, that available data are inconsistent with parity-even events only (- and -). For future experiments, we show that chiral states of hematite couple to circular polarization and differentiate - and - events, while the collinear motif supports magnetic charges.
- Received 8 October 2010
DOI:https://doi.org/10.1103/PhysRevB.83.054427
©2011 American Physical Society