Electric-field-induced X-ray Nonreciprocal Dichroism in Hematite
Takeshi Hayashida, Koei Matsumoto, Keito Arakawa, Yves Joly, Sergio Di Matteo, Kenji Tamasaku, Yoshikazu Tanaka, and Tsuyoshi Kimura

TL;DR
This study demonstrates how applying an electric field to hematite induces nonreciprocal x-ray dichroism, revealing higher-order magnetic multipoles and providing a new way to probe hidden magnetic symmetries.
Contribution
The paper introduces electric-field-induced x-ray nonreciprocal dichroism as a method to detect higher-order magnetic multipoles in antiferromagnets, supported by ab-initio simulations.
Findings
Electric field induces nonreciprocal x-ray dichroism in hematite.
The response is linked to magnetic quadrupole and toroidal octupole moments.
Simulations match experimental spectra and reveal multipole origins.
Abstract
Hematite (alpha-Fe2O3) is a prototypical room temperature antiferromagnet whose time-reversal-odd magnetic structure has recently attracted renewed attention. While such magnetic symmetry can be characterized in terms of higher-order multipoles beyond the magnetic dipole, their manifestation in measurable physical phenomena has remained largely elusive. In this work, we investigate x-ray absorption near the Fe K-edge of hematite under an applied electric field, which explicitly breaks space-inversion symmetry. We observe an electric-field-induced x-ray nonreciprocal linear dichroism (E-induced XNLD) that reflects the time-reversal-odd nature of the magnetic order. Numerical simulations based on ab-initio density functional theory reproduce the observed spectra, including their dependence on the antiferromagnetic domain and x-ray polarization. Furthermore, a symmetry-resolved multipole…
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Taxonomy
TopicsIron oxide chemistry and applications · Magnetic Properties and Synthesis of Ferrites · Multiferroics and related materials
