Orbital magnetic moments in FeCr2S4 studied by x-ray magnetic circular dichroism

Fuente: arXiv
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Main Authors: Verma, V. K., Patra, J., Singh, V. R., Nonaka, Y., Shibata, G., Ishigami, K., Tanaka, A., Ohgushi, K., Tokura, Y., Koide, T., Fujimori, A.
Format: Preprint
Published: 2025
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author Verma, V. K.
Patra, J.
Singh, V. R.
Nonaka, Y.
Shibata, G.
Ishigami, K.
Tanaka, A.
Ohgushi, K.
Tokura, Y.
Koide, T.
Fujimori, A.
author_facet Verma, V. K.
Patra, J.
Singh, V. R.
Nonaka, Y.
Shibata, G.
Ishigami, K.
Tanaka, A.
Ohgushi, K.
Tokura, Y.
Koide, T.
Fujimori, A.
contents We have investigated the element specific magnetic characteristics of single-crystal FeCr2S4 using x-ray absorption spectroscopy (XAS) and x-ray magnetic circular dichroism (XMCD). We have found that the Fe L2,3-edge XAS spectra do not exhibit clear multiplet structures, indicating strong hybridization between the Fe 3d and S 3p orbitals, leading to delocalized rather than localized electronic states. The Fe 3d and Cr 3d spin moments are antiferromagnetically coupled, consistent with the Goodenough-Kanamori rule. The orbital magnetic moments of Fe and Cr are determined to be -0.23 and -0.017 μB/ion, respectively. The large orbital magnetic moment of Fe is due to the d6 configuration under the relatively weak tetrahedra crystal field at the Fe site, and the delocalized Fe electrons maintain the orbital degree of freedom in spite of their itinerant nature. To understand phenomena such as the gigantic Kerr rotation, it is essential to consider not only the orbital degrees of freedom but also the role of spin-orbit coupling, which induces a finite orbital magnetic moment through t2 and e level hybridization under the tetrahedral crystal field. This finite orbital moment serves as a direct indicator of spin-orbit interaction strength and links element-specific orbital magnetism to the large Kerr rotation. On the other hand, the octahedral crystal-field splitting of the Cr 3d level is large enough to result in the quenching of the orbital moment of the Cr ion in FeCr2S4.
format Preprint
id arxiv_https___arxiv_org_abs_2508_14428
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Orbital magnetic moments in FeCr2S4 studied by x-ray magnetic circular dichroism
Verma, V. K.
Patra, J.
Singh, V. R.
Nonaka, Y.
Shibata, G.
Ishigami, K.
Tanaka, A.
Ohgushi, K.
Tokura, Y.
Koide, T.
Fujimori, A.
Strongly Correlated Electrons
We have investigated the element specific magnetic characteristics of single-crystal FeCr2S4 using x-ray absorption spectroscopy (XAS) and x-ray magnetic circular dichroism (XMCD). We have found that the Fe L2,3-edge XAS spectra do not exhibit clear multiplet structures, indicating strong hybridization between the Fe 3d and S 3p orbitals, leading to delocalized rather than localized electronic states. The Fe 3d and Cr 3d spin moments are antiferromagnetically coupled, consistent with the Goodenough-Kanamori rule. The orbital magnetic moments of Fe and Cr are determined to be -0.23 and -0.017 μB/ion, respectively. The large orbital magnetic moment of Fe is due to the d6 configuration under the relatively weak tetrahedra crystal field at the Fe site, and the delocalized Fe electrons maintain the orbital degree of freedom in spite of their itinerant nature. To understand phenomena such as the gigantic Kerr rotation, it is essential to consider not only the orbital degrees of freedom but also the role of spin-orbit coupling, which induces a finite orbital magnetic moment through t2 and e level hybridization under the tetrahedral crystal field. This finite orbital moment serves as a direct indicator of spin-orbit interaction strength and links element-specific orbital magnetism to the large Kerr rotation. On the other hand, the octahedral crystal-field splitting of the Cr 3d level is large enough to result in the quenching of the orbital moment of the Cr ion in FeCr2S4.
title Orbital magnetic moments in FeCr2S4 studied by x-ray magnetic circular dichroism
topic Strongly Correlated Electrons
url https://arxiv.org/abs/2508.14428