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

TL;DR

This study uses x-ray magnetic circular dichroism to analyze element-specific magnetic moments in FeCr2S4, revealing strong hybridization, antiferromagnetic coupling, and significant orbital moments in Fe linked to spin-orbit interactions.

Contribution

First detailed element-specific analysis of orbital magnetic moments in FeCr2S4 using XMCD, highlighting the role of hybridization and spin-orbit coupling in its magnetic properties.

Findings

Fe exhibits a large orbital magnetic moment due to d6 configuration.

Cr orbital moment is quenched by crystal field splitting.

Strong hybridization influences magnetic behavior.

Abstract

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 {\mu}B/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.