Large Orbital Magnetic Moment and Strong Perpendicular Magnetic Anisotropy in Heavily Intercalated FeTiS
arXiv:2103.09538 · doi:10.1021/acs.jpcc.1c02345
Abstract
Titanium disulfide TiS, which is a member of the layered transition-metal dichalcogenides with the 1T-CdI-type crystal structure, is known to exhibit a wide variety of magnetism through intercalating various kinds of transition-metal atoms of different concentrations. Among them, Fe-intercalated titanium disulfide FeTiS is known to be ferromagnetic with strong perpendicular magnetic anisotropy (PMA) and large coercive fields (). In order to study the microscopic origin of the magnetism of this compound, we have performed X-ray absorption spectroscopy (XAS) and X-ray magnetic circular dichroism (XMCD) measurements on single crystals of heavily intercalated FeTiS (). The grown single crystals showed a strong PMA with a large of . XAS and XMCD spectra showed that Fe is fully in the valence states of 2+ and that Ti is in an itinerant electronic state, indicating electron transfer from the intercalated Fe atoms to the host TiS bands. The Fe ions were shown to have a large orbital magnetic moment of , to which, combined with the spin-orbit interaction and the trigonal crystal field, we attribute the strong magnetic anisotropy of FeTiS.
24 pages, 8 figures