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Perpendicular magnetic anisotropy of iron-intercalated transition-metal disulfides studied by X-ray magnetic circular dichroism

Shibata, Goro 

Layered transition-metal dichalcogenides with the 1T-CdI$$_2$$-type crystal structure are known to exhibit a wide variety of electric and magnetic properties by intercalating various transition-metal atoms of different concentrations between adjacent layers. Among them, iron-intercalated titanium disulfides Fe$$_x$$TiS$$_2$$ and tantalum disulfides Fe$$_x$$TaS$$_2$$ are ferromagnets which exhibits strong perpendicular magnetic anisotropy (PMA) with large coercive fields of a few tesla. It is reported that Fe$$_x$$TaS$$_2$$ shows stronger PMA than Fe$$_x$$TiS$$_2$$, presumably due to the stronger spin-orbit interaction (SOI) of Ta. In the present study, in order to elucidate the microscopic origin of the strong PMA in these compounds, the electronic structure and magnetism of single-crystalline Fe$$_x$$TiS$$_2$$ and Fe$$_x$$TaS$$_2$$ have been investigated via X-ray absorption spectroscopy (XAS) and X-ray magnetic circular dichroism (XMCD). From the spectral line shapes of XAS and XMCD, the valence of Fe is shown to be essentially 2+, whereas Ti is in an itinerant electronic state between 3+ and 4+. This shows that electrons are doped from the intercalated Fe atoms into the host TiS$$_2$$ and TaS$$_2$$. Notably, clear differences in the spectral line shapes of XMCD at the Fe $$L_{2,3}$$ edges are observed between Fe$$_x$$TiS$$_2$$ and Fe$$_x$$TaS$$_2$$ despite the similarity of the crystal structures. This may be attributed to the different SOI strength between these compounds. Based on the configuration-interaction cluster-model calculations, the observed changes in the spectral line shapes can be qualitatively reproduced by virtually increasing SOI of Fe 3$$d$$ electrons.

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