Abstract
A direct comparison of the magnetic structures of a surface layer and of the bulk of Ba-M-type hexagonal ferrites with iron ions partially replaced by Sc diamagnetic ions (BaFe12−x ScxO19) has been made by simultaneous Mössbauer spectroscopy with detection of gamma rays, characteristic x-ray emission, and electrons. It has been found that, if the magnetic lattice of a Ba-M-type hexagonal ferrite is weakly diluted by Sc diamagnetic ions, a ∼300-nm thick macroscopic layer forms on the surface of a BaFe11.4Sc0.6O19 crystal, in which the iron-ion magnetic moments are noncollinear with the moments in the bulk. The noncollinear magnetic structure forms in the near-surface layer of BaFe12−x ScxO19 crystals because the exchange interaction energy is additionally reduced by the presence of such a “defect” as the surface. This is the first observation in ferromagnetic crystals of an anisotropic surface layer whose magnetic properties, as predicted by Néel, differ from those of the bulk.
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Fiz. Tverd. Tela (St. Petersburg) 41, 483–490 (March 1999)
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Kamzin, A.S., Rozenbaum, V.L. & Ol’khovik, L.P. Mössbauer studies of the surface and bulk magnetic structure of scandium-substituted Ba-M-type hexaferrites. Phys. Solid State 41, 433–439 (1999). https://doi.org/10.1134/1.1130797
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DOI: https://doi.org/10.1134/1.1130797