Simultaneous gamma, x-ray, and electron Mössbauer spectroscopy of the volume and surface magnetic structure of hexagonal M-ferrites

Direct comparative studies are made between the magnetic structures of a surface layer of thickness ～40 nm and the bulk magnetic structure of ferromagnetic single crystals of hexagonal M ferrites (BaFe₁₂O₁₉, SrFe₁₂O₁₉, PbFe₁₂O₁₉) with a magneto-plumbite structure. Measurements are made by simultaneous gamma, x-ray, and electron Mössbauer spectroscopy in order to investigate the properties of the surface layer and the bulk crystal simultaneously. Experimental data obtained with a depth resolution of ～ 10 nm show that the orientation of the magnetic moments of the iron ions (along the crystallographic c axis) does not change on approaching the surface from the crystal volume. Thus, to within an experimental error of ～ 10 nm, single crystals of the hexagonal ferrites BaFe₁₂O₁₉, SrFe₁₂O₁₉, and PbFe₁₂O₁₉ with a ferromagnetic structure do not have a “ transition” surface layer whose magnetic structure differs from that of the bulk crystal such as that which exists, with a depth of several hundred nm, in antiferromagnetic materials with weak ferromagnetism.