The influence of annealing atmosphere on magnetic properties of Fe
78.5B
13Si
8.5 amorphous alloy has been studied. Annealing in N
2, Ar, H
2 and N
2+20%O
2 atmospheres improved significantly the iron loss of the rapidly quenched amorphous ribbon, being much better than that after annealing in H
2+H
2O atmosphere. The purpose of this paper is to make clear the mechanism of this deleterious effect of annealing in a H
2O containing atmosphere.
According to infrared reflection spectra of the Fe
78.5B
13Si
8.5 amorphous alloy ribbon annealed in the H
2+H
2O atmosphere, boron in the alloy is found to be oxidized selectively to form B
2O
3 film with the thickness of several 10 nm on the ribbon surface.
Auger electron spectroscopy analysis shows that any depletion zone is not formed on the ribbon surface after annealing in the N
2, Ar, H
2 and N
2+O
2 atmospheres. On the other hand, the boron-depletion zone is detected under the oxide film formed during annealing in H
2+H
2O. The alloy composition in this boron-depletion zone is approximately 0-3 mol%B and 9-11 mol%Si, that suggests a significant decrease of the crystallization temperature.
The α-Fe crystalline phase is detected only on the ribbon surface after annealing in the H
2+H
2O atmosphere by means of thin film X-ray diffraction.
We propose the mechanism on the deleterious effect of annealing in the H
2+H
2O atmosphere that H
2O in the atmosphere oxidizes selectively boron in the amorphous alloy to form B
2O
3 film and the boron-depletion zone, and then the alloy in this zone is crystallized into α-Fe, and this surface crystalline layer induces the perpendicular magnetic anisotropy in the amorphous alloy to deteriorate the iron loss.
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