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    코발트 훼라이트 에피탁시얼 산화철의 생성과 자기특성(Ⅰ)

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    https://www.riss.kr/link?id=A76075300

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    To improve the coercivity of γ-Fe₂O₃ particles. We have made cobalt ferrite epitaxial γ-Fe₂O₃ particles by crystallizing cobalt ferrite on the surface of γ-Fe₂O₃ particles. The coercivity of Co_xFe_(3-x)O₄ which is conform to coating layer showed the most superior characteristic when the value of x was 1. On the formation of cobalt epitaxial γ-Fe₂O₃ particles, controlling reaction atmosphere as oxidation atmosphere after non-oxidation atmosphere was the optimum condition to prepare cobalt epitaxial γ-Fe₂O₃ particles with superior magnetic properties. Epitaxial growth of cobalt ferrite on the surface of γ-Fe₂O₃ particles was accomplished at 90℃ for 30 minutes.
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    To improve the coercivity of γ-Fe₂O₃ particles. We have made cobalt ferrite epitaxial γ-Fe₂O₃ particles by crystallizing cobalt ferrite on the surface of γ-Fe₂O₃ particles. The coercivity of Co_xFe_(3-x)O₄ which is conform to coating ...

    To improve the coercivity of γ-Fe₂O₃ particles. We have made cobalt ferrite epitaxial γ-Fe₂O₃ particles by crystallizing cobalt ferrite on the surface of γ-Fe₂O₃ particles. The coercivity of Co_xFe_(3-x)O₄ which is conform to coating layer showed the most superior characteristic when the value of x was 1. On the formation of cobalt epitaxial γ-Fe₂O₃ particles, controlling reaction atmosphere as oxidation atmosphere after non-oxidation atmosphere was the optimum condition to prepare cobalt epitaxial γ-Fe₂O₃ particles with superior magnetic properties. Epitaxial growth of cobalt ferrite on the surface of γ-Fe₂O₃ particles was accomplished at 90℃ for 30 minutes.

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