Journal of the Magnetics Society of Japan
Online ISSN : 1882-2932
Print ISSN : 1882-2924
ISSN-L : 1882-2924
41 巻, 6 号
選択された号の論文の3件中1~3を表示しています
Review Article
  • M. Futamoto, M. Ohtake
    2017 年 41 巻 6 号 p. 108-126
    発行日: 2017年
    公開日: 2017/11/01
    ジャーナル オープンアクセス

      The review covers the research and development of perpendicular media nanostructure focusing on the recording layer. The recording layer material includes the Co-alloys with hcp structure, the magnetic multilayers, and the alloys with ordered structures that have high magneto-crystalline anisotropies (Ku). The technologies of underlayer or interlayer for aligning the easy magnetization axis of magnetic crystal grain perpendicular to the film plane are briefly reviewed including the high Ku magnetic materials for future recording media.

      Observations of compositional and magnetization structures in sub-μm scale have played important roles in improving the recording layer. Typical data on these characteristics are explained in relation to the media structure improvements. Considering that high Ku magnetic materials will be employed in future recording media, basic experimental results related in controlling the easy magnetization axis and in keeping the surface flatness of L10-ordered magnetic materials are explained. Future possibilities for increasing the areal density beyond 1 Tb/in2 by improving the magnetic material and the nanostructure of recording layer are also discussed.

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Hard and Soft Magnetic Materials
  • K. Watanabe, K. Kakizaki, K. Kamishima
    2017 年 41 巻 6 号 p. 127-131
    発行日: 2017年
    公開日: 2017/11/01
    [早期公開] 公開日: 2017/10/17
    ジャーナル オープンアクセス

      We report the synthesis of (Zn2+Ti4+) substituted hexagonal ferrites, BaZn2(Zn0.5Ti0.5)xFe16-xO27 (W-type) and Ba2Zn2(Zn0.5Ti0.5)xFe12-xO22 (Y-type), and the relationship between their composition and magnetic properties. Substituted W-type ferrite was synthesized in the region of 0.0 ≤ x ≤ 1.5. A decrease in the Curie temperature of the W-type phase indicated that the exchange interactions between the Fe3+ ions weakened due to the substitution of Zn2+ and Ti4+ ions. Spontaneous magnetization (σS) at x = 0.5 was similar to that at x = 0.0. This reflects the equal distribution of nonmagnetic Zn2+ and Ti4+ ions to spin down sites and spin up sites, respectively. At x > 0.5, σS decreased clearly, which was possibly caused by a deviation from the collinear arrangement. Substituted Y-type ferrite was also obtained up to x = 0.5. The Y-type phase is more unstable than the W-type phase with respect to this substitution rate.

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