DocumentCode
763586
Title
Evolution With Temperature of the Magnetic Anisotropy of Ba Ferrite Particles
Author
Bottoni, Giancarlo
Author_Institution
Dipt. di Fisica, Ferrara Univ.
Volume
42
Issue
10
fYear
2006
Firstpage
2309
Lastpage
2311
Abstract
The magnetic anisotropy of pure and Co/Ti-doped Ba ferrite particles is analyzed through the evaluation of the dependence on temperature of the constants of magnetocrystalline and shape anisotropy, which both are present in the platelet-like Ba ferrite particles with hexagonal structure. In undoped Ba ferrite, the magnetocrystalline anisotropy constant is predominant on the conflicting shape anisotropy constant at all temperatures, which indicates that the magnetic anisotropy is uniaxial, with preferred direction for the magnetization along the c axis of the hexagonal particles. In doped particles, where the magnetocrystalline anisotropy is weakened by the ionic substitutions, while at high temperatures the magnetic anisotropy is substantially uniaxial with c as axis of easy magnetization, when the temperature decreases, the shape anisotropy constant becomes larger than the magnetocrystalline anisotropy constant, and consequently, the magnetic anisotropy is not uniaxial, but it presents multiple preferred directions for the magnetization
Keywords
cobalt alloys; ferrites; magnetic anisotropy; magnetic particles; titanium alloys; Co-Ti-Ba; barium ferrite particles; doping effect; hexagonal particles; hexagonal structure; magnetic anisotropy; magnetic recording; magnetization; magnetocrystalline anisotropy; shape anisotropy; Anisotropic magnetoresistance; Crystallization; Ferrites; Magnetic analysis; Magnetic anisotropy; Perpendicular magnetic anisotropy; Perpendicular magnetic recording; Saturation magnetization; Shape; Temperature dependence; Ba ferrite particles; Co/Ti-doping effect; magnetic anisotropy; magnetic recording;
fLanguage
English
Journal_Title
Magnetics, IEEE Transactions on
Publisher
ieee
ISSN
0018-9464
Type
jour
DOI
10.1109/TMAG.2006.878660
Filename
1704282
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