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The variation in coercivity was examined by annealing at 60°C cobalt-substituted acicular iron oxides with various Fe2+and cobalt contents. Except for samples containing less than 1 wt% Fe2+, the coercivity increased by the annealing at 60°C, and samples containing more Fe2+showed higher coercivity. The increase of coercivity was attributed to the magnetic anisotropy induced in cobalt-substituted acicular iron oxides, and the existence of Fe2+was considered to facilitate the migration of cobalt ions. The dependence of coercivity on Fe2+content was similar for the samples with 0.5, 1.0, 1.6, and 2.4 wt% cobalt. The coercivity of the samples containing 22-23 wt% Fe2+increased linearly with cobalt content. The coercivity of the samples containing less than 1 wt% Fe2+increased slightly with cobalt content.
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Mikio Kishimoto (1979) studied this question.
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