1972 年 33 巻 1 号 p. 70-76
Magnetocrystalline anisotropy K1 and induced magnetic anisotropy Ku of Fe–Al single crystals containing about 20 at. % Al were measured with a torque meter. The K1 of the 21.0 at. % Al alloy showed negative magnetic field dependence in high field, and the value of K1 showed a maximum at 360 K. The behavior of K1 is explained on the basis that a specimen is in a two-phase state, one of which is disordered matrix having positive K1 and the other is precipitated Fe3Al phase having negative K1. The deviation of Ku from directional order theory is explained by assuming that the shape anisotropy of Fe3Al particles plays an important role.
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