Nuclear Magnetic Resonance (NMR) of Mn 55 associated with the Mn 3+ ion at the octahedral site in its magnetically ordered state has been studied on manganese ferrite of cubic phase. Using a single crystal sample, the large anisotropic hyperfine field of +115 kOe, in addition to the isotropic hyperfine field of -360 kOe, has been observed, which is characteristic of the Mn 3+ ion at the octahedral site with the Jahn-Teller distortion. These two values of the hyperfine fields are consistent both with the theoretically calculated values and with the data of the hyperfine coupling constants of the paramagnetic Mn 3+ ion. It was found that the ground state of the Mn 3+ ion at the octahedral site was of B 1 g type and that the directions of tetragonal axes (Jahn-Teller axes) were three equivalent <100> axes. In connection with the unsuccessful observation of the quadrupole-splitted lines, which are also characteristic of NMR in the MN 3+ ion, the effects and the origins of the lower symmetry crystalline fields are discussed.
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Kubo et al. (1969) studied this question.
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