Abstract

Ferrimagnetic resonance was experimentally studied in single crystals of gadolinium iron garnet at 24,000 Mc in the vicinity of the magnetic compensation point at Tc = + 13 C. The two modes of resonance corresponding to the normal and abnormal directions of precession of the coupled Fe and Gd sublattices were observed and the results compared with a theory which includes the effect of the susceptibility of the Gd. From these measurements, the exchange field at T/sub c/ was found to be 231,000 Oe, in excellent agreement with magnetization data. In addition, information on (g/sub Fe/ g/sub Gd/) and the crystalline anisotropy were obtained. In a one degree region around the compensation temperature additional modes of resonance were observed. Each of these resonances corresponds to the Fe and Gd sublattices aligned along a (111) direction which is not parallel to the external magnetic field. (auth)

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