H. Stepankova et al., HYPERFINE FIELD ANISOTROPY IN YIG WITH DIAMAGNETIC IMPURITIES, Journal of magnetism and magnetic materials, 177, 1998, pp. 239-240
The Fe-57 NMR spectra of pure yttrium iron garnet, measured at 4.2 K,
exhibit a well-resolved satellite structure caused by antisite defects
(yttrium ions replacing iron on a sites). The analysis of the a site
spectra, obtained in a magnetic field of 0.75 T applied in several dir
ections in the (1 1 0) plane, yielded the values of the isotropic and
anisotropic terms of the hyperfine held for four resolved satellite se
ts. (C) 1998 Elsevier Science B.V. All rights reserved.