The NMR spectra of 57Fe in Pr :YIG, Nd : YIG and Yb :YIG were measured on polycrystalline samples at 4.2 K in the zero external field. In the NMR spectra of both tetrahedral and octahedral sites the resolved satellite structure appears. This structure is caused by the change of the hyperfine field on the nuclei of those Fe3+ ions, which are the nearest or next nearest neighbours of the substituted Re3+ ion. The change of the hyperfine field is given by the change of dipole and transferred contribution. Both contributions are sensitive to the kind of Re3+ ion and to the value and direction of its magnetic moment. The satellite structure of NMR spectra provides sufficient amount of information (splitting) to find unknown parameters of the non...
A series of nuclear magnetic resonance observations of 3d transition-metal ions in nonmetallic ferro...
The electron structure and site preferences of Zn and Fe cations in Y hexaferrite system were calcul...
Mossbauer studies of R2(Fe1-x-yNixCoy)17 showed that the transferred hyperfine field at Fe nuclei du...
The dependence of 57Fe NMR spectra in YIG on the external magnetic field direction was measured at 4...
Satellite structure in 57Fe NMR spectra of In3+, Sc3+, Ga3+ and Al3+ substituted yttrium iron garnet...
NMR of 57Fe nuclei is used to study the Ý antisite defects (yttrium ions on the sites nominally occu...
Magnetite single crystals with Al, Ga and Ti substitutions were measured by means of 57Fe NMR (NMR) ...
N. M. R. of Fe57 nuclei was observed in the hyperfine fields of different rare earth garnets (Dy IG,...
NMR on 57Fe nuclei was measured in two single crystals of magnetite between 4.2 and 135 K (temperatu...
Nuclear magnetic resonance is a method, which provides information about the magnitude of hyperfine ...
We present an NMR study of hyperne elds at 57Fe nuclei in polycrystalline yttrium iron garnet. We me...
10B, 11B and 57Fe NMR spectra have been taken at 4.2 K. The B spectra reflect significant changes in...
The present work focuses on analyses of the experimental 57 Fe nuclear magnetic resonance data and t...
Recent nuclear magnetic resonance studies of magnetically ordered rare earth–3d transition metal all...
The Mössbauer spectra of Pr2Fe14B and Gd2Fe14B have been measured from 85 to 295 K and fit with a se...
A series of nuclear magnetic resonance observations of 3d transition-metal ions in nonmetallic ferro...
The electron structure and site preferences of Zn and Fe cations in Y hexaferrite system were calcul...
Mossbauer studies of R2(Fe1-x-yNixCoy)17 showed that the transferred hyperfine field at Fe nuclei du...
The dependence of 57Fe NMR spectra in YIG on the external magnetic field direction was measured at 4...
Satellite structure in 57Fe NMR spectra of In3+, Sc3+, Ga3+ and Al3+ substituted yttrium iron garnet...
NMR of 57Fe nuclei is used to study the Ý antisite defects (yttrium ions on the sites nominally occu...
Magnetite single crystals with Al, Ga and Ti substitutions were measured by means of 57Fe NMR (NMR) ...
N. M. R. of Fe57 nuclei was observed in the hyperfine fields of different rare earth garnets (Dy IG,...
NMR on 57Fe nuclei was measured in two single crystals of magnetite between 4.2 and 135 K (temperatu...
Nuclear magnetic resonance is a method, which provides information about the magnitude of hyperfine ...
We present an NMR study of hyperne elds at 57Fe nuclei in polycrystalline yttrium iron garnet. We me...
10B, 11B and 57Fe NMR spectra have been taken at 4.2 K. The B spectra reflect significant changes in...
The present work focuses on analyses of the experimental 57 Fe nuclear magnetic resonance data and t...
Recent nuclear magnetic resonance studies of magnetically ordered rare earth–3d transition metal all...
The Mössbauer spectra of Pr2Fe14B and Gd2Fe14B have been measured from 85 to 295 K and fit with a se...
A series of nuclear magnetic resonance observations of 3d transition-metal ions in nonmetallic ferro...
The electron structure and site preferences of Zn and Fe cations in Y hexaferrite system were calcul...
Mossbauer studies of R2(Fe1-x-yNixCoy)17 showed that the transferred hyperfine field at Fe nuclei du...