Journal of Applied Physics · 1965 · 51 citations · 3 references
Natural SciencesMaterials EngineeringMaterials ScienceCrystal StructureElectromagnetismMagnetic MaterialsFerrimagnetic MaterialsFerromagnetismMagnetic AnisotropyMagnetic CharacterizationMagnetic Properties Of SolidsMagnetism In SolidsAnisotropy In FerromagnetsMagnetic Anisotropy MeasurementMagnetocrystalline AnisotropyPolycrystalline MaterialsPrimary AnisotropiesPrincipal DirectionsRare-earth Iron GarnetsRare-earth Magnetism
Single-crystal magnetization measurements using a force method and fields up to 17 000 Oe applied in the principal crystal directions are presented for TbIG, DyIG, HoIG, ErIG, and SmIG in the range 20°–300°K. In the region below 100°K, where these garnets have high anisotropies, the results differ from the original measurements of Pauthenet on polycrystalline samples by as much as 6 μB, though the compensation temperatures found are close to those of Pauthenet. Residual anisotropies in the magnetization <1 μB are apparent for ErIG and TbIG below 80°K.
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Annals of Physics · 1958 · 204 citations
Magnetocrystalline Anisotropy of Rare-Earth Iron Garnets
R. F. Pearson · Journal of Applied Physics · 1962 · 118 citations
Magnetic Study of the Lighter Rare-Earth Ions in the Iron Garnets
S. Geller, H. J. Williams, R. C. Sherwood et al. · Physical Review · 1963 · 107 citations