K.A. Chao
Physical Review B
Precise measurements of YbFeO3 magnetization in the spin-reoirentation temperature interval are performed. It is shown that ytterbium orthoferrite is well described by the modified mean-field theory recently developed for ErFeO3. This validates the conjecture about the essential influence of the rare-earth ion's anisotropic paramagnetism on the magnetization behavior in the reorientation regions of all orthoferrites with Γ4→Γ24→ Γ2 phase transitions. © 2005 The American Physical Society.
K.A. Chao
Physical Review B
U. Wieser, U. Kunze, et al.
Physica E: Low-Dimensional Systems and Nanostructures
J.H. Stathis, R. Bolam, et al.
INFOS 2005
P.C. Pattnaik, D.M. Newns
Physical Review B