Gs. Patrin et al., Spin-reorientational phase transition in the basal plane in an alpha-Fe2O3:(Ga, Dy) crystal, PHYS SOL ST, 42(10), 2000, pp. 1881-1886
A spin-reorientational phase transition in the basal plane, which was exper
imentally observed earlier, is explained in terms of a model in which the c
rystalline Fe-ion matrix is considered as a continuum, while dopant Dy ions
are treated as quasi-Ising ions. The transition is established to be due t
o the Fe-subsystem anisotropy competing with that of the rare-earth subsyst
em. (C) 2000 MAIK "Nauka/ Interperiodica".