1978 Volume 45 Issue 4 Pages 1204-1212
Molecular field equations for Γ4, Γ24 and Γ2 phases of rare earth orthochromites and orthoferrites are derived and applied to the analysis of the observed magnetization in GdCrO3. The Cr–Cr, Cr–Gd and Gd–Gd interactions are determined so as to fit the observed magnetization. The free energy is calculated by using these values of the parameters. It is shown that the single-ion anisotropy of the Gd3+ ion and the Gd3+–Gd3+ interaction contribute to the magnetization below 10 K and to the free energy below 3 K, while the Cr3+–Gd3+ antisymmetric exchange interaction stabilizes the free energy below 10 K.
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