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Low-temperature magnetic behavior of gadolinium ortho-ferrite and certain of its substitution compounds

V. N. DerkachenkoDonets Physicotechnical Institute, Academy of Sciences of the Ukrainian SSRA. M. KadomtsevaDonets Physicotechnical Institute, Academy of Sciences of the Ukrainian SSRT. L. OvchinnikovaDonets Physicotechnical Institute, Academy of Sciences of the Ukrainian SSRВ. А. ТимофееваDonets Physicotechnical Institute, Academy of Sciences of the Ukrainian SSRВ. А. ХохловDonets Physicotechnical Institute, Academy of Sciences of the Ukrainian SSR
ABI

Abstract

The rotational moments of gadolinium ortho-ferrite were measured in different crystallographic planes at 2.1°K. The rotation diagrams obtained indicate the presence of a magnetic ordering of the spins of the Gd3+ ions along the a axis of the crystal. A “flipping” of the Gd3+ antiferromagnetic sublattices was observed with the application of a magnetic field of ∼ 104 Oe along the a axis of the rhombic crystal. It is assumed that monoclinic distortions of the lattice occur during the ordering of the Gd3+ ions. The magnetization of GdFeO3, GdAl0.1Fe0.9O3 and GdGa0.1Fe0.9O3 were measured over the 4.2–80°K temperature range. It is shown that the spontaneous moment of the iron ions changes little with the partial substitution of Fe3+ ions by Ga3+ and Al3+ ions, while the effective field acting on the rare-earth ions, caused by the iron ions, increases. The possible cause of this phenomenon is discussed.

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