INTERMEDIATE STATE OF (111) FERRITE GARNET CRYSTAL WAFERS NEAR THE SPIN REORIENTATION TEMPERATURE. / Kandaurova G.S., Pamyatnykh L.A., Fikhtner R.E. // Soviet physics. Technical physics. - 1984. - V. 29, l. 6. - P. 687-688.

ISSN:
00385662
Type:
Article
Abstract:
It is shown that the pseudouniaxial state is stable over a wide temperature range and is present as an intermediate state during the transition of the crystal from the multiaxial magnetic to the uniaxial states. It is shown that the multiaxial to uniaxial transition proceeding through the intermediate pseudouniaxial structure involves a spin reorientation which is caused by the different temperature dependences of the cubic and induced uniaxial magnetic anisotropies and is accompanied by a radical change in the hysteresis loops. Also studied were the domain structure, magnetic anisotropy, and hysteresis properties of (111) single-crystal (TbErGd)//3Fe//5O//1//2 ferrite garnet wafers of thickness 50-100 mu m for 280 less than equivalent to T less than equivalent to 400 K. The magnetooptic Faraday effect was used to observe the domain structure.
Author keywords:
Index keywords:
FERRITES; HYSTERESIS; MAGNETIC PROPERTIES; MAGNETOOPTICAL EFFECTS; FERRITE GARNET CRYSTAL WAFERS; INTERMEDIATE STATE; SPIN REORIENTATION TEMPERATURE; GARNETS
DOI:
нет данных
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Affiliations A. M. Gor'kii Ural State Univ, Sverdlovsk, USSR, A. M. Gor'kii Ural State Univ, Sverdlovsk, USSR
Correspondence Address Kandaurova, G.S.; A. M. Gor'kii Ural State Univ, Sverdlovsk, USSR, A. M. Gor'kii Ural State Univ, Sverdlovsk, USSR
CODEN SPTPA
Language of Original Document English
Abbreviated Source Title Sov Phys Tech Phys
Source Scopus