Сибирский федеральный университет

Тип публикации: статья из журнала

Год издания: 2000

Идентификатор DOI: 10.1134/1.1318881

Аннотация: A spin-reorientational phase transition in the basal plane, which was experimentally observed earlier, is explained in terms of a model in which the crystalline 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 to the Fe-subsystem anisotropy competing with that of the rare-earth subsystem. (C) 2000 MAIK "Nauka/ Interperiodica".

Журнал: PHYSICS OF THE SOLID STATE

Выпуск журнала: Vol. 42, Is. 10

Номера страниц: 1881-1886

ISSN журнала: 10637834

Место издания: MELVILLE

Издатель: AMER INST PHYSICS

• Patrin G.S. (Kirenskii Inst. of Physics,Siberian Division,Russian Academy of Sciences)
• Shabalin A.V. (Krasnoyarsk State University)
• Eremin E.V. (Kirenskii Inst. of Physics,Siberian Division,Russian Academy of Sciences)

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