Сибирский федеральный университет

Тип публикации: статья из журнала

Год издания: 2012

Идентификатор DOI: 10.1134/S1063783412090235

Аннотация: The X-ray diffraction, Mossbauer, calorimetric, and magnetic characteristics of zirconolite GdFeTi2O7 have been measured to determine the ground magnetic state. A kink dependent on the magnetic prehistory of the sample has been revealed in the temperature dependence of the magnetic moment at T = 3 K. Mossbauer spectroscopy has confirmed the nonequivalence of the iron ion positions in GdFeTi2O7. The experimental data obtained allow the conclusion on the formation of a spin glass state with the freezing temperature T (f) = 3 K in the GdFeTi2O7 compound.

Журнал: PHYSICS OF THE SOLID STATE

Выпуск журнала: Vol. 54, Is. 9

Номера страниц: 1813-1816

ISSN журнала: 10637834

Место издания: NEW YORK

Издатель: MAIK NAUKA/INTERPERIODICA/SPRINGER

• Petrakovskii G.A. (Siberian Federal University)
• Drokina T.V. (Siberian Federal University)
• Velikanov D.A. (Siberian Federal University)
• Bayukov O.A. (Siberian Federal University)
• Molokeev M.S. (Kirensky Institute of Physics,Siberian Branch of the Russian Academy of Sciences)
• Kartashev A.V. (Kirensky Institute of Physics,Siberian Branch of the Russian Academy of Sciences)
• Shadrina A.L. (Kirensky Institute of Physics,Siberian Branch of the Russian Academy of Sciences)
• Mitsuk A.A. (Siberian Federal University)

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