Structural, magnetic and Mössbauer studies on nickel‐zinc ferrites synthesized via a precipitation route
Author(s) -
Date S. K.,
Joy P. A.,
Kumar P. S. Anil,
Sahoo B.,
Keune W.
Publication year - 2004
Publication title -
physica status solidi (c)
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.21
H-Index - 46
eISSN - 1610-1642
pISSN - 1610-1634
DOI - 10.1002/pssc.200405489
Subject(s) - crystallite , superparamagnetism , ferrite (magnet) , materials science , mössbauer spectroscopy , hyperfine structure , analytical chemistry (journal) , magnetization , quadrupole splitting , coprecipitation , nuclear magnetic resonance , chemistry , crystallography , metallurgy , magnetic field , inorganic chemistry , composite material , physics , chromatography , quantum mechanics
Polycrystalline Ni‐Zn ferrite, with a well‐defined composition, Ni 0.8 Zn 0.2 Fe 2 O 4 , synthesized by a low‐temperature method showed the formation of a cubic ferrite phase with a crystallite size of ∼15 nm and saturation magnetization of M s ≈ 44 emu/g at room temperature. When calcined at higher temperatures (up to 1200 °C) the magnetization increased continuously to M s ≈ 67 emu/g. To understand the magnetic nature of the cubic ferrite phase formed at a temperature as low as 80 °C, 57 Fe Mössbauer spectra were recorded for samples annealed at three different temperatures, without any external magnetic field, and with an external field of H ext = 5 T, at 4.2 K. The spectral parameters at room temperature, namely, isomer shift, quadrupole splitting and hyperfine field, confirmed the presence of ultrafine superparamagnetic crystallites of Ni‐Zn ferrite. The Mössbauer spectra at 4.2 K revealed spin relaxation effects resulting in very broad sextets, characteristic of ultrafine crystallites. The Mössbauer spectra recorded at 4.2 K and H ext = 5 T showed well‐resolved two‐sextet pattern with characteristic hyperfine interaction parameters of the cubic ferrite phase. (© 2004 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)
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