Langhof N, Göbbels M (2009)
Publication Language: English
Publication Type: Journal article
Publication year: 2009
Publisher: Elsevier
Book Volume: 182
Pages Range: 2725-2732
Journal Issue: 10
DOI: 10.1016/j.jssc.2009.07.024
The iron rich part of the system was examined in the temperature range of 1200-1380 °C in air, with focus on the solid solutions of M-type hexaferrites. Samples of suitable compositions were studied by electronprobe microanalysis (EPMA). Substituted Sr-hexaferrites in the system Sr-La-Co-Fe-O do not follow the 1:1 substitution mechanism of La/Co in M-type ferrites. Due to the presence and limited Co2+-incorporation Fe3+-ions are reduced to Fe2+ within the crystal lattice to obtain charge balance. In all examined M-type ferrites divalent iron is formed, even at 1200 °C. The substitution principle Sr2++Fe3+↔La3++(Fe2+, Co2+) yields to the general substitution formula for the M-type hexaferrite Sr2 +
APA:
Langhof, N., & Göbbels, M. (2009). Hexaferrites an phase relations in the iron-rich part of the system Sr-La-Co-Fe-O. Journal of Solid State Chemistry, 182(10), 2725-2732. https://doi.org/10.1016/j.jssc.2009.07.024
MLA:
Langhof, Nico, and Matthias Göbbels. "Hexaferrites an phase relations in the iron-rich part of the system Sr-La-Co-Fe-O." Journal of Solid State Chemistry 182.10 (2009): 2725-2732.
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