A Mössbauer study of manganese-doped magnetite
A series of Fe 3− x Mn x O 4 samples with x=0–0.6 was prepared using the hydrothermal method. The system was characterized using transmission Mössbauer spectroscopy. The dependence of the site hyperfine magnetic fields and populations on the content x of Mn substitution was derived from the spectra....
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Published in | Materials letters Vol. 57; no. 12; pp. 1867 - 1869 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Amsterdam
Elsevier B.V
01.03.2003
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | A series of Fe
3−
x
Mn
x
O
4 samples with
x=0–0.6 was prepared using the hydrothermal method. The system was characterized using transmission Mössbauer spectroscopy. The dependence of the site hyperfine magnetic fields and populations on the content
x of Mn substitution was derived from the spectra. The results are consistent with Mn
2+ ions substituting for Fe
2+ ions in the octahedral B sublattice. In particular, the site-specific substitution of Mn ions for the B2 sites was evidenced. |
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Bibliography: | ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 |
ISSN: | 0167-577X 1873-4979 |
DOI: | 10.1016/S0167-577X(02)01092-3 |