Magnetization of lithiated magnetite, LixFe3O4

It is shown that annealed lithiated magnetites LixFe3O4, with x less than or equal to 0.60, present a regular Fe distribution between octahedral and tetrahedral sites. Their saturation magnetisation, remanent magnetisation and coercive field change linearly as a function of the lithium concentration...

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Veröffentlicht in:Journal of materials science letters 1997, Vol.16 (3), p.231-233
Hauptverfasser: NETO, J. M, NUNEZ, E, DOMINGUES, P. H
Format: Artikel
Sprache:eng
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Zusammenfassung:It is shown that annealed lithiated magnetites LixFe3O4, with x less than or equal to 0.60, present a regular Fe distribution between octahedral and tetrahedral sites. Their saturation magnetisation, remanent magnetisation and coercive field change linearly as a function of the lithium concentration. Non-annealed materials present a non-regular Fe distribution due to interstitial Li ions. 13 refs.
ISSN:0261-8028
DOI:10.1023/A:1018559909080