CATIONIC DISTRIBUTION AND OXIDATION MECHANISM OF TRIVALENT MANGANESE IONS IN SUBMICROMETER MNXCOFE2-XO4 SPINEL FERRITES

Citation
M. Laarj et al., CATIONIC DISTRIBUTION AND OXIDATION MECHANISM OF TRIVALENT MANGANESE IONS IN SUBMICROMETER MNXCOFE2-XO4 SPINEL FERRITES, Journal of solid state chemistry, 125(1), 1996, pp. 67-74
Citations number
33
Categorie Soggetti
Chemistry Inorganic & Nuclear","Chemistry Physical
ISSN journal
00224596
Volume
125
Issue
1
Year of publication
1996
Pages
67 - 74
Database
ISI
SICI code
0022-4596(1996)125:1<67:CDAOMO>2.0.ZU;2-6
Abstract
Submicrometer Mn2CoFe2-xO4 (0 less than or equal to x < 1) spinel part icles with a spherical shape were prepared at low temperature from oxa lic precursors. Because of their small crystallite size (about 50 nm), these ferrite particles can be oxidized below 400 degrees C giving cu bic deficient spinels having both Mn3+ and Mn4+ ions because of oxide- reduction phenomena, Information about the valence state of the mangan ese and cobalt ions and cation distribution between tetrahedral (A) an d octahedral (B) sites are derived from lattice parameter variation, I R spectroscopy, thermogravimetric analysis, and electrical conductivit y, A kinetics study of the oxidation of Mn3+ ions shows that oxidation proceeds by cation diffusion through a topotactic reaction with a con stant chemical diffusion coefficient for x < 0.60 and variable above x = 0.80 and an activation energy close to 115 kJ mol(-1) but, however, depending on manganese substitution content. (C) 1996 Academic Press, Inc.