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
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.