J. Kusinski et al., MICROSTRUCTURAL AND MICROANALYTICAL EXAMINATIONS OF PARTIALLY REDUCEDDOPED WUSTITES, Solid state ionics, 68(3-4), 1994, pp. 185-192
In this paper we report results on microstructural and compositional c
haracterization of (Fe1-x-yCay)O, (Re1-x-yMny)O and (Fe1-x-yMgy)O wust
ites and their reduction behaviour using optical, scanning and transmi
ssion electron microscopy and X-ray microanalysis. The microstructure
of mangano- and magnesio-wustites does not show any significant differ
ences when compared to FeO. This is due to the complete solubility of
Mn and Mg in FeO and to small differences in ionic sizes between iron
and these elements. In contrast, due to significant differences betwee
n iron and calcium, the microstructure of calcio-wustite consists of s
tacking faults in an ordered matrix. The density of the stacking fault
s increases with respect to Ca addition, up to about 1.5 wt% of Ca. Fu
rther addition of Ca atoms results in the precipitation of CaFe5O7 cal
cium ferrite plates as a consequence of low Ca solubility in FeO and i
ts segregation to the stacking faults.