S. Xie et al., Mixed oxygen ionic and electronic conduction in CaFe0.2T0.8O3-delta: a combined oxygen permeation and electrical conductivity study, SOL ST ION, 118(1-2), 1999, pp. 23-28
A combined oxygen permeation and electrical conductivity study on CaFe0.2Ti
0.8O3-delta was conducted in the temperature range of 1100-850 degrees C, a
iming at clarifying the oxygen transport mechanism. The oxide shows appreci
ated oxygen permeability at elevated temperature. An oxygen permeation flux
of 6.37 x 10(8) mol cm(-2) s(-1) was observed at 1100 degrees C by applyin
g an oxygen partial pressure difference to a 0.84-mm thick disk-shaped, sam
ple (P-O2(h) = 0.209 and P-O2(l) = 0.004 atm). The apparent activation ener
gy for oxygen permeation remained almost unchanged (170 kT/mol) with the va
riation of the sample thickness in the range of 2.5-0.8 mm. This indicates
that the oxygen permeation kinetics is controlled by the transport of charg
e carriers in the bulk of sample, and can by promoted by further reduction
of the thickness. In combination with electrical conductivity measurements,
the partial conductivities of oxygen ions and electron holes, sigma(l) and
sigma(e) were determined. The value of sigma(l) is comparable to that for
sigma(e) at the high temperature of 1100 degrees C, but the latter became d
ominant at reduced temperature. This is due to the much higher activation e
nergy associated with the transport of oxygen ions (179 +/- 6 kJ/mol) than
that for electron holes (22 +/- 2 kJ/mol). It becomes clear that increasing
the partial conductivity of oxygen ions in the oxide should lead to the im
provement of the oxygen permeability of the oxide. (C) 1999 Published by El
sevier Science B.V. All rights reserved.