Oxygen ionic conduction in the perovskite-type Sr0.97Ti0.60Fe0.40O3-delta w
as studied using oxygen permeability, Faradaic efficiency and total electri
cal conductivity measurements at 973-1223 K. The ion transference numbers o
f the strontium titanate-ferrite in air vary from 0.005 to 0.08, decreasing
with decreasing temperature. The electron-hole conductivity of the oxide i
s relatively low but exceeds the ionic conductivity. The activation energy
for the electronic conductivity is 35+/-3 kJ/mol at 470-890 K and drops at
higher temperatures. Studying the oxygen permeation through dense Sr0.97Ti0
.60Fe0.40O3-delta ceramic membranes as a function of membrane thickness sho
wed that at temperatures above 1170 K the permeation fluxes are limited by
both bulk ionic conductivity and surface exchange rates. Depositing of poro
us layers of the same material or a mixture of platinum and praseodymium ox
ide onto the membrane feed-side surface leads to a significant increase in
the oxygen permeability. Decreasing temperature results in increasing role
of the bulk ionic transport in Sr0.97Ti0.60Fe0.40O3-delta as the permeation
-determining factor. The oxygen permeation fluxes at 1073 K are limited pre
dominantly by the oxygen ionic conductivity of the ceramics. The thermal ex
pansion coefficients of the ceramic material in air were calculated from di
latometric data to be 11.7 x 10(-6) K-1 in the temperature range 300-720 K
and 16.6 X 10(-6) K-1 at 720-1070 K. (C) 2000 Elsevier Science B.V. All rig
hts reserved.