Both total and partial electronic conductivity of iron-doped calcium titana
tes, of general formula CaTi1-xFexO3-delta (x = 0, 0.1,...0.5), were invest
igated as a function of oxygen partial pressure at high temperatures (900,
1000 degrees C) by means of the four-probe technique and the Hebb-Wagner po
larization method, respectively. The oxygen partial pressure interval exten
ded from 1 to 10(-18) atm. Ti substitution by Fe results in a considerable
increase of both ionic and electronic conductivity and in appearance of a w
ide region of primarily ionic conductivity, independent of the oxygen parti
al pressure. Of these compositions, the x = 0.2 sample has the highest oxyg
en ion conductivity. A model of defect equilibrium is discussed. (C) 1999 E
lsevier Science BN. All rights reserved.