The conductivities of a protonic conductor, 10 mole percent (m/o) In2O
3-doped CaZrO3, were measured in an atmosphere containing hydrogen or
deuterium with the 4-wires ac impedance technique at temperatures rang
ing from 623 to 1673 K. In high oxygen activities, H+/D+-isotope effec
ts were observed below about 1100 K. The ratio of conductivities of pr
otons to deuterons increased as the temperature decreased and rose to
about 1.6 at 673 K. It was made clear by this observation that at low
temperatures electrical conduction is dominated by proton and at high
temperatures by positive hole, respectively. On the other hand, at hig
h hydrogen activities, the isotope effects were observed up to about 1
600 K and it was concluded that proton is dominant below this temperat
ure. Over that temperature, the isotope effects vanished and the elect
rical conductivities were independent of gas potentials. It was conclu
ded that electrical conduction over 1600 K was dominated by oxide ions
. As electrical carriers obey the thermally activated process, the act
ivation energies were calculated by the least squares method. The obta
ined activation energies of protons, deuterons, positive holes, and ox
ide ion vacancies were 0.74 +/- 0.05, 0.70 +/- 0.05, 1.21 +/- 0.07, an
d 2.5 +/- 0.5 eV, respectively. Based on the model of defects equilibr
ia and these experimental findings, the protonic conduction domain of
the specimen was determined and is represented in temperature-potentia
l diagrams.