Complex changes in the electrical properties of the oxide ion-conducti
ng solid electrolyte Ca12Al14O33 were observed on heating in reducing
atmospheres. On gentle reduction the high oxide ion conductivity of Ca
12Al14O33 Was gradually destroyed, due to the formation and growth of
resistive grain boundary and surface components. An interesting effect
is the thickening of the grain boundary layer on reduction as indicat
ed by capacitance data; the grain boundary appears to form a shell aro
und the residual, oxide ion conducting core of the individual grains.
Similar impedance responses were observed in samples annealed below 70
0-degrees-C and in samples slow cooled from higher temperatures. Under
more severe reduction, at temperatures above 800-degrees-C, the surfa
ce layer was no longer observed and the conductivity of both the shell
and core increased and appeared to become electronic. This behaviour
could be retained to lower temperatures by quenching. These observatio
ns are consistent with two reduction processes: the mobile oxide ions
are effectively trapped as immobile hydroxides at lower temperatures,
whereas more extensive reduction at high temperatures yields conductiv
e electronic behaviour.