Electrical Conductivity of Y2O3 as a Function of Oxygen Partial Pressure in Wet and Dry Atmospheres

The electrical conductivity of polycrystalline Y₂O₃ has been studied as a function of the partial pressure of oxygen (10^–14 to 10⁵ Pa) at 900° to 1500°C in atmospheres saturated with water vapor at 12°C or dried with P₂O₅. Yttria is a p -conductor at high oxygen activities. The p -conductivity increases with increasing P _O2 and decreases with increasing P_H2O. At low oxygen activities the oxide is a mixed ionic/electronic conductor. The ionic conductivity is approximately independent of P _O2 and increases with increasing P _H2O. In the Y₂O₃ samples, excesses of lower-valent cation impurities (in the 10 to 100 mol-ppm range) are the dominating negatively charged defects, and in the presence of water vapor they are compensated by interstitial protons. At high P _H2O levels additional protons are probably compensated by interstitial oxygen ions. At high temperatures (±1100°C) and for high P _O2 and low P _H2O, the protons are no longer dominant, and the lower-valent cations are mainly compensated by electron holes. The electrical conductivity exhibits hysteresis-like effects which are interpreted in terms of segregation/desegregation of impurities at grain boundaries. The mobility of electron holes in yttria at 1500°C is estimated to be of the order of magnitude of 0.05 cm². s^–1. V^–1