Abstract. The high temperature conductivity of polycrystalline Sr~.xTiO3_~ samples in air was found to be lower than the conductivity of SrTiO 3 samples. However, the dependence of the electrical conductivity on the oxygen partial pressure showed that this trend can be reverted under reducing conditions. Both trends contradict the expected effects of A-site deficiency on the defect chemistry. Differences in average grain sizes give a plausible explanation for these findings. The dependence of the conductivity on the oxygen partial pressure suggests that p-type conductivity is dominant in air, for every sample, and one can thus assume that the number of grain boundaries plays a negative role on this contribution. Electrochemical permeability measurements confirmed that the ionic transport number of strontium titanate in air remains small.