Electrically
insulating A2B2O5 brownmillerite
materials can be transformed through a reversible,
topotactic phase transition to conducting ABO3−δ perovskite phases. Such systems are of emerging interest for resistive
random-access devices. The key process for the phase transition is
oxygen diffusion, but to date, experimental or computational studies
yielding oxygen diffusion coefficients in brownmillerite materials
are rare. In this study, we use molecular dynamics simulations to
directly investigate oxygen tracer diffusion in the brownmillerite
Sr2Fe2O5 phase and the SrFeO2.5 perovskite phase. Our results for brownmillerite Sr2Fe2O5 go beyond computed diffusion coefficients:
They indicate that oxygen vacancies execute two-dimensional diffusion
between the equatorial sites of the FeO6 octahedra, and
surprisingly, that oxygen interstitials are not confined to the oxygen-vacancy
channels (as widely assumed in the literature) but migrate two-dimensionally
by interstitial and interstitialcy mechanisms in the FeO4 layers. Comparisons with experimental data are possible for the
perovskite phase, and good agreement is found between simulation and
experiment for the oxygen-vacancy diffusivity in terms of both absolute
magnitude and activation enthalpy.