Oxygen grain-boundary diffusion in (La,Sr)FeO3−δ perovskite-oxides probed by molecular-dynamics simulations†

Alexander Bonkowski, John A. Kilner and Roger A. De Souza
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Abstract

Faster grain-boundary diffusion of oxygen has been observed experimentally in polycrystalline samples of Fe-based perovskite oxides at low temperatures, but this behaviour is at present not well understood. In our study, the influence of grain boundaries on oxygen diffusion is studied by means of classical atomistic simulation techniques. Oxygen tracer diffusion coefficients are determined for monocrystalline and polycrystalline simulation cells of orthorhombic La0.9Sr0.1FeO3−δ and cubic La0.6Sr0.4FeO3−δ by molecular-dynamics simulations at temperatures in the range 1000 ≤ T/K ≤ 2000. In particular, the effects of different oxygen nonstoichiometries δ and of equilibrium (as opposed to random) defect distributions were examined. Our results indicate, that the disrupted structures of the grain boundaries hinder oxygen diffusion; that Sr accumulation within grain-boundary regions does not produce faster diffusion; but that faster grain-boundary diffusion is observed when δ is decreased substantially with a consequent decrease in the rate of lattice diffusion.

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分子动力学模拟探测(La,Sr)FeO3-δ包晶氧化物中的氧晶界扩散†
实验观察到,在低温条件下,铁基过晶石氧化物的多晶样品中氧的晶界扩散速度更快,但目前对这种行为还没有很好的理解。在我们的研究中,通过经典原子模拟技术研究了晶界对氧扩散的影响。在 1000 ≤ T/K ≤ 2000 的温度范围内,通过分子动力学模拟确定了正方晶 La0.9Sr0.1FeO3-δ 和立方晶 La0.6Sr0.4FeO3-δ 的单晶和多晶模拟单元的氧示踪扩散系数。特别是,我们研究了不同氧非化学计量δ和平衡(而非随机)缺陷分布的影响。我们的研究结果表明,晶界的破坏结构阻碍了氧的扩散;晶界区域内的硒积累并不会加快扩散速度;但当δ大幅度降低,晶格扩散速度随之降低时,晶界扩散速度会加快。
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