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Oxygen conduction mechanism in Ca3Fe2Ge3O12 garnet-type oxide

机译:Ca3Fe2Ge3O12石榴石型氧化物中的氧传导机理

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摘要

We investigate the oxygen conduction mechanism in a garnet-type oxide, Ca3Fe2Ge3O12, for the first time in detail by first-principle calculations. The nudged elastic band results confirm that this oxide has a lower migration barrier energy (0.45 eV) for an oxygen interstitial (Oi) with the kick-out mechanism than that (0.76 eV) for an oxygen vacancy. The migration paths for Oi are delocalized and connected to the neighboring cells in three-dimensional space. This oxide does not have a very low formation energy of Oi when the Fermi level is near the lowest unoccupied molecular orbital at a high temperature, which implies the possibility of electron doping by high-valence cations. These theoretical results suggest that the doping of Ca3Fe2Ge3O12 for generation of excess Oi provides a good oxygen-ion conductivity, along with the electronic conductivity.
机译:我们通过第一性原理计算首次详细研究了石榴石型氧化物Ca3Fe2Ge3O12中的氧传导机理。弹力带的微调结果证实,该氧化物对具有起爆机理的氧间隙(Oi)的迁移势垒能量(0.45 ^ eV)比对氧空位的迁移势垒能量(0.76 ^ eV)低。 Oi的迁移路径是非本地化的,并连接到三维空间中的相邻单元格。当费米能级在高温下处于最低的未占据分子轨道附近时,该氧化物的Oi形成能不会非常低,这暗示着电子可能被高价阳离子掺杂。这些理论结果表明,掺杂Ca3Fe2Ge3O12以产生过量的Oi以及良好的氧离子电导率以及电子电导率。

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