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In Situ Atomic-Scale Probing of the Reduction Dynamics of 2-Dimensional Fe2O3 Nanostructures

机译:二维Fe2O3纳米结构还原动力学的原位原子尺度探测

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摘要

Atomic-scale structural dynamics and phase transformation pathways were probed, in situ, during the hydrogen-induced reduction of Fe2O3 nanostructure bi-crystals using an environmental transmission electron microscope. Reduction commenced with the α-Fe2O3 → γ-Fe2O3 phase transformation of one part of the bi-crystal, resulting in the formation of a two-phase structure of α-Fe2O3 and γ-Fe2O3. The progression of the phase transformation into the other half of the bi-crystalline Fe2O3 across the bi-crystalline boundary led to the formation of a single crystal phase of γ-Fe2O3 with concomitant oxygen-vacancy ordering on every third {422} plane, followed by transformation into Fe3O4. Further reduction resulted in the coexistence of Fe3O4, FeO, and Fe via the transformation pathway Fe3O4 → FeO → Fe. The series of phase transformations was accompanied with the formation of a Swiss-cheese-like structure, induced by the significant volume shrinkage occurring upon reduction. These results elucidated the atomistic mechanism of the reduction of Fe oxides and demonstrated formation of hybrid structures of Fe oxides via tuning the phase transformation pathway.
机译:使用环境透射电子显微镜,在氢诱导的Fe2O3纳米结构双晶体还原过程中,就地探测了原子尺度的结构动力学和相变途径。还原从一部分双晶的α-Fe2O3→γ-Fe2O3相变开始,导致形成α-Fe2O3和γ-Fe2O3两相结构。相变跨双晶边界进入双晶Fe2O3另一半的过程导致形成γ-Fe2O3单晶相,并在每三个{422}平面上伴随着氧空位有序,通过转化为Fe3O4。进一步还原导致Fe 3 O 4 ,FeO和Fe通过转化途径Fe 3 O 4 共存。 sub>→FeO→Fe。一系列相变伴随着瑞士奶酪样结构的形成,这是由还原时发生的体积收缩引起的。这些结果阐明了铁氧化物还原的原子机理,并证明了通过调节相变途径形成铁氧化物的杂化结构。

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