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缺氧钙钛矿在拓扑转变过程中表面离子的迁移动力学

Migration Kinetics of Surface Ions in Oxygen-Deficient Perovskite During Topotactic Transitions.

作者信息

Cao Lei, Petracic Oleg, Wei Xian-Kui, Zhang Hengbo, Duchoň Tomáš, Gunkel Felix, Koutsioubas Alexandros, Zhernenkov Kirill, Rushchanskii Konstantin Z, Hartmann Heinrich, Wilhelm Marek, Li Zichao, Xie Yufang, He Suqin, Weber Moritz L, Veltruská Kateřina, Stellhorn Annika, Mayer Joachim, Zhou Shengqiang, Brückel Thomas

机构信息

Institute of Ion Beam Physics and Materials Research, Helmholtz-Zentrum Dresden-Rossendorf, 01328, Dresden, Germany.

School of Advanced Materials, Peking University, Shenzhen Graduate School, Shenzhen, 518055, China.

出版信息

Small. 2021 Dec;17(51):e2104356. doi: 10.1002/smll.202104356. Epub 2021 Nov 17.

Abstract

Oxygen diffusivity and surface exchange kinetics underpin the ionic, electronic, and catalytic functionalities of complex multivalent oxides. Towards understanding and controlling the kinetics of oxygen transport in emerging technologies, it is highly desirable to reveal the underlying lattice dynamics and ionic activities related to oxygen variation. In this study, the evolution of oxygen content is identified in real-time during the progress of a topotactic phase transition in La Sr MnO epitaxial thin films, both at the surface and throughout the bulk. Using polarized neutron reflectometry, a quantitative depth profile of the oxygen content gradient is achieved, which, alongside atomic-resolution scanning transmission electron microscopy, uniquely reveals the formation of a novel structural phase near the surface. Surface-sensitive X-ray spectroscopies further confirm a significant change of the electronic structure accompanying the transition. The anisotropic features of this novel phase enable a distinct oxygen diffusion pathway in contrast to conventional observation of oxygen motion at moderate temperatures. The results provide insights furthering the design of solid oxygen ion conductors within the framework of topotactic phase transitions.

摘要

氧扩散率和表面交换动力学是复杂多价氧化物的离子、电子和催化功能的基础。为了理解和控制新兴技术中氧传输的动力学,非常需要揭示与氧变化相关的潜在晶格动力学和离子活性。在本研究中,在La Sr MnO外延薄膜的拓扑相变过程中,实时确定了表面和整个体相中氧含量的演变。使用极化中子反射测量法,获得了氧含量梯度的定量深度分布,这与原子分辨率扫描透射电子显微镜一起,独特地揭示了表面附近新结构相的形成。表面敏感的X射线光谱进一步证实了转变过程中电子结构的显著变化。与在中等温度下对氧运动的传统观察相比,这个新相的各向异性特征使得氧扩散途径截然不同。这些结果为在拓扑相变框架内进一步设计固体氧离子导体提供了见解。

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