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Probing Cation and Vacancy Ordering in the Dry and Hydrated Yttrium-Substituted BaSnO3 Perovskite by NMR Spectroscopy and First Principles Calculations: Implications for Proton Mobility

化学 结晶学 空位缺陷 核磁共振波谱 密度泛函理论 化学位移 钙钛矿(结构) 核磁共振谱数据库 光谱学 氟-19核磁共振 计算化学 立体化学 物理化学 谱线 物理 量子力学 天文
作者
Lucienne Buannic,Frédéric Blanc,Derek S. Middlemiss,Clare P. Grey
出处
期刊:Journal of the American Chemical Society [American Chemical Society]
卷期号:134 (35): 14483-14498 被引量:51
标识
DOI:10.1021/ja304712v
摘要

Hydrated BaSn1–xYxO3–x/2 is a protonic conductor that, unlike many other related perovskites, shows high conductivity even at high substitution levels. A joint multinuclear NMR spectroscopy and density functional theory (total energy and GIPAW NMR calculations) investigation of BaSn1–xYxO3–x/2 (0.10 ≤ x ≤ 0.50) was performed to investigate cation ordering and the location of the oxygen vacancies in the dry material. The DFT energetics show that Y doping on the Sn site is favored over doping on the Ba site. The 119Sn chemical shifts are sensitive to the number of neighboring Sn and Y cations, an experimental observation that is supported by the GIPAW calculations and that allows clustering to be monitored: Y substitution on the Sn sublattice is close to random up to x = 0.20, while at higher substitution levels, Y–O–Y linkages are avoided, leading, at x = 0.50, to strict Y–O–Sn alternation of B-site cations. These results are confirmed by the absence of a “Y–O–Y” 17O resonance and supported by the 17O NMR shift calculations. Although resonances due to six-coordinate Y cations were observed by 89Y NMR, the agreement between the experimental and calculated shifts was poor. Five-coordinate Sn and Y sites (i.e., sites next to the vacancy) were observed by 119Sn and 89Y NMR, respectively, these sites disappearing on hydration. More five-coordinated Sn than five-coordinated Y sites are seen, even at x = 0.50, which is ascribed to the presence of residual Sn–O–Sn defects in the cation-ordered material and their ability to accommodate O vacancies. High-temperature 119Sn NMR reveals that the O ions are mobile above 400 °C, oxygen mobility being required to hydrate these materials. The high protonic mobility, even in the high Y-content materials, is ascribed to the Y–O–Sn cation ordering, which prevents proton trapping on the more basic Y–O–Y sites.
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