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含间隙氧的磷灰石氧导体的低温晶体结构

Low temperature crystal structures of apatite oxygen-conductors containing interstitial oxygen.

作者信息

León-Reina L, Porras-Vázquez J M, Losilla E R, Sheptyakov D V, Llobet A, Aranda M A G

机构信息

Departamento de Química Inorgánica, Cristalografía y Mineralogía, Universidad de Málaga, 29071, Málaga, Spain.

出版信息

Dalton Trans. 2007 May 28(20):2058-64. doi: 10.1039/b616211h. Epub 2007 Apr 2.

Abstract

Oxygen-stoichiometric La(9.33) square(0.67)(Si(6)O(24))O2 and oxygen-excess La(8.65)Sr(1.35)(Ge(6)O(24))O(2.32) and La(8.65)Sr(1.35)(Si(6)O(24))O(2.32) oxy-apatites have been structurally characterized at low temperatures by the Rietveld method. Oxygen-interstitial distribution has been studied at 15 K for La(9.33) square(0.67)(Si(6)O(24))O2 and La(8.65)Sr(1.35)(Ge(6)O(24))O(2.32) by time-of-flight neutron powder diffraction and at 4 K for La(8.65)Sr(1.35)(Si(6)O(24))O(2.32) by constant-wavelength neutron powder diffraction. The low temperature structural study was undertaken in order to distinguish between the effects of static disorder, originated mainly from the presence of interstitial oxygens, and the anisotropic thermal vibrations. At such low temperatures, the influence of the anisotropic thermal vibrations is minimised. This structural study has firmly established the existence of interstitial oxygens in these materials, which may be useful as electrolytes for solid oxide fuel cells.

摘要

氧化学计量比的La(9.33)□(0.67)(Si(6)O(24))O2以及富氧的La(8.65)Sr(1.35)(Ge(6)O(24))O(2.32)和La(8.65)Sr(1.35)(Si(6)O(24))O(2.32)氧磷灰石已通过Rietveld方法在低温下进行了结构表征。通过飞行时间中子粉末衍射在15 K下对La(9.33)□(0.67)(Si(6)O(24))O2和La(8.65)Sr(1.35)(Ge(6)O(24))O(2.32)的氧间隙分布进行了研究,并通过恒波长中子粉末衍射在4 K下对La(8.65)Sr(1.35)(Si(6)O(24))O(2.32)的氧间隙分布进行了研究。进行低温结构研究是为了区分主要源自间隙氧存在的静态无序效应和各向异性热振动效应。在如此低的温度下,各向异性热振动的影响被最小化。该结构研究已确凿地证实了这些材料中存在间隙氧,这些材料可用作固体氧化物燃料电池的电解质。

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