Interstitial oxide positions in oxygen-excess oxy-apatites

被引：80

作者：

Leon-Reina, Laura ^{[1
]}

Porras-Vazquez, J. Manuel ^{[1
]}

Losilla, Enrique R. ^{[1
]}

Aranda, Miguel A. G. ^{[1
]}

机构：

[1] Univ Malaga, Dept Quim Inorgan Cristalog & Mineral, E-29071 Malaga, Spain

来源：

SOLID STATE IONICS | 2006年 / 177卷 / 15-16期

关键词：

SOFC; oxide ion conductor; apatite synchrotron; neutron diffraction;

D O I：

10.1016/j.ssi.2006.05.034

中图分类号：

O64 [物理化学（理论化学）、化学物理学];

学科分类号：

070304 ; 081704 ;

摘要：

Several oxy-apatites materials, La8.65Sr1.35(Si6O24)O-2.32, La8.65Sr1.35(Ge6O24)O-2.32, La9Sr1(Si5.5Al0.5O24)O-2.25, La-9.67 rectangle(0.33)(Si5.5Al0.5O24) O-2.25, La8.5Sr1.5(Si5.5Al0.5O24)O-2 and La-9.5 rectangle(0.5)(Si5.5Al0.5O24)O-2 have been prepared as crystalline phases. The impedance study showed that all samples are oxide ion conductors and their conductivities are similar to those previously reported for related oxy-apatites. A thorough study on the oxygen sublattices for oxygen excess samples has been carried out using neutron powder diffraction data by the Rietveld method. The structural study shows the presence of interstitial oxide anions close to the periphery apatite channels. However, the interstitial oxide position in cation stoichiometric silicates, f i. La8.65Sr1.35(Si6O24)O-2.32, is different from that in germanates, f. i. La8.65Sr1.35(Ge6O24)O-2.32. This is likelyclue to the different structural flexibility of the two tetrahedral groups and it explains the previously reported evidence of higher oxygen contents for germanates oxy-apatites. The structural characteristics of these oxide anion conductors are discussed. (c) 2006 Elsevier B.V. All rights reserved.

引用

页码：1307 / 1315

页数：9

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