Investigation on double perovskite Ba4Ca2Ta2O11

被引:13
|
作者
Baliteau, S. [1 ]
Mauvy, F. [1 ]
Fourcade, S. [1 ]
Grenier, J. C. [1 ]
机构
[1] Univ Bordeaux 1, CNRS, UPR 9048, ICMC Bordeaux, F-33608 Pessac, France
关键词
Ba4Ca2Ta2O11; Double perovskite; Oxygen ionic and protonic conductions; PROTONIC CONDUCTION; IONIC-CONDUCTION; OXYGEN; WATER;
D O I
10.1016/j.solidstatesciences.2009.06.023
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
The structure, conductivity and water uptake of the oxygen-deficient perovskite-type compound Ba4Ca2Ta2O11 have been investigated. Ba4Ca2Ta2O11 crystallizes in the cryolite structure (cubic, Fm3m SG) with a = 8.4508(2) angstrom, under dry air. The compound can be partially hydrated up to a maximum water content of approximately 0.52 mol H2O per mol Ba4Ca2Ta2O11. In moist air, the structure symmetry becomes monoclinic (C2/m) and the temperature dependence of total conductivity shows a different behavior because of changes in transport mechanism. Three regions can be observed as a function of temperature. For the low temperature range 200-400 degrees C, the protonic conduction is prevailing with an activation energy E-A = 0.85 eV. In the intermediate temperature range (400-600 degrees C). O2- anionic and protonic conductions are mixed with an activation energy E-A = 0.45 eV and in the third region, for temperatures above 600 degrees C, O2- conduction is prevailing with an activation energy E-A = 0.85 eV. (C) 2009 Elsevier Masson SAS. All rights reserved.
引用
收藏
页码:1572 / 1575
页数:4
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