Oxide ion conduction in Ba, Ca and Sr doped apatite-type lanthanum silicates

被引:58
作者
Beaudet-Savignat, S. [1 ]
Vincent, A. [1 ]
Lambert, S. [1 ]
Gervais, F. [1 ]
机构
[1] Univ Tours, CNRS,UMR 6157, CEA, LEMA, F-37000 Tours, France
关键词
D O I
10.1039/b615104c
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
The apatite-type compounds La-9.33 square 0.67Si6O26, La10-xBax(SiO4)(6)O2+delta with x = 0.5 -> 2, La9Ca1(SiO4)(6)O2 + delta and La9Sr1Si6(SiO4)(6)O2 + delta were prepared by high temperature solid state reaction with a high purity level. The La9Ba1Si6O26.5 composition is a good electrolyte for SOFCs at intermediate temperature, with a pure ionic conductivity of 1.16 x 10(-2) S cm(-1) at 700 degrees C and low activation energy of 0.74 eV. Moreover the conductivity is stable after one month of ageing at 900 degrees C under air or reducing atmosphere and is increased with the ceramic grain size. The comparison of undoped La(9.3)3 square 0.67Si6O26 apatite and doped La(9)AE(1)(SiO4)(6)O-26 apatites with AE= Ca, Sr, Ba shows an increase in conductivity with the doping concentration. For doped apatites, the conductivities and activation energy are related to the dopant size, the best properties being obtained for the barium doping. The existence of some extra oxide ions was demonstrated by NPD experiments for oxygen excess apatites but there was no evidence for a new crystallographic interstitial oxygen site in the hexagonal channel. The oxide ion O(5) in the hexagonal channel exhibits a large spread of the nuclear density along the c-axis in all samples, probably due to a static disorder. The cooperative displacements of the SiO4 tetrahedra and of the La( 3) site towards the O( 5) channel suggest a conduction mechanism involving mainly the extra oxide ions with a migration path between the O( 5) channel and the SiO4 tetrahedra along the [001] direction.
引用
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页码:2078 / 2087
页数:10
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