Oxygen ionic and electronic transport in apatite ceramics

被引:54
|
作者
Shaula, AL [1 ]
Kharton, VV
Waerenborgh, JC
Rojas, DP
Marques, FMB
机构
[1] Univ Aveiro, CICECO, Dept Ceram & Glass Engn, P-3810193 Aveiro, Portugal
[2] Inst Tecnol & Nucl, Dept Chem, P-2686953 Sacavem, Portugal
关键词
electrical conductivity; ionic conductivity; thermal expansion; apatite; fuel cells;
D O I
10.1016/j.jeurceramsoc.2005.03.106
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
The development of novel oxygen ion conducting solid electrolytes is of great interest for high-temperature electrochemical applications such as solid oxide fuel cells (SOFCs). This work was focused on the study of transport properties of apatite-type La10Si6-xFexO27-x/2 (x = 1-2). Single-phase apatite ceramics with density higher than 98% were prepared by the standard solid-state synthesis route. The materials were characterized by X-ray diffraction, dilatometry, impedance spectroscopy and faradaic efficiency measurements. The total conductivity and Seebeck coefficient were studied as function of the oxygen partial pressure varying in the range 10(-16) Pa to 50 kPa. The ionic conductivity of apatite phases was found to increase with oxygen content. In air, the ion transference numbers of La10Si6-xFexO27-x/2 (x= 1.0-1.5) at 700-950 degrees C are higher than 0.99, whilst the p-type electronic contribution to the total conductivity of La10Si4Fe2O26 is about 3%. Mossbauer spectroscopy showed that the coordination of iron cations, which are all trivalent within the detection limits, increases with oxygen intercalation in the lattice. Reducing P(02) below 10(-8) Pa leads to a decrease in the ionic transport and growing n-type electronic contribution, the role of which increases with iron additions. The average thermal expansion coefficients in air are (8.2-9.9) x 10(-6) K-1 at 100-1000 degrees C. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2583 / 2586
页数:4
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