Using in situ X-ray absorption spectroscopy to study the local structure and oxygen ion conduction mechanism in (La0.6Sr0.4)(CO0.2Fe0.8)O3-δ

被引:23
作者
Itoh, Takanori [1 ]
Nakayama, Masanobu [2 ]
机构
[1] AGC SeimiChem Co Ltd, Chigasaki, Kanagawa 2538585, Japan
[2] Nagoya Inst Technol, Dept Mat Sci & Engn, Showa Ku, Nagoya, Aichi 4668555, Japan
关键词
X-ray absorption spectroscopy; XANES; EXAFS; Oxygen ion conduction; Perovskite; Valence; CHEMICAL DIFFUSION; 3-DIMENSIONAL VISUALIZATION; NONSTOICHIOMETRY; LA0.6SR0.4CO0.8FE0.2O3-DELTA; PEROVSKITES; CRYSTAL;
D O I
10.1016/j.jssc.2012.03.021
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
To study the local structure and oxygen ion conduction mechanism in (La0.6Sr0.4)(Co0.2Fe0.8)O-3-delta (LSCF) as a function of the oxygen partial pressure (P(O-2)), in situ the Co and Fe K-edge X-ray absorption spectroscopy (XAS) was measured at elevated temperatures of 900 and 1000 K. The reduction of the Co and Fe valence, i.e., the oxygen content (3 - delta) in LSCF, followed the change of P(O-2) from 1 to 10(-4) atm during similar to 4000 s. The quantitative analysis of the X-ray absorption near edge structure (XANES) and the extended X-ray absorption fine structure (EXAFS) indicated that the Fe valence was higher than the Co valence at oxidative condition (delta approximate to 0) in LSCF. Whereas the Co valence decreased more than the Fe valence after reduction of P(O-2) at both 900 and 1000 K. From the relaxation plots of the valence and the oxygen content (3 - delta) for Co and Fe after changing P(O-2), we successfully determined D-chem and E-a of an oxygen ion migration around Co and Fe in LSCF. A structural model with and without oxygen vacancies and an oxygen ion conduction mechanism for LSCF are proposed based on these results. (C) 2012 Elsevier Inc. All rights reserved.
引用
收藏
页码:38 / 46
页数:9
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