Redox behavior and transport properties of La0.5-xSr0.5-xFe0.4Ti0.6O3-δ (0<x<0.1) validated by Mossbauer spectroscopy

被引:21
作者
Fagg, DP [1 ]
Waerenborgh, JC
Kharton, VV
Frade, JR
机构
[1] Univ Aveiro, UIMC, Dept Ceram & Glass Engn, P-3810193 Aveiro, Portugal
[2] Inst Tecnol & Nucl, Dept Chem, P-2686953 Sacavem, Portugal
[3] Belarusian State Univ, Inst Physicochem Problems, Minsk 220080, BELARUS
关键词
perovskite; titanate-ferrite; Mossbauer spectroscopy; electrical conductivity; reduction;
D O I
10.1016/S0167-2738(01)01000-1
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 range of perovskite-type solid solution formation in the system La0.5-xSr0.5-xTi0.6Fe0.4O3-delta in oxidizing conditions is determined from X-ray diffraction and Mossbauer spectroscopy data to correspond to approximately 0-10% of the A-site concentration, similar to other numerous perovskite systems. Reduction and subsequent reoxidation of the oxides leads to a narrowing of this range and the segregation of the hematite phase at x = 0.05. Increasing A-site deficiency results in the formation of oxygen vacancies and decreasing stability in reducing environments. The total conductivity of La0.5-xSr0.5-xTi0.6Fe0.4O3-delta. (x=0.02-0.10) ceramics is essentially independent of composition in air and increases with increasing x in reducing atmospheres, due to increasing concentrations of n-type charge carriers and the formation of metallic iron. Partial decomposition of the perovskite phase in hydrogen, resulting in metal Fe formation, was found to be reversible when the A-site deficiency is small (x<0.05). Mossbauer spectroscopic data showed that, contrary to other perovskite-type titanates-ferrites, the concentration of Fe4+ cations in the perovskite lattice of oxidized La0.5-xSr0.5-xTi0.6Fe0.O-4(3-delta) is negligible. (C) 2002 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:87 / 93
页数:7
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