Crystal structure of Fe-doped lanthanum gallate for oxygen partial pressures studied by neutron powder diffraction

被引:0
作者
Mori, Kazuhiro [1 ]
Kiyanagi, Ryoji [2 ]
Richardson, James W., Jr. [2 ]
Fieramosca, Joe [2 ]
Onodera, Yohei [1 ]
Itoh, Keiji [1 ]
Sugiyama, Masaaki [1 ]
Kamiyama, Takashi [3 ]
Fukunaga, Toshiharu [1 ]
机构
[1] Kyoto Univ, Inst Res Reactor, Kumatori, Osaka 5900494, Japan
[2] Argonne Natl Lab, Div Intense Pulsed Neutron Source, Argonne, IL 60439 USA
[3] High Energy Accelerator Res Org, Inst Mat Struct Sci, Tsukuba, Ibaraki 3050801, Japan
关键词
Mixed conductor; LaGaO(3); Fe-doping; Perovskite structure; Neutron diffraction; PEROVSKITE-TYPE OXIDE; IONIC-CONDUCTIVITY; CO; NI;
D O I
10.1016/j.ssi.2008.07.001
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
Neutron powder diffraction experiments were carried out to investigate a change in a crystal structure of La(0.8)Sr(0.2)Ga(0.65)Fe(0.35)O(3) for oxygen partial pressures, P(O2), at 800 degrees C. The crystal structure was refined on the basis of the R3c syrnmetry for the P(O2) range from 10(-1) to 10(-20) atm, by the Rietveld analysis. It was found that lattice parameters, a and c, monotonically expand with decreasing P(O2), and then both expansions are rapidly suppressed below 10(-4) atm. In the meantime, I(M-O) and I(O-O)(2) also discontinuously increased with decreasing P(O2), while I(O-O)(1) did not change at all P(O2), where I(M-O), I(O-O)(1) and I(O-O)(2) are the bond lengths within a MO(6) octahedron (M = Ga(0.65)Fe(0.35)). This result indicates that the I(M-O) and the I(O-O)(2) are more important than the I(O-O)(1) for such a complicated lattice expansion for P(O2). (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:541 / 545
页数:5
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