Synthesis and Ionic Conduction of Cation-deficient Apatite La9.33-2x/3MxSi6O26 Doped with Mg,Ca,Sr
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Synthesis and Ionic Conduction of Cation-deficient Apatite La9.33-2x/3MxSi6O26 Doped with Mg,Ca,Sr
Synthesis and Ionic Conduction of Cation-deficient Apatite La9.33-2x/3MxSi6O26 Doped with Mg,Ca,Sr
中国化学工程学报(英文版)2008年16卷第3期 页码:488-491
Affiliations:
1. Guangdong Key Laboratory of Green Chemicals, College of Chemical Engineering and Energy, South China University of Technology,Guangzhou,China,510640
2. College of Environmental and Engineering, South China University of Technology,Guangzhou,China,510640
Author bio:
Funds:
Natural Science Foundation of Guangdong Province (06025657);Guangdong Provincial Green Chemicals
DOI:
中图分类号:
纸质出版:2008
Accepted:
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袁文辉, 顾亚萍, 李莉. Synthesis and Ionic Conduction of Cation-deficient Apatite La9.33-2x/3MxSi6O26 Doped with Mg,Ca,Sr[J]. 中国化学工程学报(英文版), 2008,16(3):488-491.
M
袁文辉, 顾亚萍, 李莉. Synthesis and Ionic Conduction of Cation-deficient Apatite La9.33-2x/3MxSi6O26 Doped with Mg,Ca,Sr[J]. 中国化学工程学报(英文版), 2008,16(3):488-491.DOI:
MDOI:
Synthesis and Ionic Conduction of Cation-deficient Apatite La9.33-2x/3MxSi6O26 Doped with Mg,Ca,Sr
Apatite-type lanthanum silicate with special conduction mechanism via interstitial oxygen has attracted considerable interest in recent years. In this work
pure powder of La
9.33-2x/3
M
x
Si
6
O
26
(M=Mg
Ca
Sr) is prepared by the sol-gel method with sintering at 1000℃. The powder is characterized by X-ray diffraction (XRD) and scanning electron micrograph (SEM). The apatite can be obtained at relatively low temperature as compared to the conventional solid-state reaction method. The measurements of conductivity of a series of doped samples La
9.33-2x/3
M
x
Si
6
O
26
(M=Ca
Mg
Sr) indicate that the type of dopant and the amount have a significant effect on the conductivity. The greatest decrease in conductivity is observed for Mg doping
following the Ca and the Sr doped apatites. The effect is ultimately attributed to the amount of oxygen interstitials
which is affected by the crystal lattice distortion arising from cation vacancies.
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