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La9.33Si6O26 Oxygen ionic conductor was synthesized by solid state reaction method. Its structure was determined by single-crystal X-ray diffraction analysis at room temperature. The results showed that La9.33Si6O26 oxide has the apatite structure with space group P63/m. AC impedance measurements indicated that the oxides sintered in nitrogen have much higher conductivity than those sintered in air. The effects of grain boundaries on the conductivity were discussed.

参考文献

[1] R A George;N F Besstte .[J].Journal of Power Sources,1998,71:131.
[2] T Kudo;H Obayashi .[J].Journal of the Electrochemical Society,1976,123:415.
[3] P O Battle;C R A Catlow;J W Heapand;L.M.Moroney .[J].Journal of Solid State Chemistry,1986,63:8.
[4] T Ishihara;T Shibayama;S Ishikawa;K.Hosoi,H.Nishiguchi Y.Takita .[J].Journal of the European Ceramic Society,2004,24:1329.
[5] S Nakayama;H Aono;Y Sadaoka .[J].Chemistry Letters,1995,24:431.
[6] S Nakayama;T Kageyama;H Aono;Y.Sadaoka .[J].Journal of Materials Chemistry,1995,5:1801.
[7] H Arikawa;N Nishiguchi;T Ishiihara;Y.Takita .[J].Solid-State Ionicis,2000,136-137:31.
[8] S Tao;J T S Irvine .[J].Materials Research Bulletin,2001,36:1245.
[9] S Nakayama;M Sakamoto;M Higuchi;K.Kodaira,M.Sata,S.Kakita,T.Suzuki K.Itoh .[J].Journal of the European Ceramic Society,1999,19:507.
[10] J E H Sansom;D Richings;P R Slater .[J].Solid-State Ionicis,2001,139:205.
[11] H Okudera;Y Masubuchi;S Kikkawa;A.Yoshiasa .[J].Solid-State Ionicis,2005,176:1473.
[12] X-RED 1.08a,STOE Data Reduction Program[M].STOE & Cie GmbH Darmstadt,Germany,1996
[13] X-SHAPE 1.02,Crystal Optimisation for Numerical Absorption Correction[M].STOE & Cie GmbH Darmstadt,Germany,1996
[14] P J Panteix;I Julien;D Bernache-Assollant;P.Abelard .[J].Materials Chemistry and Physics,2006,95:313.
[15] S Nakayama;M Sakamoto .[J].Journal of the European Ceramic Society,1998,18:1413.
[16] J R Tolchard;M S Islam;P R Slater .[J].Journal of Materials Chemistry,2003,13:1956.
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