Float zone growth and characterization of Pr9.33(SiO4)6O2 and Sm9.33(SiO4)6O2 single crystals with an apatite structure

被引:41
作者
Higuchi, M [1 ]
Katase, H
Kodaira, K
Nakayama, S
机构
[1] Hokkaido Univ, Grad Sch Engn, Div Mat Sci & Engn, Sapporo, Hokkaido 0608628, Japan
[2] Niihama Natl Coll Technol, Niihama 7928580, Japan
关键词
praseodymium silicate; samarium silicate; apatite structure; floating zone method; oxide ionic conductivity;
D O I
10.1016/S0022-0248(00)00577-7
中图分类号
O7 [晶体学];
学科分类号
0702 ; 070205 ; 0703 ; 080501 ;
摘要
Single crystals of apatite-type praseodymium silicate (Pr-9.33(SiO4)(6)O-2) and samarium silicate (Sm-9.33(SiO4)(6)O-2) with high oxide ionic conductivity have been grown by the floating zone method. The as-grown crystals of Pr-9.33(SiO4)(6)O-2 and Sm-9.33(SiO4)(6)O-2 are green and orange, respectively, and both crystals are transparent. The crystals do not contain inclusions, low-angle grain boundaries or twin structures but the samarium silicate crystals contain a few cracks perpendicular to the c-axis whereas the praseodymium silicate crystals are crack-free. Microcracks are also introduced in the samarium silicate crystals during the cutting and polishing processes. The oxide ionic conductivities of these crystals are comparable to that of neodymium silicate with the same structure. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:282 / 286
页数:5
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