OH-groups in natural perovskite - An IR spectroscopic study

被引:4
作者
Beran, A [1 ]
Libowitzky, E [1 ]
机构
[1] UNIV BERN,LAB CHEM & MINERAL KRISTALLOG,CH-3012 BERN,SWITZERLAND
关键词
perovskite; trace hydroxyl; microFTIR-spectroscopy;
D O I
10.1080/01411599608242405
中图分类号
O7 [晶体学];
学科分类号
0702 ; 070205 ; 0703 ; 080501 ;
摘要
IR spectra of a natural CaTiO3 perovskite single-crystal show two absorption bands at 3394 and 3326 cm(-1) which are attributed to structural OH defects. The two bands are weakly pleochroic in a (001) section, but show a more distinct anisotropic behaviour in (110) with a stronger component of absorption perpendicular to [001]. A plausible model for the mode of OH incorporation on a preferred atomic position is derivable under the assumption of vacancies in the Ca-lattice. An OH dipole direction roughly pointing along [110] with O2 oxygens acting as donor oxygens is consistent with the measured pleochroic scheme of the bands.
引用
收藏
页码:211 / 215
页数:5
相关论文
共 6 条
[1]  
BERAN A, 1996, IN PRESS CAN MINERAL, V34
[2]  
GILLET P, 1993, PHYS CHEM MINER, V20, P141
[3]  
HU L, 1992, AM MINERAL, V77, P359
[4]   SYNCHROTRON INFRARED ABSORBENCY MEASUREMENTS OF HYDROGEN IN MGSIO3 PEROVSKITE [J].
MEADE, C ;
REFFNER, JA ;
ITO, E .
SCIENCE, 1994, 264 (5165) :1558-1560
[5]  
Novak A., 1974, Large Molecules, V18, DOI [10.1007/BFb0116438, DOI 10.1007/BFB0116438]
[6]  
PATERSON MS, 1982, B MINERAL, V105, P20