Raman and infrared study of phyllosilicates containing heavy metals (Sb, Bi): bismutoferrite and chapmanite

被引:30
作者
Frost, Ray L. [1 ]
Bahfenne, Silmarilly [1 ]
Cejka, Jiri [1 ,2 ]
Sejkora, Jiri [2 ]
Plasil, Jakub [2 ]
Palmer, Sara J. [1 ]
机构
[1] Queensland Univ Technol, Inorgan Mat Res Program, Sch Phys & Chem Sci, Brisbane, Qld 4001, Australia
[2] Natl Museum, CZ-11579 Prague 1, Czech Republic
基金
澳大利亚研究理事会;
关键词
bismutoferrite; chapmanite; kaolinite; Raman spectroscopy; infrared spectroscopy; hydroxyl ions; adsorbed water; hydrogen bonds; VIBRATIONAL SPECTROSCOPY; LAYERED SILICATES; MINERALS; KAOLINITE; SPECTRA;
D O I
10.1002/jrs.2512
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
The kaolinite-like phyllosilicate minerals bismutoferrite BiFe(2)(3+)Si(2)O(8)(OH) and chapmanite SbFe(2)(3+)Si(2)O(8)(OH) have been studied by Raman spectroscopy and complemented with infrared spectra. Tentatively interpreted spectra were related to their molecular structure. The antisymmetric and symmetric stretching vibrations of the Si-O-Si bridges, delta SiOSi and delta OSiO bending vibrations, nu (Si-O(terminal)) stretching vibrations, nu OH stretching vibrations of hydroxyl ions, and delta OH bending vibrations were attributed to the observed bands. Infrared bands in the range 3289-3470 cm(-1) and Raman bands in the range 1590-1667 cm(-1) were assigned to adsorbed water. O-H center dot center dot center dot O hydrogen-bond lengths were calculated from the Raman and infrared spectra. Copyright (C) 2009 John Wiley & Sons, Ltd.
引用
收藏
页码:814 / 819
页数:6
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