Raman spectroscopy of dawsonite NaAl(CO3)(OH)2

被引:68
作者
Frost, Ray L. [1 ]
Bouzaid, Jocelyn M. [1 ]
机构
[1] Queensland Univ Technol, Inorgan Mat Res Program, Sch Phys & Chem Sci, Brisbane, Qld 4001, Australia
关键词
barentsite; dawsonite; tunisite; smithsonite; carbonate; hydroxyl; infrared and Raman spectroscopy; MONT SAINT-HILAIRE; CHEMICAL UTILIZATION; CARBONATE; MINERALS; ALUMINUM; AL;
D O I
10.1002/jrs.1733
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
Raman spectroscopy both at 298 and 77 K complemented with infrared spectroscopy was used to study the structure of dawsonite. Previous crystallographic studies concluded that the structure of dawsonite was a simple one; however, both Raman and infrared spectroscopy show that this conclusion is incorrect. Multiple bands are observed in both the Raman and infrared spectra in the antisymmetric stretching and bending regions, showing that the symmetry of the carbonate anion is reduced and in all probability the carbonate anions are not equivalent in the dawsonite structure. Multiple OH deformation vibrations centred around 950 cm(-1) in both Raman and infrared spectra show that the OH units in the dawsonite structure are non-equivalent. Calculations using the position of the Raman and infrared OH stretching vibrations enabled estimates of the hydrogen-bond distances of 0.2735 and 0.27219 pm at 298 K, and 0.27315 and 0.2713 pm at 77 K to be made. This indicates strong hydrogen bonding of the OH units in the dawsonite structure. Copyright (C) 2007 John Wiley & Sons, Ltd.
引用
收藏
页码:873 / 879
页数:7
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