Raman spectroscopic study of synthetic reevesite and cobalt substituted reevesite (Ni,Co)6Fe2(OH)16(CO3)•4H2O

被引:28
作者
Frost, Ray L. [1 ]
Bakon, Kathleen H. [1 ]
Palmer, Sara J. [1 ]
机构
[1] Queensland Univ Technol, Sch Phys & Chem Sci, Inorgan Mat Res Program, Brisbane, Qld 4001, Australia
基金
澳大利亚研究理事会;
关键词
hydrotalcite; brucite; reevesite; Raman microscopy; carrboydite; hydrohonessite; takovite; mountkeithite; WOLF CREEK METEORITE; CRYSTAL-STRUCTURES; PYROAURITE; MINERALS; NICKEL; PECORAITE; SULFATE; HYDROHONESSITE; HYDROTALCITE; CARRBOYDITE;
D O I
10.1002/jrs.2280
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
Raman spectroscopy, complemented with infrared spectroscopy of compounds equivalent to reevesite, formula (Ni,Co)(6)Fe-2(OH)(16)(CO3)center dot 4H(2)O, with the ratio of Ni/Co ranging from 0 to 1, have been synthesised and characterised based on the molecular structure of the synthesised mineral. The combination of Raman spectroscopy with infrared spectroscopy enables an assessment of bands attributable to water stretching and brucite-like surface hydroxyl units to be obtained. Raman spectroscopy shows a reduction in the symmetry of the carbonate anion, leading to the conclusion that the carbonate anion is bonded to the brucite-like hydroxyl surface and to the water in the interlayer. Variation in the position of the carbonate anion stretching vibrations occurs and is dependent on the Ni/Co ratio. Water bending modes are identified in both the Raman and infrared spectra at positions greater than 1620 cm(-1), indicating that water is strongly hydrogen bonded to both the interlayer anions and the hydrotalcite surface. Copyright (C) 2009 John Wiley & Sons, Ltd.
引用
收藏
页码:78 / 83
页数:6
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