A vibrational spectroscopic study of the silicate mineral harmotome - (Ba,Na,K)1-2(Si,Al)8O16•6H2O - A natural zeolite

被引:3
|
作者
Frost, Ray L. [1 ]
Lopez, Andres [1 ]
Wang, Lina [1 ,2 ]
Romano, Antonio Wilson [3 ]
Scholz, Ricardo [4 ]
机构
[1] Queensland Univ Technol, Fac Sci & Engn, Sch Chem Phys & Mech Engn, Brisbane, Qld 4001, Australia
[2] Tianjin Univ Technol, Sch Chem & Chem Engn, Tianjin, Peoples R China
[3] Univ Fed Minas Gerais, Dept Geol, BR-31270901 Belo Horizonte, MG, Brazil
[4] Univ Fed Ouro Preto, Sch Mines, Dept Geol, BR-3540000 Ouro Preto, MG, Brazil
基金
澳大利亚研究理事会;
关键词
Harmotome; Zeolite; Barium; Silicate; Raman spectroscopy; Infrared spectroscopy; TETRAHEDRA; CRYSTALS; GLASSES;
D O I
10.1016/j.saa.2014.07.072
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
The mineral harmotome (Ba,Na,K)(1-2)(Si,Al)(8)O-16 center dot 6H(2)O is a crystalline sodium calcium silicate which has the potential to be used in plaster boards and other industrial applications. It is a natural zeolite with catalytic potential. Raman bands at 1020 and 1102 cm(-1) are assigned to the SiO stretching vibrations of three dimensional siloxane units. Raman bands at 428, 470 and 491 cm(-1) are assigned to OSiO bending modes. The broad Raman bands at around 699, 728, 768 cm(-1) are attributed to water librational modes. Intense Raman bands in the 3100 to 3800 cm(-1) spectral range are assigned to OH stretching vibrations of water in harmotome. Infrared spectra are in harmony with the Raman spectra. A sharp infrared band at 3731 cm(-1) is assigned to the OH stretching vibration of SiOH units. Raman spectroscopy with complimentary infrared spectroscopy enables the characterization of the silicate mineral harmotome. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:70 / 74
页数:5
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