Spectroscopic characterization of natural chrysotile

被引：48
作者：
Anbalagan, G. [1 ]
Sivakumar, G. [2 ]
Prabakaran, A. R. [3 ]
Gunasekaran, S. [3 ]
机构：
[1] Presidency Coll, PG & Res Dept Phys, Madras 5, Tamil Nadu, India
[2] Annamalai Univ, Dept Phys, CISL, Chidambaram 2, India
[3] Pachaiyappas Coll, PG & Res Dept Phys, Madras 30, Tamil Nadu, India
来源：
VIBRATIONAL SPECTROSCOPY | 2010年 / 52卷 / 02期
关键词：
Chrysotile; FT-IR; FT-Raman; EPR; (29)Si NMR; (27)Al NMR; X-RAY-DIFFRACTION; SERPENTINE MINERALS; RAMAN SPECTROSCOPY; INFRARED-SPECTRA; SI-29; NMR; IDENTIFICATION; ASBESTOS; PHYLLOSILICATES; REFLECTANCE;
D O I：
10.1016/j.vibspec.2009.11.007
中图分类号：
O65 [分析化学];
学科分类号：
070302 ; 081704 ;
摘要：
Chrysotile, a variety of serpentine mineral was investigated by vibrational and magnetic resonance spectroscopic methods. The SEM photograph of the sample shows that chrysotile is made up of thin and flexible fibrils, classified as asbestos. The calculated lattice parameters were a = 5.1961 +/- 0.0053 angstrom. b = 9.2365 +/- 0.0107 angstrom, c = 14.6208 +/- 0.0039 angstrom; beta = 90.15 +/- 0.19 degrees; Z = 4, with space group C2/m. Three bands observed in the highest wavenumber region (3689 and 3648 cm(-1)) originate from the stretching vibrations of the two crystallographically different OH groups. The Raman spectrum shows bending vibrations of the SiO(4) tetrahedra at 390 and 348 cm(-1). Substitution of the Si ions in SiO(4) tetrahedra by Al ions leads to low-field shifts in the (29)Si NMR spectrum and the resonance line corresponding to Q(3) (1 Al) was observed at -89 ppm. This result was supported by the resonance line at approximate to 57 ppm in (27)Al NMR spectrum. (C) 2009 Elsevier B.V. All rights reserved.
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页码：122 / 127
页数：6
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