A SEM, EDS and vibrational spectroscopic study of the tellurite mineral: Sonoraite Fe3+Te4+O3(OH)•H2O

被引:3
作者
Frost, Ray L. [1 ]
Lopez, Andres [1 ]
Scholz, Ricardo [2 ]
机构
[1] Queensland Univ Technol, Sch Chem Phys & Mech Engn, Fac Sci & Engn, Brisbane, Qld 4001, Australia
[2] 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
Tellurite; Sonoraite; Cliffordite; Keystoneite; Raman spectroscopy; Infrared spectroscopy; ZEMANNITE;
D O I
10.1016/j.saa.2015.03.089
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
We have undertaken a study of the tellurite mineral sonorite using electron microscopy with EDX combined with vibrational spectroscopy. Chemical analysis shows a homogeneous composition, with predominance of Te, Fe, Ce and In with minor amounts of S. Raman spectroscopy has been used to study the mineral sonoraite an examples of group A(XO3), with hydroxyl and water units in the mineral structure. The free tellurite ion has C-3v symmetry and four modes, 2A(1) and 2E. An intense Raman band at 734 cm(-1) is assigned to the v(1) (TeO3)(2-) symmetric stretching mode. A band at 636 cm(-1) is assigned to the v(3) (TeO3)(2-) antisymmetric stretching mode. Bands at 350 and 373 cm(-1) and the two bands at 425 and 438 cm(-1) are assigned to the (TeO3)(2-) v(2) (A(1)) bending mode and (TeO3)(2-) v(4) (E) bending modes. The sharp band at 3283 cm(-1) assigned to the OH stretching vibration of the OH units is superimposed upon a broader spectral profile with Raman bands at 3215, 3302, 3349 and 3415 cm(-1) are attributed to water stretching bands. The techniques of Raman and infrared spectroscopy are excellent for the study of tellurite minerals. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:225 / 229
页数:5
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