Raman spectroscopy of halotrichite from Jaroso, Spain

被引:20
作者
Frost, RL
Weier, ML
Kloprogge, JT
Rull, F
Martinez-Frias, J
机构
[1] Queensland Univ Technol, Sch Phys & Chem Sci, Inorgan Mat Res Program, Brisbane, Qld 4001, Australia
[2] Univ Valladolid, CSIC, INTA, Ctr Astrobiol,Unidad Asociada, Valladolid 47006, Spain
基金
澳大利亚研究理事会;
关键词
sulphate; halotrichite; jarosite; Raman spectroscopy;
D O I
10.1016/j.saa.2004.12.023
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
Raman spectroscopy complimented with infrared ATR spectroscopy has been used to characterise a halotrichite FeSO4 center dot Al-2(SO4)(3)center dot 22H(2)O from The Jaroso Ravine, Aquilas, Spain. Halotrichites form a continuous solid solution series with pickingerite and chemical analysis shows that the jarosite contains 6% Mg2+. Halotrichite is characterised by four infrared bands at 3569.5, 3485.7, 3371.4 and 3239.0 cm(-1). Using Libowitsky type relationships, hydrogen bond distances of 3.08, 2.876, 2.780 and 2.718 angstrom were determined. Two intense Raman bands are observed at 987.7 and 984.4 cm(-1) and are assigned to the v, symmetric stretching vibrations of the sulphate bonded to the Fe2+ and the water units in the structure. Three sulphate bands are observed at 77 K at 1000.0, 991.3 and 985.0 cm(-1) suggesting further differentiation of the sulphate units. Raman spectrum of the v(2) and v(4) region of halotrichite at 298 K shows two bands at 445.1 and 466.9 cm(-1), and 624.2 and 605.5 cm(-1), respectively, confirming the reduction of symmetry of the sulphate in halotrichite. (c) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:176 / 180
页数:5
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