Effect of the lanthanide ionic radius on the Raman spectroscopy of lanthanide agardite minerals

被引:8
作者
Frost, RL
Erickson, KL
Weier, ML
McKinnon, AR
Williams, PA
Leverett, P
机构
[1] Queensland Univ Technol, Sch Phys & Chem Sci, Inorgan Mat Res Program, Brisbane, Qld 4001, Australia
[2] Univ Western Sydney, Sch Sci, Penrith, NSW 1797, Australia
关键词
agardite; goudeyite; mixite; petersite;
D O I
10.1002/jrs.1243
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
Raman microscopy was used to study the Raman spectra of a series of rare earth element agardites ACU(6)(AsO4)(3)(OH)(6)(.)3H(2)O, where A = lanthanicle(3+). These minerals have a porous framework similar to that of zeolites with a structure based on (A(3+))(1-x)(A(2+))(x)CU6(OH)(6)(AsO4)(3-x)(AsO3OH)(x). Two sets of AsO stretching vibrations were found and assigned to the vibrational modes of AsO4 and HAsO4 units. The position of selected bands was found to be sensitive to the lanthanide ionic radius. Raman spectra of the low-wavenumber region are complex. Bending modes of the AsO4 and HAsO4 units were found to be sensitive to the ionic radius of the lanthanide ion. Linear relationships between positions of the Raman bands were derived, with correlation coefficients > 0.90. Copyright (C) 2004 John Wiley Sons, Ltd.
引用
收藏
页码:961 / 966
页数:6
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