Infrared and Raman spectroscopic characterization of the carbonate mineral huanghoite - And in comparison with selected rare earth carbonates

被引:21
|
作者
Frost, Ray L. [1 ]
Lopez, Andres [1 ]
Scholz, Ricardo [2 ]
Xi, Yunfei [1 ]
Belotti, Fernanda Maria [3 ]
机构
[1] Queensland Univ Technol, Fac Sci & Engn, Sch Chem Phys & Mech Engn, Brisbane, Qld 4001, Australia
[2] Univ Fed Ouro Preto, Sch Mines, Dept Geol, BR-3540000 Ouro Preto, MG, Brazil
[3] Univ Fed Itajuba, Itabira, MG, Brazil
基金
澳大利亚研究理事会;
关键词
Huanghoite; Carbonate; Molecular structure; Raman spectroscopy; Infrared spectroscopy; ELECTRON-MICROSCOPY; CRYSTAL-STRUCTURE; NB DEPOSIT; PARISITE-(CE); REE; POLYTYPES; ARSENATE;
D O I
10.1016/j.molstruc.2013.07.051
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Raman spectroscopy complimented with infrared spectroscopy has been used to study the rare earth based mineral huanghoite with possible formula given as BaCe(CO3)(2)F and compared with the Raman spectra of a series of selected natural halogenated carbonates from different origins including bastnasite, parisite and northupite. The Raman spectrum of huanghoite displays three bands are at 1072, 1084 and 1091 cm(-1) attributed to the CO symmetric stretching vibration. The observation of three symmetric stretching vibrations is very unusual. The position of CO32- symmetric stretching vibration varies with mineral composition. Infrared spectroscopy of huanghoite show bands at 1319, 1382, 1422 and 1470 cm(-1). No Raman bands of huanghoite were observed in these positions. Raman spectra of bastnasite, parisite and northupite show a single band at 1433, 1420 and 1554 cm(-1) assigned to the v(3) (CO3)(2-) antisymmetric stretching mode. The observation of additional Raman bands for the v(3) modes for some halogenated carbonates is significant in that it shows distortion of the carbonate anion in the mineral structure. Four Raman bands for huanghoite are observed at 687, 704, 718 and 730 cm-land assigned to the (CO3)(2)- v(2) bending modes. Raman bands are observed for huanghoite at around 627 cm(-1) and are assigned to the (CO3)2- v(4) bending modes. Raman bands are observed for the carbonate v(4) in phase bending modes at 722 cm(-1) for bastnasite, 736 and 684 cm(-1) for parisite, 714 cm(-1) for northupite. Raman bands for huanghoite observed at 3259, 3484 and 3589 cm(-1) are attributed to water stretching bands. Multiple bands are observed in the OH stretching region for bastnasite and parisite indicating the presence of water and OH units in their mineral structure. Vibrational spectroscopy enables new information on the structure of huanghoite to be assessed. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:221 / 225
页数:5
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