Infrared and Raman spectroscopic characterization of the carbonate mineral weloganite - Sr3Na2Zr(CO3)6•3H2O and in comparison with selected carbonates

被引:14
作者
Frost, Ray L. [1 ]
Xi, Yunfei [1 ]
Scholz, Ricardo [2 ]
Belotti, Fernanda Maria [3 ]
Candido Filho, Mauro [4 ]
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, BR-35903087 Itabira, MG, Brazil
[4] Univ Fed Ouro Preto, Sch Mines, Min Engineer Dept, BR-3540000 Ouro Preto, MG, Brazil
基金
澳大利亚研究理事会;
关键词
Raman spectroscopy; Weloganite; Carbonate; Infrared spectroscopy; Zirconium; MALACHITE; AZURITE;
D O I
10.1016/j.molstruc.2013.02.005
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
The mineral weloganite Na2Sr3Zr(CO3)(6)center dot 3H(2)O has been studied by using vibrational spectroscopy and a comparison is made with the spectra of weloganite with other carbonate minerals. Weloganite is member of the mckelveyite group that includes donnayite-(Y) and mckelveyite-(Y). The Raman spectrum of weloganite is characterized by an intense band at 1082 cm(-1) with shoulder bands at 1061 and 1073 cm(-1), attributed to the CO32- symmetric stretching vibration. The observation of three symmetric stretching vibrations is very unusual. The position of CO32- symmetric stretching vibration varies with mineral composition. The Raman bands at 1350, 1371, 1385, 1417, 1526, 1546, and 1563 cm(-1) are assigned to the v(3)(CO3)(2-) antisymmetric stretching mode. The observation of additional Raman bands for the v(3) modes for weloganite is significant in that it shows distortion of the carbonate anion in the mineral structure. The Raman band observed at 870 cm(-1) is assigned to the (CO3)(2-) v(2) bending mode. Raman bands observed for weloganite at 679, 682, 696, 728, 736, 749, and 762 cm(-1) are assigned to the (CO3)(2-) v(4) bending modes. A comparison of the vibrational spectra is made with that of the rare earth carbonates decrespignyite, bastnasite, hydroxybastnasite, parisite, and northupite. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:101 / 106
页数:6
相关论文
共 20 条
[1]  
ADLER HH, 1963, AM MINERAL, V48, P839
[2]  
Aleksandrov I.V., 1965, ZAP VSER MINERAL OBS, V94, P323
[3]  
Back ME, 2008, MINERALOGICAL RECORD
[4]  
Chen T. T., 1975, CAN MINERAL, V13, P22
[5]  
Fan HR, 2003, ACTA PETROL SIN, V19, P169
[6]  
Farmer V.C., 1974, Mineralogical Society Monograph 4: The Infrared Spectra of Minerals, 1974
[7]   Raman spectroscopy of halogen-containing carbonates [J].
Frost, Ray L. ;
Dickfos, Marilla J. .
JOURNAL OF RAMAN SPECTROSCOPY, 2007, 38 (11) :1516-1522
[8]   Thermal stability of azurite and malachite in relation to the formation of mediaeval glass and glazes [J].
Frost, RL ;
Ding, Z ;
Kloprogge, JT ;
Martens, WN .
THERMOCHIMICA ACTA, 2002, 390 (1-2) :133-144
[9]   Raman spectroscopic study of azurite and malachite at 298 and 77 K [J].
Frost, RL ;
Martens, WN ;
Rintoul, L ;
Mahmutagic, E ;
Kloprogge, JT .
JOURNAL OF RAMAN SPECTROSCOPY, 2002, 33 (04) :252-259
[10]   INFRA-RED SPECTRA OF AZURITE AND MALACHITE [J].
GOLDSMITH, JA ;
ROSS, SD .
SPECTROCHIMICA ACTA PART A-MOLECULAR SPECTROSCOPY, 1968, A 24 (12) :2131-+