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A vibrational spectroscopic study of the silicate mineral ardennite-(As)
被引:9
|作者:
Frost, Ray L.
[1
]
Lopez, Andres
[1
]
Xi, Yunfei
[1
]
Scholz, Ricardo
[2
]
Gandini, Antonio Luciano
[2
]
机构:
[1] Queensland Univ Technol, Sch Chem Phys & Mech Engn, Fac Sci & Engn, Brisbane, Qld 4001, Australia
[2] Univ Fed Ouro Preto, Dept Geol, Sch Mines, BR-3540000 Ouro Preto, MG, Brazil
基金:
澳大利亚研究理事会;
关键词:
Silicate;
Raman spectroscopy;
Ardennite-(As);
Infrared spectroscopy;
Adsorbed water;
CRYSTAL-STRUCTURE;
ALPS;
D O I:
10.1016/j.saa.2013.09.148
中图分类号:
O433 [光谱学];
学科分类号:
0703 ;
070302 ;
摘要:
We have used a combination of scanning electron microscopy with EDX and vibrational spectroscopy to study the mineral ardennite-(As). The mineral ardennite-(As) of accepted formula Mn-4(2+)(Al,Mg)(6)(Si3O10) (SiO4)(2)(AsO4,VO4)(OH)(6) is a silicate mineral which may contain arsenate and/or vanadates anions. Because of the oxyanions present, the mineral lends itself to analysis by Raman and infrared spectroscopy. Qualitative chemical analysis shows a homogeneous phase, composed by Si, Mn, Al and As. Ca and V were also observed in partial substitution for Mn and As. Raman bands at 1197, 1225, 1287 and 1394 cm(-1) are assigned to SiO stretching vibrations. The strong Raman bands at 779 and 877 cm(-1) are assigned to the AsO43- antisymmetric and symmetric stretching vibrations. The Raman band at 352 cm(-1) is assigned to the nu(2) symmetric bending vibration. The series of Raman bands between 414 and 471 cm(-1) are assigned to the v(4) out of plane bending modes of the AsO43- units. Intense Raman bands observed at 301 and 314 cm(-1) are attributed to the MnO stretching and bending vibrations. Raman bands at 3041, 3149, 3211 and 3298 cm(-1) are attributed to the stretching vibrations of OH units. There is vibrational spectroscopic evidence for the presence of water adsorbed on the ardennite-(As) surfaces. (C) 2013 Elsevier B.V. All rights reserved.
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页码:987 / 991
页数:5
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