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A vibrational spectroscopic study of tengerite-(Y) Y2(CO3)3 2–3H2O

[Display omitted] •The mineral tengerite-(Y) has been studied by vibrational spectroscopy.•Multiple carbonate stretching modes support the concept of non-equivalent carbonate units.•Intense sharp bands at 464, 479 and 508cm−1 are assigned to YO stretching modes.•Multiple Raman and infrared bands in...

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Bibliographic Details
Published in:Spectrochimica acta. Part A, Molecular and biomolecular spectroscopy Molecular and biomolecular spectroscopy, 2015-02, Vol.137, p.612-616
Main Authors: Frost, Ray L., López, Andrés, Wang, Lina, Scholz, Ricardo, Sampaio, Ney Pinheiro, de Oliveira, Fernando A.N.
Format: Article
Language:English
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Summary:[Display omitted] •The mineral tengerite-(Y) has been studied by vibrational spectroscopy.•Multiple carbonate stretching modes support the concept of non-equivalent carbonate units.•Intense sharp bands at 464, 479 and 508cm−1 are assigned to YO stretching modes.•Multiple Raman and infrared bands in the OH stretching region are observed. The mineral tengerite-(Y) has been studied by vibrational spectroscopy. Multiple carbonate stretching modes are observed and support the concept of non-equivalent carbonate units in the tengerite-(Y) structure. Intense sharp bands at 464, 479 and 508cm−1 are assigned to YO stretching modes. Raman bands at 765 and 775cm−1 are assigned to the CO32− ν4 bending modes and Raman bands at 589, 611, 674 and 689cm−1 are assigned to the CO32− ν2 bending modes. Multiple Raman and infrared bands in the OH stretching region are observed, proving the existence of water in different molecular environments in the structure of tengerite-(Y).
ISSN:1386-1425
DOI:10.1016/j.saa.2014.08.107