Please use this identifier to cite or link to this item: http://www.repositorio.ufop.br/handle/123456789/4342
Title: Vibrational spectroscopic study of the sulphate mineral glaucocerinite (Zn,Cu)10Al6(SO4)3(OH)32-18H2O - a natural layered double hydroxide.
Authors: Frost, Ray Leslie
Theiss, Frederick L.
López, Andrés
Cipriano, Ricardo Augusto Scholz
Keywords: Raman spectroscopy
Glaucocerinite
Sulphate
Infrared spectroscopy
Issue Date: 2014
Citation: FROST, R. L. et al. Vibrational spectroscopic study of the sulphate mineral glaucocerinite (Zn,Cu)10Al6(SO4)3(OH)32-18H2O - a natural layered double hydroxide. Spectrochimica Acta. Part A, Molecular and Biomolecular Spectroscopy, v. 127, p. 349-353, 2014. Disponível em: <http://www.sciencedirect.com/science/article/pii/S138614251400273X>. Acesso em: 07 out. 2014.
Abstract: We have studied the molecular structure of the mineral glaucocerinite (Zn,Cu)5Al3(SO4)1.5(OH)16_9(H2O) using a combination of Raman and infrared spectroscopy. The mineral is one of the hydrotalcite supergroup of natural layered double hydroxides. The Raman spectrum is characterised by an intense Raman band at 982 cm_1 with a low intensity band at 1083 cm_1. These bands are attributed to the sulphate symmetric and antisymmetric stretching mode. The infrared spectrum is quite broad with a peak at 1020 cm_1. A series of Raman bands at 546, 584, 602, 625 and 651 cm_1 are assigned to the m4 (SO4)2_ bending modes. The observation of multiple bands provides evidence for the reduction in symmetry of the sulphate anion from Td to C2v or even lower symmetry. The Raman band at 762 cm_1 is attributed to a hydroxyl deformation mode associated with AlOH units. Vibrational spectroscopy enables aspects of the molecular structure of glaucocerinite to be determined.
URI: http://www.repositorio.ufop.br/handle/123456789/4342
metadata.dc.identifier.doi: https://doi.org/10.1016/j.saa.2014.02.086
ISSN: 1386-1425
metadata.dc.rights.license: O periódico Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy concede permissão para depósito deste artigo no Repositório Institucional da UFOP. Número da licença 3487300090327.
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