""This paper relates an infrared (IR) (6000–2500; 1400–400 cm−1) spectroscopic study of sideronatrite, Na2Fe3+(SO4)2(OH)·3H2O. Spectra in the 600–1250 cm−1 range are dominated by fundamental S–O absorption bands. Factor-group analysis based on the space group P212121 (Formula ) is in accordance with the observed band multiplicity. A broad and convolute absorption centred around 3400 cm−1 and a sharp band at 3605 cm−1 are observed in the 2900–3900 cm−1 frequency region. The resolution of the broad band is significantly improved at liquid nitrogen temperature; seven components can be fitted to the pattern and these can be assigned to H2O\\\/OH molecules in the structure. All components in the broad band and the sharp absorption at 3605 cm−1 are strongly polarized for E\\\/\\\/a, in accordance with the structure analysis results. Infrared transmission spectroscopy is a useful tool to identify these sulfate minerals occurring in specific geological environments. ""

DELLA VENTURA, G., Ventruti, G., Bellatreccia, F., Scordari, F., Cestelli Guidi, M. (2013). FTIR transmission spectroscopy of sideronatrite, a sodium-iron hydrous sulfate. MINERALOGICAL MAGAZINE, 77, 499-507 [10.1180/minmag.2013.077.4.09].

FTIR transmission spectroscopy of sideronatrite, a sodium-iron hydrous sulfate

DELLA VENTURA, Giancarlo;BELLATRECCIA, FABIO;
2013-01-01

Abstract

""This paper relates an infrared (IR) (6000–2500; 1400–400 cm−1) spectroscopic study of sideronatrite, Na2Fe3+(SO4)2(OH)·3H2O. Spectra in the 600–1250 cm−1 range are dominated by fundamental S–O absorption bands. Factor-group analysis based on the space group P212121 (Formula ) is in accordance with the observed band multiplicity. A broad and convolute absorption centred around 3400 cm−1 and a sharp band at 3605 cm−1 are observed in the 2900–3900 cm−1 frequency region. The resolution of the broad band is significantly improved at liquid nitrogen temperature; seven components can be fitted to the pattern and these can be assigned to H2O\\\/OH molecules in the structure. All components in the broad band and the sharp absorption at 3605 cm−1 are strongly polarized for E\\\/\\\/a, in accordance with the structure analysis results. Infrared transmission spectroscopy is a useful tool to identify these sulfate minerals occurring in specific geological environments. ""
2013
DELLA VENTURA, G., Ventruti, G., Bellatreccia, F., Scordari, F., Cestelli Guidi, M. (2013). FTIR transmission spectroscopy of sideronatrite, a sodium-iron hydrous sulfate. MINERALOGICAL MAGAZINE, 77, 499-507 [10.1180/minmag.2013.077.4.09].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11590/267653
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