Abstract
The mineral aluminite has been studied using a number of techniques, including scanning electron microscopy (SEM) with energy dispersive spectroscopy (EDX) and Raman and infrared spectroscopy. Raman spectroscopy identifies multiple sulphate symmetric stretching modes in line with the three sulphate crystallographically different sites. Raman spectroscopy also identifies a low intensity band at 1069cm−1 which may be attributed to a carbonate symmetric stretching mode, indicating the presence of thaumasite. The observation of multiple bands in this ν4 spectral region offers evidence for the reduction in symmetry of the sulphate anion from Td to C2v or even lower symmetry. The Raman band at 3588cm−1 is assigned to the OH unit stretching vibration and the broad feature at around 3439cm−1 to water stretching bands. Water stretching vibrations are observed at 3157, 3294, 3378 and 3439cm−1. Vibrational spectroscopy enables an assessment of the molecular structure of aluminite to be made.
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