Choudhary G. & Fernandes S. (2011) Spectroscopic examination of commercially available quartz varieties- a gemmological perspective. Presented at GIA International Gemmological Symposium 2011 held at Carlsbad, California on 29-30 May 2011. Abstract in proceedings volume.
The lack of inclusions and visible growth features (colour zoning) makes the separation of colourless natural and synthetic quartz quite challenging. Though found colourless in nature, it can also be produced by heating other quartz varieties, such as amethyst, citrine, smoky, green (praseolite), and greenish yellow (lemon). Rock crystal, the purest variety of quartz, often contains aluminum (Al3+) impurities where the charge imbalance is compensated by a nearby interstitial alkali ion; this is a precursor for smoky quartz, which is produced by natural or artificial irradiation. Iron impurities, having different charge states, result in green (Fe2+), yellow (Fe3+), and violet (Fe4+). As a result, both natural and synthetic materials can be heated to 250-500ºC to produce the colourless variety. Infrared spectra offer the most valuable means for differentiating between natural and synthetic quartz, and for correlating the features observed in the spectroscopic data with colour varieties of natural and synthetic material. In our study, the OH, Al-OH/Li, Al-OH, Si-O / Al-OH, and Si-O related peaks at around 3593, 3480, 3379, 3305, and 3198 cm-1 consistently appeared in natural rock crystal, while the 3584, 3421, 3297, and 3198 cm-1 peaks were present in synthetic rock crystal; the most important peak in distinguishing natural from synthetic crystals was at 3480 cm-1. The data also help differentiate between natural and synthetic versions of other coloured varieties and whether the colour is natural or produced by heating.
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