dc.contributor.author |
Ranatunge, D. |
|
dc.contributor.author |
Fernando, G.W.A.R. |
|
dc.date.accessioned |
2019-06-04T07:25:16Z |
|
dc.date.available |
2019-06-04T07:25:16Z |
|
dc.date.issued |
2015 |
|
dc.identifier.citation |
Ranatunge, D. and G.W.A.R. Fernando (2015). Powder XRD Study of Gem Quality Corundum (Alpha-Al2O3): A Qualitative Method to Identify Synthetic and Natural Corundum, Proceedings of the 31st Technical Session of Geological Society of Sri Lanka, Published Online - 27th February 2015 (http://www.gsslweb.org), p.13. |
en_US |
dc.identifier.issn |
www.gsslweb.org |
|
dc.identifier.uri |
http://repository.ou.ac.lk/handle/94ousl/391 |
|
dc.description.abstract |
Differentiation of synthetic and natural gemstones is a chief concern for gem dealers and major jewellery importers. Natural corundum is a precious stone and, one of the most important exports of Sri Lanka. Corundum (α – Al2O3) is known by different names depending on the colour it exhibits which in turn depends on the impurities that are present. The colour depends on the valence state of the impurity element present in corundum such as Cr3+ in ruby, Fe3+ in yellow sapphire and Fe-Ti complex in blue sapphire. There have been a number of incidences of synthetically grown corundum available in the market which cannot easily be differentiated with natural corundum with normal routine tests. Present paper deals with the X ray powder diffraction results on different colours of natural and synthetic gem quality corundum and gives evidence of an external morphology and internal growth features that reflect their formation conditions, especially disorder brought about by such synthetic treatments. This can be effectively used for diagnostic purposes for detecting the synthetic stones. Four (04) sets of corundum samples from different origins, both natural and synthetic have been analysed at the Industrial Technology Institute (ITI) for X ray powder diffraction (XRD). The characteristic set of d-spacings generated in a typical X-ray scan provides a unique "fingerprint" of the mineral or minerals present in the sample. The positions and the intensities of the peaks are used for identifying the underlying structure (or phase) of the material. The XRD results of both natural and synthetic corundum samples were found to be consistent with the standard international reference of corundum. Broadening of the peak was measured by calculating the Full Width at Half Maximum (FWHM) of the peak. Then, a graph was drawn as 2θ vs FWHM to find the behaviour of the broadening of the peaks. According to comparison of 4 sets of different colours of corundum, it was observed that shifting of XRD peaks of synthetic corundum are considerably high and high strain could be seen in synthetic corundums than that of natural variety. |
en_US |
dc.language.iso |
en_US |
en_US |
dc.publisher |
Geological Society of Sri Lanka |
en_US |
dc.relation.ispartofseries |
31;13 |
|
dc.subject |
gemstones |
en_US |
dc.subject |
Sri Lanka |
en_US |
dc.subject |
synthetic ruby |
en_US |
dc.subject |
natural Ruby |
en_US |
dc.subject |
XRD |
en_US |
dc.subject |
Full Width at Half Maximum (FWHM) |
en_US |
dc.title |
Powder XRD Study of Gem Quality Corundum (Alpha-Al2O3): A Qualitative Method to Identify Synthetic and Natural Corundum |
en_US |
dc.type |
Other |
en_US |