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Wednesday, April 25, 2007

Dyed Natural Corundum As A Ruby Imitation

(via ICA Early Warning Flash, No.50, December 11, 1991) SSEF writes:

The following observations were made in the SSEF laboratory and further during examination of stones by Dr K Schmetzer and Mr F J Schupp, Germany.

Submitted stone chains and faceted stones were consisting of a heavily fractured type of natural corundum material, probably stained during quench cracking. They were sold as originating from India. The flattened beads were up to 15mm in diameter, the faceted oval stones between 5 and 8 carats.

Closer examination under the microscope reveals that the red color is deposited on irregular fracture planes only. The material is colored by a violetish red stain, the result of an artificial fracture treatment. The color is similar to the color of somewhat dark ruby and makes a convincing ruby imitation.

The stones show natural inclusions which consist of sets of parallel twin lamellae in one or two directions, forming straight intersection lines. Boehmite particles are confined to these intersection lines. Small double refractive mineral inclusions forming clusters were also observed. Stones with similar properties are known by us to come from East Africa. In immersion, light yellow or greenish yellow portions are forming areas between the fractures, showing the original color of the material. The red color is only seen in fractures. In thick pieces, the artificial treatment (i.e the stained fractures) is more difficult to see.

Beside of the above, the treated material can be recognized by a yellow fluorescence under long wave UV radiation. The red artificial color is said to fade after exposure of some weeks to daylight. Also the rather uneven color distribution on the fractures, as seen under magnification, is diagnostic.

The chromophore element of ruby is chromium. The easiest way to prove its presence in corundum is by observing the absorption spectrum with a pocket spectroscope. Chromium causes a prominent set of absorption lines and a fluorescence doublet in the red part of the spectrum. These characteristics are not visible in the dyed corundum since they lack chromium and therefore are not ruby.

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