More On Coated Topaz

(via Gemmology Queensland, Vol 3, No.6, July 2002)

Blue, bluish green, and green surface-diffused topaz that are produced in the USA by heat diffusion of a cobalt rich (› blue) or cobalt and nickel rich (› green) powders, have been marketed since 1998. The color, which is uniform to the naked eye, is confined to a thin layer on or jut below the surface of the treated colorless topaz. When examined (immersed) under magnification the diffused layer has a patchy color distribution. Chipped facets reveal underlying colorless topaz. This coating may produce anomalous (› 1.81) reading with the gem refractometer. When examined with the VIS spectroscope, cobalt absorption bands at 560, 590 and 640nm are visible, and this color-enhanced topaz commonly gives a red response when examined with the Chelsea filter.

Well….a new coated topaz has appeared on the market. This treated topaz, that has a brownish ‘imperial’ topaz color was created by Prof Vladimir Balitsky of the Mineralogical Institute, Russian Academy of Sciences. Details of this new treatment were revealed in his recent lecture to The Gemmological Association of All Japan.

The starting material is faceted F-bearing colorless topaz that is coated with a thin layer of iron oxide by heat diffusion. This thin coating gives the topaz a brownish yellow color. When the coating is examined in tangential illumination the facet displays a high, iridescent luster. As the coating is comparatively soft, it is readily abraded and chipped thus exposing the underlying colorless topaz. Refractive indices from the coated facets were 1.61 – 1.62 (normal for F-topaz, including yellow or brown topaz), but the coated topaz did not display the orange LWUV fluorescence normally displayed by imperial (OH-type) topaz.

The Professor remarked that hydrothermally grown synthetic topaz will be soon released on to the world market.