(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.
Wednesday, April 18, 2007
Chinese Pearl Enhancement Techniques
(Gemmology Queensland, Volume 3, No.6, June 2002)
According to Guo & Shi on pages 32-36 of Volume XXII of The Journal of the Gemmological Association of Hong Kong, Chinese pearl processors apply a range of enhancement technology to both their freshwater and saltwater cultured pearls. These routine treatments include:
- Pre treatment
- Bleaching
- Increasing whiteness
- Adding luster
- Dyeing
- Polishing
Pre Treatment
Pre-treatment process includes sorting, drilling, expansion and dehydration steps. Pearls are sorted on the basis of thickness of nacre, color, luster, shape and size. Drilling allows stringing and setting removes some external defects, and is an essential prerequisite for subsequent treatments for reducing oil content, bleaching, adding whiteness and dyeing pearls. Expansion looses the pearl’s structure and so facilitates future treatment. Two techniques of expansion are used at a temperature of 70-80°C and for times that depend on the depth of color of the pearl (darker color, more time). These techniques of expansion are:
- Heating pearls that have been wrapped in gauze in deionized water.
- Immersion of pearls in an unspecified liquid.
- Dehydration follows expansion. The removal of water from cracks in the pearl is accomplished by immersion in anhydrous ethanol and glycerol.
Bleaching
Bleaching is used to create white pearls and to remove disfiguring colors and stains from the pearls. The common bleaching solution consists of a mixture of hydrogen peroxide, a solvent of surface active reagent (detergent), and a pH stability regulator. Factors affecting the efficiency of bleaching include concentration of hydrogen peroxide, temperature pH of bleaching solution, composition of surface active agent, pH stabilizer and solvent duration of light exposure, and the frequency of stirring and renewal of the bleaching solution.
Two formulations are commonly used for bleaching pearls:
- Hydrogen peroxide carbinol ammonia, 12-alkyl sodium sulphate, Britton-Robinson buffer solvent.
- Hydrogen peroxide chloroform, ethanol amine, 12-alkyl sodium sulphate, Britton-Robinson buffer solvent.
- Common bleaching conditions are a temperature of 30-35°C in association with light exposure. Hydrogen peroxide of 2-3% is commonly used, while bleaching times range from 2-3 days for light colored pearls to more than 10 days for darker colored pearls. The bleaching solution is changed every four days.
Increasing Whiteness
Following bleaching some pearls still retail a yellowish tone due to the presence of pigments resistant to the bleaching effect of hydrogen peroxide. These pearls are further treated with a fluorescent whitener. This is a dye molecule that is activated by the UV in visible light to emit a bluish fluorescence which neutralizes the residual yellow color of pearl and produces a whiter pearl. A Swiss manufactured whitener FP, dissolved in acetone and the surface active agents acrylic acid for 12-alkyl sodium sulphate is the fluorescence whitener commonly used on Chinese pearls.
Adding Luster
This is claimed to be one of the most important processes in pearl enhancement. It involves immersing the pearls in a weakly alkaline TGP (magnesium compounds) solution and keeping them constantly stirred at even temperature for several days.
Dyeing
As bleached pearls usually have some residual uneven color, they are dyed to yield fashionable and marketable colors. Specific dyes are used to produce predictable colors, e.g. potassium permanganate solution with golden NH-R yields golden pearls, while Luo Dan Ming B in alcohol produces pink pearls. These dyes can be either water, oil or alcohol based.
Polishing
Polishing, the last step enhances both the smoothness and luster of the pearls. This step involves surface polishing, usually by tumbling in a mild abrasive, followed by coating of the pearls with a thin layer of wax.
The Problem
- Which of these treatments should be detected?
- Which of these treatments should be disclosed?
According to Guo & Shi on pages 32-36 of Volume XXII of The Journal of the Gemmological Association of Hong Kong, Chinese pearl processors apply a range of enhancement technology to both their freshwater and saltwater cultured pearls. These routine treatments include:
- Pre treatment
- Bleaching
- Increasing whiteness
- Adding luster
- Dyeing
- Polishing
Pre Treatment
Pre-treatment process includes sorting, drilling, expansion and dehydration steps. Pearls are sorted on the basis of thickness of nacre, color, luster, shape and size. Drilling allows stringing and setting removes some external defects, and is an essential prerequisite for subsequent treatments for reducing oil content, bleaching, adding whiteness and dyeing pearls. Expansion looses the pearl’s structure and so facilitates future treatment. Two techniques of expansion are used at a temperature of 70-80°C and for times that depend on the depth of color of the pearl (darker color, more time). These techniques of expansion are:
- Heating pearls that have been wrapped in gauze in deionized water.
- Immersion of pearls in an unspecified liquid.
- Dehydration follows expansion. The removal of water from cracks in the pearl is accomplished by immersion in anhydrous ethanol and glycerol.
Bleaching
Bleaching is used to create white pearls and to remove disfiguring colors and stains from the pearls. The common bleaching solution consists of a mixture of hydrogen peroxide, a solvent of surface active reagent (detergent), and a pH stability regulator. Factors affecting the efficiency of bleaching include concentration of hydrogen peroxide, temperature pH of bleaching solution, composition of surface active agent, pH stabilizer and solvent duration of light exposure, and the frequency of stirring and renewal of the bleaching solution.
Two formulations are commonly used for bleaching pearls:
- Hydrogen peroxide carbinol ammonia, 12-alkyl sodium sulphate, Britton-Robinson buffer solvent.
- Hydrogen peroxide chloroform, ethanol amine, 12-alkyl sodium sulphate, Britton-Robinson buffer solvent.
- Common bleaching conditions are a temperature of 30-35°C in association with light exposure. Hydrogen peroxide of 2-3% is commonly used, while bleaching times range from 2-3 days for light colored pearls to more than 10 days for darker colored pearls. The bleaching solution is changed every four days.
Increasing Whiteness
Following bleaching some pearls still retail a yellowish tone due to the presence of pigments resistant to the bleaching effect of hydrogen peroxide. These pearls are further treated with a fluorescent whitener. This is a dye molecule that is activated by the UV in visible light to emit a bluish fluorescence which neutralizes the residual yellow color of pearl and produces a whiter pearl. A Swiss manufactured whitener FP, dissolved in acetone and the surface active agents acrylic acid for 12-alkyl sodium sulphate is the fluorescence whitener commonly used on Chinese pearls.
Adding Luster
This is claimed to be one of the most important processes in pearl enhancement. It involves immersing the pearls in a weakly alkaline TGP (magnesium compounds) solution and keeping them constantly stirred at even temperature for several days.
Dyeing
As bleached pearls usually have some residual uneven color, they are dyed to yield fashionable and marketable colors. Specific dyes are used to produce predictable colors, e.g. potassium permanganate solution with golden NH-R yields golden pearls, while Luo Dan Ming B in alcohol produces pink pearls. These dyes can be either water, oil or alcohol based.
Polishing
Polishing, the last step enhances both the smoothness and luster of the pearls. This step involves surface polishing, usually by tumbling in a mild abrasive, followed by coating of the pearls with a thin layer of wax.
The Problem
- Which of these treatments should be detected?
- Which of these treatments should be disclosed?
Stanthorpe’s Green Diamond
(via Gemmology Queensland, Volume 3, No.9, September 2002 / The Queensland Government Mining Journal of 15th April, 1924)
A Sad Tale
In a letter to the Brisbane Daily Mail, Mr Oscar Meston (Mining Warden at Stanthorpe) writes:
“On 10th March a cable from London stated that the only known green diamond in existence would be exhibited at the Wembley Exhibition. It weighs a carat and a half, is worth £1750, and was found in the Transvaal in 1923. The Stanthorpe mineral field has produced a rival to this remarkable gem. A few years ago my eye was attracted by ‘coruscation’ from a heap of tailings on an abandoned tin claim. I discovered the source of the light to be a small green stone, which I immediately recognized as a diamond. It was a perfect octahedron, pale green in color, flawless, and a limpid beauty—and it weighed two carats and a half. The surface showed very fine striations, evidently caused by movement under enormous pressure. I offered the stone to several gem merchants in Sydney, but found them almost as adamant as the diamond itself. Their chief objection was the excessive hardness of the Australian diamond and consequent lapidarian difficulties. The utmost I could obtain for the stone was 20 guineas. On the basis of valuation of the Transvaal stone, I lost approximately £2900 on the transaction.”
A Sad Tale
In a letter to the Brisbane Daily Mail, Mr Oscar Meston (Mining Warden at Stanthorpe) writes:
“On 10th March a cable from London stated that the only known green diamond in existence would be exhibited at the Wembley Exhibition. It weighs a carat and a half, is worth £1750, and was found in the Transvaal in 1923. The Stanthorpe mineral field has produced a rival to this remarkable gem. A few years ago my eye was attracted by ‘coruscation’ from a heap of tailings on an abandoned tin claim. I discovered the source of the light to be a small green stone, which I immediately recognized as a diamond. It was a perfect octahedron, pale green in color, flawless, and a limpid beauty—and it weighed two carats and a half. The surface showed very fine striations, evidently caused by movement under enormous pressure. I offered the stone to several gem merchants in Sydney, but found them almost as adamant as the diamond itself. Their chief objection was the excessive hardness of the Australian diamond and consequent lapidarian difficulties. The utmost I could obtain for the stone was 20 guineas. On the basis of valuation of the Transvaal stone, I lost approximately £2900 on the transaction.”
Every One Needs A 10x
(How to) Use it seriously
(via Gemmology Queensland, No.3. No 6, July 2002) Trevor Linton writes:
Carry it all the time and use it as much as possible every day. A 10x lens increases knowledge. A 10x is the first and possibly the most serious instrument used by both the amateur and professional when investigating a gemstone’s features and information as to its origin.
The hand lens, (10x or times—10) is a combination of lenses that provides magnified detail to the observer. It is the most important instrument you can use when an unknown gemstone is given to you either for purchase or for identification. Do not dismiss this step of the investigation into a gemstone during your quest for information, as the hand lens is the only instrument that provides an overall view of a gemstone. The 10x hand lens, in experienced hands, and under quality lighting, can provide essential identification features on 90 percent of gemstones: by noting hardness, refractive index, birefringence, dichroism and dispersion as well as indications of the gemstone’s origin from inclusions and many methods of man’s treatment.
The quality of a 10x hand lens is usually dependant on price, which can vary from A $10 to $320 depending on its type, source, manufacturer and country of origin. There are three main lens combinations that govern the quality of the lens: the plano-convex doublet, the achromatic doublet, and the compound triplet. Each has its advantages and disadvantages.
The first type, the economic doublet has two simple crown glass lenses facing each other at approximately two thirds of their focal length. This combination of lenses provides a 40 percent field of vision that is in reasonable focus and has a relatively flat field. When observing a sheet of squared paper with the doublet, an image appears. This is suitable for rough investigation of stones, but when serious images of a flat facet are required, it leaves a lot to be desired……as straight lines are curved, only the center is in focus as the observed field is curved through a doublet. The colors red and blue are not in focus with green. The advantage for the doublet is economy. A lot of detail can be gathered for a small outlay of dollars with a doublet. Chromatic aberration is usually not a great influence with gemstones as only highlights are refracted in to the differing points of color focus that produce color fringing. Most gemstone observations are in gemstones of one color or colorless gemstones.
Increased color resolution is achieved with a flint glass lens cemented to the inside a double sided convex crown glass lens forming an achromatic compound lens that corrects for the chromatic aberrations that defocus colors in a lens system. This second type of lens system produces straight lines over most of the field of view. An achromatic doublet is a very good, yet still economic 10x system of lenses.
The third lens type, the triplet lens, is a solid system of glass lenses using three layers of glass cemented together forming an aplanatic (in a plane) triplet. The image of a flat plane forms as a plane at the point of focus. This is the best system for hand lenses, when correctly designed and used under normal observation. A triplet has minimal spherical and chromatic aberration and a flat field.
When purchasing a hand lens, buy one that is better than you initially need. If you buy the best triplet lens, use it to your advantage. That s what the whole project should be about. You have to achieve quality observation. There is little advantage in using a quality lens without good lighting and knowledge of how to use both.
When using the hand lens there are several basic rules, and many techniques to develop:
- Spectacles should not be worn unless severe optical defects are present within eyes.
- Choose a good quality light source, with a very narrow beam of high intensity light directed on to your work area and not spilling light towards your eye or the background.
- Work over a soft white cloth that allows easy pick up of gemstones with tweezers. This soft cloth also prevents dropped gemstones from bouncing off the work area on to the floor.
- Clean the sample free from dust and grease (fingerprints) with a lint free cloth. A quality glasses cleaning cloth is suitable.
- Always pick up gemstones with tweezers after cleaning.
- When using the right eye hold the hand lens in the right hand about 25mm in front of the eye, with the index finger primary knuckle resting on the neck.
- Keep both eyes open. This can occur with experience. When the closed eye lid flutters letting light in there is a complimentary iris movement in the open eye.
- Holding the lens close to the eye with one hand, bring the gemstone close with the other hand and rest both hands together for stability. Position the stone 25mm in front of the lens with the gem’s surface in focus, under the light.
- Ensure the lens is straight in front of your eye and is not twisted. Looking off the central axis will produce ‘coma’ color fringing on all images that severely limit quality observing.
- Work systematically around the surface of all faceted gemstones before being drawn into the gems interior. There are many features available for observation, especially around the girdle. Gemstones such as diamond reveal their true nature on the girdle, with natural crystal surfaces left on opposite side of the girdle as the cutters try to achieve maximum weight from the rough stone. The treatment of the girdle or how it was formed is a good guide to the cutting quality and whether care was taken during the gem’s manufacture.
- Do not neglect other features such as flat facets and sharp facet edges that indicate hard gemstones. Concave facets or molding marks at the girdle indicate cast glass. Reflect a fluorescent tube image from the facet for an image of a straight flat facet. Surface luster of facet edges chips indicates the refractive index of the gemstone. Try looking at glass or quartz and comparing surface chips with those on sapphire or diamond. Yes diamond does chip before it cleaves in to two diamonds.
The history of a gemstone’s growth, and subsequent heat and coloring activities induced by man, occurs in the gem’s inclusions. Your 10x hand lens will reveal many of these features under these proposed lighting techniques of use.
Inclusion types have a greater listing than there are gemstone types. Quartz alone has 550 officially listed inclusion types. Quartz is a low temperature forming gemstone; it is of the last to crystallize and includes many other gems that form before it does. Pegmatites in which quartz forms have plenty of liquid and gas so there are many of these inclusions in the ‘veils’ that form within fractures of quartz crystal.
Igneous (volcanic) gemstones can be easily distinguished from metamorphic gems by the individual suites of inclusions within each type. Man-made gems may be chemically identical with those of nature, but man’s techniques of manufacturing these gems create characteristic inclusions that are identifiable with your 10x hand lens.
An interesting feature is found on many older gemstones when a flat plane of air bubbles are glued in a layer between the crown and pavilion of a doublet. These are very easily found with a hand lens. Dispersion of color at individual facets is a good indicator of high refractive index and hardness.
Other hand lenses in use through the industry, such as the Coddington lens and the darkfield loupe have specific features for overcoming specific problems. For example, The Coddington lens is a solid glass cylinder with a restricting light aperture half way at its focal point. This light restriction reduces many aberration errors by preventing them passing the restriction. The darkfield loupe provides correct darkfield lighting for identifying small inclusions in gemstones and direction specific illumination on fracture fill inclusions. This is a small pocket portable, torch based instrument that has power full application in the diamond market of Europe, USA and Asia.
Recommendations
- Use your 10x for it can increase your knowledge and understanding of gemstones.
- A 10x lens is so much faster to use than a microscope that requires more detailed observation. Wear it out as soon as possible and buy a better quality lens as a Christmas present to yourself. If an excuse is needed, it will improve your observing and self-confidence. Do no think that the old 10x will do for the time being.
- Your 10x lens will repay with valuable information.
- Understanding information from a 10x depends on experience gained from informed and correct use f your most important instrument.
(via Gemmology Queensland, No.3. No 6, July 2002) Trevor Linton writes:
Carry it all the time and use it as much as possible every day. A 10x lens increases knowledge. A 10x is the first and possibly the most serious instrument used by both the amateur and professional when investigating a gemstone’s features and information as to its origin.
The hand lens, (10x or times—10) is a combination of lenses that provides magnified detail to the observer. It is the most important instrument you can use when an unknown gemstone is given to you either for purchase or for identification. Do not dismiss this step of the investigation into a gemstone during your quest for information, as the hand lens is the only instrument that provides an overall view of a gemstone. The 10x hand lens, in experienced hands, and under quality lighting, can provide essential identification features on 90 percent of gemstones: by noting hardness, refractive index, birefringence, dichroism and dispersion as well as indications of the gemstone’s origin from inclusions and many methods of man’s treatment.
The quality of a 10x hand lens is usually dependant on price, which can vary from A $10 to $320 depending on its type, source, manufacturer and country of origin. There are three main lens combinations that govern the quality of the lens: the plano-convex doublet, the achromatic doublet, and the compound triplet. Each has its advantages and disadvantages.
The first type, the economic doublet has two simple crown glass lenses facing each other at approximately two thirds of their focal length. This combination of lenses provides a 40 percent field of vision that is in reasonable focus and has a relatively flat field. When observing a sheet of squared paper with the doublet, an image appears. This is suitable for rough investigation of stones, but when serious images of a flat facet are required, it leaves a lot to be desired……as straight lines are curved, only the center is in focus as the observed field is curved through a doublet. The colors red and blue are not in focus with green. The advantage for the doublet is economy. A lot of detail can be gathered for a small outlay of dollars with a doublet. Chromatic aberration is usually not a great influence with gemstones as only highlights are refracted in to the differing points of color focus that produce color fringing. Most gemstone observations are in gemstones of one color or colorless gemstones.
Increased color resolution is achieved with a flint glass lens cemented to the inside a double sided convex crown glass lens forming an achromatic compound lens that corrects for the chromatic aberrations that defocus colors in a lens system. This second type of lens system produces straight lines over most of the field of view. An achromatic doublet is a very good, yet still economic 10x system of lenses.
The third lens type, the triplet lens, is a solid system of glass lenses using three layers of glass cemented together forming an aplanatic (in a plane) triplet. The image of a flat plane forms as a plane at the point of focus. This is the best system for hand lenses, when correctly designed and used under normal observation. A triplet has minimal spherical and chromatic aberration and a flat field.
When purchasing a hand lens, buy one that is better than you initially need. If you buy the best triplet lens, use it to your advantage. That s what the whole project should be about. You have to achieve quality observation. There is little advantage in using a quality lens without good lighting and knowledge of how to use both.
When using the hand lens there are several basic rules, and many techniques to develop:
- Spectacles should not be worn unless severe optical defects are present within eyes.
- Choose a good quality light source, with a very narrow beam of high intensity light directed on to your work area and not spilling light towards your eye or the background.
- Work over a soft white cloth that allows easy pick up of gemstones with tweezers. This soft cloth also prevents dropped gemstones from bouncing off the work area on to the floor.
- Clean the sample free from dust and grease (fingerprints) with a lint free cloth. A quality glasses cleaning cloth is suitable.
- Always pick up gemstones with tweezers after cleaning.
- When using the right eye hold the hand lens in the right hand about 25mm in front of the eye, with the index finger primary knuckle resting on the neck.
- Keep both eyes open. This can occur with experience. When the closed eye lid flutters letting light in there is a complimentary iris movement in the open eye.
- Holding the lens close to the eye with one hand, bring the gemstone close with the other hand and rest both hands together for stability. Position the stone 25mm in front of the lens with the gem’s surface in focus, under the light.
- Ensure the lens is straight in front of your eye and is not twisted. Looking off the central axis will produce ‘coma’ color fringing on all images that severely limit quality observing.
- Work systematically around the surface of all faceted gemstones before being drawn into the gems interior. There are many features available for observation, especially around the girdle. Gemstones such as diamond reveal their true nature on the girdle, with natural crystal surfaces left on opposite side of the girdle as the cutters try to achieve maximum weight from the rough stone. The treatment of the girdle or how it was formed is a good guide to the cutting quality and whether care was taken during the gem’s manufacture.
- Do not neglect other features such as flat facets and sharp facet edges that indicate hard gemstones. Concave facets or molding marks at the girdle indicate cast glass. Reflect a fluorescent tube image from the facet for an image of a straight flat facet. Surface luster of facet edges chips indicates the refractive index of the gemstone. Try looking at glass or quartz and comparing surface chips with those on sapphire or diamond. Yes diamond does chip before it cleaves in to two diamonds.
The history of a gemstone’s growth, and subsequent heat and coloring activities induced by man, occurs in the gem’s inclusions. Your 10x hand lens will reveal many of these features under these proposed lighting techniques of use.
Inclusion types have a greater listing than there are gemstone types. Quartz alone has 550 officially listed inclusion types. Quartz is a low temperature forming gemstone; it is of the last to crystallize and includes many other gems that form before it does. Pegmatites in which quartz forms have plenty of liquid and gas so there are many of these inclusions in the ‘veils’ that form within fractures of quartz crystal.
Igneous (volcanic) gemstones can be easily distinguished from metamorphic gems by the individual suites of inclusions within each type. Man-made gems may be chemically identical with those of nature, but man’s techniques of manufacturing these gems create characteristic inclusions that are identifiable with your 10x hand lens.
An interesting feature is found on many older gemstones when a flat plane of air bubbles are glued in a layer between the crown and pavilion of a doublet. These are very easily found with a hand lens. Dispersion of color at individual facets is a good indicator of high refractive index and hardness.
Other hand lenses in use through the industry, such as the Coddington lens and the darkfield loupe have specific features for overcoming specific problems. For example, The Coddington lens is a solid glass cylinder with a restricting light aperture half way at its focal point. This light restriction reduces many aberration errors by preventing them passing the restriction. The darkfield loupe provides correct darkfield lighting for identifying small inclusions in gemstones and direction specific illumination on fracture fill inclusions. This is a small pocket portable, torch based instrument that has power full application in the diamond market of Europe, USA and Asia.
Recommendations
- Use your 10x for it can increase your knowledge and understanding of gemstones.
- A 10x lens is so much faster to use than a microscope that requires more detailed observation. Wear it out as soon as possible and buy a better quality lens as a Christmas present to yourself. If an excuse is needed, it will improve your observing and self-confidence. Do no think that the old 10x will do for the time being.
- Your 10x lens will repay with valuable information.
- Understanding information from a 10x depends on experience gained from informed and correct use f your most important instrument.
Tuesday, April 17, 2007
Natural Forsterite And Synthetic Forsterite
(via Gemmology Queensland, Vol.4, No.1, January 2003) Hiroshi Kitawaki writes:
Forsterite is one of the end member minerals in the olivine group of minerals. It was named after a British mineral collector Jacob Forster.
Many solid solutions of olivine minerals are known, among which forsterite and fayalite form an isomorphous series. A yellow green crystal, with intermediate composition in this isomorphous series is called peridot. This gemstone is a birthstone of August and is one of the popular gemstones. On the other hand, forsterite is not common a as gemstone.
A forsterite that a chemical formula of, or close to, the end member is rare because one element (Mg) in the formula is generally replaced easily by Fe in nature. The mineral, forsterite, is found in ultrabasic rock or dolomitic limestone that had gone through thermal metamorphism.
Natural Forsterite
The green stone described in this report is a natural forsterite that we recently investigated and it is said to be from Sri Lanka according to its client. Its RI measured 1.635 – 1.670 with DR 0.035. The SG was 3.29 and the stone was inert to UV light. Directionally oriented minute needle-like inclusions were observed under magnification. Its compositional analysis by X-ray fluorescence detected considerable amount of Fe and very small amount of Ca and Mn as well as the main elements of Mg and Si.
Crystals within the olivine group have been extensively studied, and used in heat resistant materials, insulators or lasers. Among the crystals used in industry, single crystal forsterite of high quality and large size have been synthesized by the crystal pulling method for use as crystals that laze the near infrared.
Synthetic forsterite
Synthetic forsterite, which is marketed as Tanzaniod has been synthesized in Russia for gem use. As you can easily imagine from its name, it is meant to imitate tanzanite. The RI, DR and SG of the Tanzaniod are consistent with those of natural forsterite, with Tanzaniod fluorescing a weak orange to yellow and greenish yellow under long and short wave ultraviolet lights respectively. Prominent pleochroism of blue and violet is also recognized. Under the hand-held spectroscope, absorption bands are seen on 490nm, 520nm and 580nm. Dot-like and short needle-like inclusions are observed under magnification. The compositional analysis by fluorescent X-ray detected considerable amount of Co and V, other than the main elements of Mg and Si.
Forsterite is one of the end member minerals in the olivine group of minerals. It was named after a British mineral collector Jacob Forster.
Many solid solutions of olivine minerals are known, among which forsterite and fayalite form an isomorphous series. A yellow green crystal, with intermediate composition in this isomorphous series is called peridot. This gemstone is a birthstone of August and is one of the popular gemstones. On the other hand, forsterite is not common a as gemstone.
A forsterite that a chemical formula of, or close to, the end member is rare because one element (Mg) in the formula is generally replaced easily by Fe in nature. The mineral, forsterite, is found in ultrabasic rock or dolomitic limestone that had gone through thermal metamorphism.
Natural Forsterite
The green stone described in this report is a natural forsterite that we recently investigated and it is said to be from Sri Lanka according to its client. Its RI measured 1.635 – 1.670 with DR 0.035. The SG was 3.29 and the stone was inert to UV light. Directionally oriented minute needle-like inclusions were observed under magnification. Its compositional analysis by X-ray fluorescence detected considerable amount of Fe and very small amount of Ca and Mn as well as the main elements of Mg and Si.
Crystals within the olivine group have been extensively studied, and used in heat resistant materials, insulators or lasers. Among the crystals used in industry, single crystal forsterite of high quality and large size have been synthesized by the crystal pulling method for use as crystals that laze the near infrared.
Synthetic forsterite
Synthetic forsterite, which is marketed as Tanzaniod has been synthesized in Russia for gem use. As you can easily imagine from its name, it is meant to imitate tanzanite. The RI, DR and SG of the Tanzaniod are consistent with those of natural forsterite, with Tanzaniod fluorescing a weak orange to yellow and greenish yellow under long and short wave ultraviolet lights respectively. Prominent pleochroism of blue and violet is also recognized. Under the hand-held spectroscope, absorption bands are seen on 490nm, 520nm and 580nm. Dot-like and short needle-like inclusions are observed under magnification. The compositional analysis by fluorescent X-ray detected considerable amount of Co and V, other than the main elements of Mg and Si.
Natural Hemimorphite And Natural Smithsonite
(via Gemmology Queensland, Vol.4,No.2, February 2003) Hiroshi Kitawaki writes:
We have increasingly encountered natural blue hemimorphite recently. Some of these seem to be easily confused with smithsonite, and this month we are comparing the gemological characteristics of these two stones.
Hemimorphite
The name Hemimorphite was derived from the form of the crystals of this mineral that shows distinct hemimorphism (in which both terminations show different forms). Its Japanese name is Ikyoku-Kou. The mineral is orthorhombic. It is not durable, as its hardness is low at about 4½ to 5 on Mohs scale. However, those hemimorphites with beautiful color, or pronounced transparency, are often cut for jewelry. Colorless, blue, yellow or brown are common, but cabochoned blue stones are more popular these days. The RI of hemimorphite is about 1.61-1.64 with DR 0.022. Its SG is 3.4 to 3.5, and it is inert to UV with no particular feature in the spectrum. Fibrous crystals of hemimorphite characteristically appear striped when examined magnification.
Smithsonite
Smithsonite was named after the mineralogist J Smithson who contributed financially to the establishment of the Smithsonian Institution in Washington, USA. The mineral is named Ryo-Aen-Icou in Japanese, which relates to its chemical composition. Smithsonite is a trigonal mineral, and it is isomorphous with calcite. Although the stone, like hemimorphite, possesses low hardness of 4 to 4½, pose a challenge to its durability. Smithsonites with beautiful colors such as blue, pink, green or yellow will be cabochoned or even faceted. The RI is around 1.62-1.84 and it has a large DR of 0.037. Its SG is 4.3 to 4.5.
When comparing the features of the minerals described above, a SG test will be the most useful way to distinguish them. When use of SG test is restricted due to the presence of setting, elemental analysis or infrared spectral analysis by FTIR will provide you with discriminatory information.
We have increasingly encountered natural blue hemimorphite recently. Some of these seem to be easily confused with smithsonite, and this month we are comparing the gemological characteristics of these two stones.
Hemimorphite
The name Hemimorphite was derived from the form of the crystals of this mineral that shows distinct hemimorphism (in which both terminations show different forms). Its Japanese name is Ikyoku-Kou. The mineral is orthorhombic. It is not durable, as its hardness is low at about 4½ to 5 on Mohs scale. However, those hemimorphites with beautiful color, or pronounced transparency, are often cut for jewelry. Colorless, blue, yellow or brown are common, but cabochoned blue stones are more popular these days. The RI of hemimorphite is about 1.61-1.64 with DR 0.022. Its SG is 3.4 to 3.5, and it is inert to UV with no particular feature in the spectrum. Fibrous crystals of hemimorphite characteristically appear striped when examined magnification.
Smithsonite
Smithsonite was named after the mineralogist J Smithson who contributed financially to the establishment of the Smithsonian Institution in Washington, USA. The mineral is named Ryo-Aen-Icou in Japanese, which relates to its chemical composition. Smithsonite is a trigonal mineral, and it is isomorphous with calcite. Although the stone, like hemimorphite, possesses low hardness of 4 to 4½, pose a challenge to its durability. Smithsonites with beautiful colors such as blue, pink, green or yellow will be cabochoned or even faceted. The RI is around 1.62-1.84 and it has a large DR of 0.037. Its SG is 4.3 to 4.5.
When comparing the features of the minerals described above, a SG test will be the most useful way to distinguish them. When use of SG test is restricted due to the presence of setting, elemental analysis or infrared spectral analysis by FTIR will provide you with discriminatory information.
Natural Hemimorphite And Natural Smithsonite
(via Gemmology Queensland, Vol.4,No.2, February 2003) Hiroshi Kitawaki writes:
We have increasingly encountered natural blue hemimorphite recently. Some of these seem to be easily confused with smithsonite, and this month we are comparing the gemological characteristics of these two stones.
Hemimorphite
The name Hemimorphite was derived from the form of the crystals of this mineral that shows distinct hemimorphism (in which both terminations show different forms). Its Japanese name is Ikyoku-Kou. The mineral is orthorhombic. It is not durable, as its hardness is low at about 4½ to 5 on Mohs scale. However, those hemimorphites with beautiful color, or pronounced transparency, are often cut for jewelry. Colorless, blue, yellow or brown are common, but cabochoned blue stones are more popular these days. The RI of hemimorphite is about 1.61-1.64 with DR 0.022. Its SG is 3.4 to 3.5, and it is inert to UV with no particular feature in the spectrum. Fibrous crystals of hemimorphite characteristically appear striped when examined magnification.
Smithsonite
Smithsonite was named after the mineralogist J Smithson who contributed financially to the establishment of the Smithsonian Institution in Washington, USA. The mineral is named Ryo-Aen-Icou in Japanese, which relates to its chemical composition. Smithsonite is a trigonal mineral, and it is isomorphous with calcite. Although the stone, like hemimorphite, possesses low hardness of 4 to 4½, pose a challenge to its durability. Smithsonites with beautiful colors such as blue, pink, green or yellow will be cabochoned or even faceted. The RI is around 1.62-1.84 and it has a large DR of 0.037. Its SG is 4.3 to 4.5.
When comparing the features of the minerals described above, a SG test will be the most useful way to distinguish them. When use of SG test is restricted due to the presence of setting, elemental analysis or infrared spectral analysis by FTIR will provide you with discriminatory information.
We have increasingly encountered natural blue hemimorphite recently. Some of these seem to be easily confused with smithsonite, and this month we are comparing the gemological characteristics of these two stones.
Hemimorphite
The name Hemimorphite was derived from the form of the crystals of this mineral that shows distinct hemimorphism (in which both terminations show different forms). Its Japanese name is Ikyoku-Kou. The mineral is orthorhombic. It is not durable, as its hardness is low at about 4½ to 5 on Mohs scale. However, those hemimorphites with beautiful color, or pronounced transparency, are often cut for jewelry. Colorless, blue, yellow or brown are common, but cabochoned blue stones are more popular these days. The RI of hemimorphite is about 1.61-1.64 with DR 0.022. Its SG is 3.4 to 3.5, and it is inert to UV with no particular feature in the spectrum. Fibrous crystals of hemimorphite characteristically appear striped when examined magnification.
Smithsonite
Smithsonite was named after the mineralogist J Smithson who contributed financially to the establishment of the Smithsonian Institution in Washington, USA. The mineral is named Ryo-Aen-Icou in Japanese, which relates to its chemical composition. Smithsonite is a trigonal mineral, and it is isomorphous with calcite. Although the stone, like hemimorphite, possesses low hardness of 4 to 4½, pose a challenge to its durability. Smithsonites with beautiful colors such as blue, pink, green or yellow will be cabochoned or even faceted. The RI is around 1.62-1.84 and it has a large DR of 0.037. Its SG is 4.3 to 4.5.
When comparing the features of the minerals described above, a SG test will be the most useful way to distinguish them. When use of SG test is restricted due to the presence of setting, elemental analysis or infrared spectral analysis by FTIR will provide you with discriminatory information.
Fortall™
Jewellery News Asia writes:
This is a new emerald green man-made material that is being marketed through Rough Synthetic Stones Co Ltd (RSS) of Bangkok.
This crystal pulled material has:
- An emerald green color…although the crystals are also available in black, blue, brown, and red colors
- A hardness of 7 on Mohs scale
- A specific gravity of 2.70
- A refractive index (presumably SR) of 1.72
Before being marketed as a jewelry accessory, this material has been used for industrial purposes. Fortall™ is available both as rough and as faceted stones.
This is a new emerald green man-made material that is being marketed through Rough Synthetic Stones Co Ltd (RSS) of Bangkok.
This crystal pulled material has:
- An emerald green color…although the crystals are also available in black, blue, brown, and red colors
- A hardness of 7 on Mohs scale
- A specific gravity of 2.70
- A refractive index (presumably SR) of 1.72
Before being marketed as a jewelry accessory, this material has been used for industrial purposes. Fortall™ is available both as rough and as faceted stones.
Created Turquoise & Coral
Sanwa Pearl Trading are marketing look-alike imitation of turquoise and coral that are being produced in Germany ‘under high pressure and temperature by a special bonding agent and contain no epoxy resin.’
Branded Cubic Zirconia
Machine cut faceted CZ that displays the ‘hearts & arrows’ effect is being marketed as Hsini Star™ cubic zirconia.
Be on the look out for:
- CZ that displays an alexandrite effect when viewed in different light sources.
- Brown CZ that imitates brown diamond.
- Black CZ that does not change color when submitted to high temperature.
Be on the look out for:
- CZ that displays an alexandrite effect when viewed in different light sources.
- Brown CZ that imitates brown diamond.
- Black CZ that does not change color when submitted to high temperature.
Monday, April 16, 2007
Pyrite vs Marcasite
(via Gemmology Queensland, Vol.4, No.7, July 2003)
The marcasites of jewelry are a misnomer, for the brassy colored flattened pyramids and rose cuts, that were hand set or cemented into mid-18th century and Victorian jewelry, were manufactured from pyrite…not marcasite. Marcasite’s lack of chemical stability makes this mineral useless for jewelry purposes.
The word pyrite is derived from the Greek root pyros = fire, thus alluding to the sparks generated when this mineral is struck by steel. The origin of the word marcasite is less certain but is likely derived from the Latin word marcasita.
Although, chemically pyrite and marcasite are dimorphs of the mineral iron sulphide (FeS), their properties are quite different.
Pyrite
Crystal system: cubic
Habit: interpenetrant cubes; modified pyritohedra
Color: brassy yellow
Hardness: 6-6½
Fracture: conchoidal; uneven
Specific gravity: 5
Luster: metallic
Diaphaneity: opaque
Streak: greenish black
Identifying features: brassy with greenish black streak
Marcasite
Crystal system: orthorhombic
Habit: spear-shaped twins; cocks-comb aggregates
Color: brassy yellow
Hardness: 6-6½
Fracture: uneven
Specific gravity: 4.8-4.9
Luster: metallic
Diaphaneity: opaque
Streak: grayish brownish black
Identifying features: evidence of surface degredation (powdering)
Presently marcasite (pyrite) set jewelry is rapidly coming back into vogue as inexpensive surface decoration for jewelry and watches. Most of the newer marcasites are being manufactured in China, and are glued into silver or silver plated copper settings; their cutting and polishing into pointed square shapes must be accurate.
A Tip
When checking marcasite-set jewelry for quality, ensure:
- each marcasite is of uniform size and thickness.
- polished surfaces are free of surface pits.
- the marcasites display a uniform brassy metallic luster in reflected light.
The marcasites of jewelry are a misnomer, for the brassy colored flattened pyramids and rose cuts, that were hand set or cemented into mid-18th century and Victorian jewelry, were manufactured from pyrite…not marcasite. Marcasite’s lack of chemical stability makes this mineral useless for jewelry purposes.
The word pyrite is derived from the Greek root pyros = fire, thus alluding to the sparks generated when this mineral is struck by steel. The origin of the word marcasite is less certain but is likely derived from the Latin word marcasita.
Although, chemically pyrite and marcasite are dimorphs of the mineral iron sulphide (FeS), their properties are quite different.
Pyrite
Crystal system: cubic
Habit: interpenetrant cubes; modified pyritohedra
Color: brassy yellow
Hardness: 6-6½
Fracture: conchoidal; uneven
Specific gravity: 5
Luster: metallic
Diaphaneity: opaque
Streak: greenish black
Identifying features: brassy with greenish black streak
Marcasite
Crystal system: orthorhombic
Habit: spear-shaped twins; cocks-comb aggregates
Color: brassy yellow
Hardness: 6-6½
Fracture: uneven
Specific gravity: 4.8-4.9
Luster: metallic
Diaphaneity: opaque
Streak: grayish brownish black
Identifying features: evidence of surface degredation (powdering)
Presently marcasite (pyrite) set jewelry is rapidly coming back into vogue as inexpensive surface decoration for jewelry and watches. Most of the newer marcasites are being manufactured in China, and are glued into silver or silver plated copper settings; their cutting and polishing into pointed square shapes must be accurate.
A Tip
When checking marcasite-set jewelry for quality, ensure:
- each marcasite is of uniform size and thickness.
- polished surfaces are free of surface pits.
- the marcasites display a uniform brassy metallic luster in reflected light.
Another Use For Lapis Lazuli
(via Gemmology Queensland, Vol.4, No.9, September 200 / From the Precious Lapis Lazuli gemstone)
Lapis lazuli pigment was once only attainable in small quantities. Recent advancements in refining technology has made it possible to produce a pure natural lapis pigment (ultramarine blue) of consistent high quality in commercial quantities.
The pigment originates from the Chilean lapis lazuli deposit owned by Las Flores de los andes S.A and located high in the Chilean Andes in the province of Coquimbo. It is produced in Chile by Lapis Pigments S.A with technical advice from European scientists.
The pure royal blue pigment, also known as natural ultramarine blue, is extracted from the gemstone. Lapis lazuli has a history of more than five thousand years as jewelry, ornamental art and as a pigment. The great masters of the Renaissance period immortalized the blue ultramarine pigment in their famous works. The value of the pigment then exceeded the price of gold.
The natural lapis lazuli pigment differentiates itself from this synthetic counterpart by the vibrancy of the blue that it produces. The natural pigment particles, large in size, have an irregular and angular shape. With their multiple surfaces this natural pigment reacts to light like a finely faceted diamond, thereby producing an ever-changing display of rich vibrant blues. This creates a three-dimensional, gem-like effect that is not attainable with the very small, round and uniformly shaped particles of the synthetic ultramarine blue pigment.
The natural lapis lazuli is suitable for use in paints, lacquers, inks and cosmetics. It is successfully being used in the coating of metallic and other surfaces.
Lapis lazuli pigment was once only attainable in small quantities. Recent advancements in refining technology has made it possible to produce a pure natural lapis pigment (ultramarine blue) of consistent high quality in commercial quantities.
The pigment originates from the Chilean lapis lazuli deposit owned by Las Flores de los andes S.A and located high in the Chilean Andes in the province of Coquimbo. It is produced in Chile by Lapis Pigments S.A with technical advice from European scientists.
The pure royal blue pigment, also known as natural ultramarine blue, is extracted from the gemstone. Lapis lazuli has a history of more than five thousand years as jewelry, ornamental art and as a pigment. The great masters of the Renaissance period immortalized the blue ultramarine pigment in their famous works. The value of the pigment then exceeded the price of gold.
The natural lapis lazuli pigment differentiates itself from this synthetic counterpart by the vibrancy of the blue that it produces. The natural pigment particles, large in size, have an irregular and angular shape. With their multiple surfaces this natural pigment reacts to light like a finely faceted diamond, thereby producing an ever-changing display of rich vibrant blues. This creates a three-dimensional, gem-like effect that is not attainable with the very small, round and uniformly shaped particles of the synthetic ultramarine blue pigment.
The natural lapis lazuli is suitable for use in paints, lacquers, inks and cosmetics. It is successfully being used in the coating of metallic and other surfaces.
Colored Gemstone Grading…..Friend or Foe?
(via Rapaport Diamond Report, Vol.30, No.9, March 2, 2007) Antoinette Matlins writes:
“If you walk around the AGTA show, you do not see many AGTA grading reports. Who is getting these reports? It is not the dealers, but often the consumers. They invest in the stones and send them to grading labs to verify what the dealers have told them. The colored gemstone dealers in this industry are not educated. They often represent material as natural and not heated when, in fact, the goods are heated. Dealers don’t understand the science of gemology but simply tell their clients whatever they have been told. The dealers know they have been making money this way, so why change? The trade in general has not accepted its responsibilities to the final client and most do not provide proper documentation. I have offered to provide gemological services and educational seminars free of charge to AGTA members. They never call me.”
“If you walk around the AGTA show, you do not see many AGTA grading reports. Who is getting these reports? It is not the dealers, but often the consumers. They invest in the stones and send them to grading labs to verify what the dealers have told them. The colored gemstone dealers in this industry are not educated. They often represent material as natural and not heated when, in fact, the goods are heated. Dealers don’t understand the science of gemology but simply tell their clients whatever they have been told. The dealers know they have been making money this way, so why change? The trade in general has not accepted its responsibilities to the final client and most do not provide proper documentation. I have offered to provide gemological services and educational seminars free of charge to AGTA members. They never call me.”
NDT Solution
Non-destructive Testing for Identifying Natural, Synthetic, Treated, and Imitation Gem Materials
(via Gemmology Queensland, Volume 4, No.9, September 2003) Taijin Lu and James E Shigley writes:
In the daily business of NDT, it is easy to lose sight of the wide range of applications for NDT techniques. In this month’s featured article, the authors have outlined the application of NDT techniques in evaluating natural and synthetic gems. It is always interesting to see in what new ways NDT is used, and how it helps diverse industries or endeavors—G.P.Singh, Associate Technical Editor, The American Society For NonDestructive Testing.
Introduction
Accurate identification is essential to maintain the commercial value of gemstones. It is also required to enable jewelers to disclose to their customers the correct identity of the gemstones they sell. In identifying and studying fashioned gemstones, any testing must be performed nondestructively without altering the gemstones shape or appearance. When presented for testing, some gemstones are mounted in jewelry, which can further complicate the testing procedure. By using standard gem testing instruments and techniques, trained gemologists can recognize most gem materials. In some instances, however, they may not be able to distinguish certain synthetic and laboratory treated gem materials, which can have almost the same visual appearance and gemological properties as their natural counterparts. Use of advanced nondestructive imaging, spectroscopic, and chemical analysis techniques helps establish criteria to distinguish gem materials. Several examples are presented of nondestructive testing techniques currently used in gemology.
Gems include a wide range of materials (natural, synthetic, treated, and imitation diamonds, colored stones, and pearls). This requires gathering observations and measurements to determine distinctive characteristics of gem materials. Such characteristics are summarized in standard reference books (Webster, 1994; Liddicoat, 1981).
With the continued development of crystal growth technology, various synthetic and imitation gem materials are increasingly encountered in the jewelry industry (Nassau, 1980; Nassau, 1983, Gubelin and Koivula, 1986; Nassau et al., 1997). For example, synthetic cubic zirconia, and synthetic moissanite (SiC-6H) have a very similar appearance to diamonds, and are used as imitation diamonds. Some of these synthetic materials, such as synthetic ruby, sapphire and emerald, can be grown by several growth techniques (hydrothermal, flux, melt).
Various processes (such as irradiation, heating, filling of open fractures or cavities, and coating) are also used to treat low quality gem materials to improve their color, appearance, or durability (Moses et al., 1999; Johnson et al., 1999; McClure et al., 1999, Reinitz et al., 2000, Nassau, 1983). Typical examples of heat treated gemstones include sapphire (corundum) and citrine (quartz). Irradiation with gamma rays, X-rays, electrons, or neutrons is used to alter the color of specimens of diamond, topaz, and quartz. Both diamonds and emeralds can have surface reaching openings filled with various substances to improve their clarity.
Since synthetic and treated gem materials are regularly seen today in the jewelry market, it is important for gemologists to be able to identify them. Although effective in many cases, traditional gem testing instruments and methods cannot always distinguish synthetic and laboratory treated gem materials from their natural counterparts. Advanced nondestructive characterization techniques enable the gemologist to find diagnostic properties to distinguish these materials. The goal of the gem research program at the Gemological Institute of America is to find relatively practical methods and/or instruments to identify gemstones based on the differences revealed by both standard and advanced nondestructive characterization. Systematic documentation of the gemological properties of various gem materials of known origin, carried out by similar research institutions and others, is also necessary to develop gem identification criteria.
In this article, characterization methods commonly used today in gemology are briefly reviewed, and examples of several methods to identify gem materials are discussed.
Nondestructive methods of gem identification
A number of instruments have been developed over the years to assist the jeweler and gemologist in the identification of gem materials. These instruments are mainly used for evaluating the appearance of gemstones. Visual characteristics such a color, luster, growth features, and inclusions are examined with a 10x magnifier (loupe) and a binocular microscope with bright and dark field illumination and polarizing functions. Refractive index and birefringence (double refraction) are determined by a refractometer. Pleochroism (dichroism) is examined with a dichroscope. Strains and optical character are observed using a polariscope. Visible absorption spectrum is examined with a hand spectroscope. Specific gravity, electric conductivity, and thermal conductivity are measured by a hydrostatic balance, conductivity meter, and thermal conductivity tester respectively. Trained gemologists are familiar with this equipment (Webster, 1994; Liddicoat, 1981).
Advanced methods
The physical and compositional differences between natural, synthetic, and treated gem materials can range from significant to minor. Thus, it is necessary to check for potentially small differences through advanced analytical methods which have sufficiently high resolution and sensitivity. To achieve better resolution and sensitivity, minor modifications had to be made to some of these instruments. These include the design of special sample holders for faceted and/or mounted gem samples, and optimizing the illumination conditions by use of, for example, an optical fiber system for microscopy and spectroscopy. Special accessories such as liquid nitrogen cryogenic unit are also used to record visible absorption spectra of diamonds at low temperature.
Use of the techniques, together with published information, allows the systematic gathering of a database of information on the gem materials to support the developments of practical gem identification criteria.
Application
In the past, a number of low cost natural minerals and man made materials have been used as imitations of colorless diamond. Since these materials differ compositionally from diamond, they have significant differences in one or more of their physical properties, which allow them to be distinguished. The most widespread diamond imitation material today is cubic zirconia (cubic zirconium oxide). Because diamond’s thermal conductivity is superior to that of imitations, jewelers can quickly distinguish diamonds from cubic zirconia and other previously used imitation materials (synthetic corundum, synthetic spinel, zircon, synthetic rutile, strontium titanate, yttrium aluminum garnet, and gadolium gallium garnet) by use of a simple thermal conductivity meter.
Within the past two years, anew near colorless diamond imitation, synthetic moissanite (SiC-6H), has been marketed for jewelry purposes. The thermal conductivity of synthetic moissanite is quite close to that of diamond, so much so that is can be mistakenly identified as diamond using a conventional thermal probe. However, it is optically anisotropic, which causes the junctions between adjacent polished facets to appear doubled when looking through a fashioned piece with a 10x magnifier or a binocular microscope. The refractive appearance of natural diamonds, on the other hand, always includes clearly single junctions between facets. Synthetic moissanite also exhibits electrical conductivity, and has quite different visible, infrared, and Raman spectra from that of diamonds (Nassau, 1983).
Some natural diamonds possess open, surface reaching cleavages which reflect light, and thus make a fashioned diamond look less attractive. During the past decade, a process has been developed to inject a high refractive index, glass-like material into these cleavages to lessen their visibility. Diamond treated in this way can be recognized by the distinctive visual appearance of the filled cracks that can be seen with 10x magnification. Confirmation of this conclusion can be obtained by X-ray radiography, where the photographic image reveals the filled crack. Chemical analysis can detect the presence of high atomic weight elements such as lead or bismuth, which are components of the glass-like filler material used to increase the refractive index (Koivula et al, 1989; Kammerling et al, 1994).
Coloration can be produced in diamond by exposing them to a source of radiation. This coloration can be modified by subsequent heat treatment. In some cases, irradiation treatment gives rise to unusual color zoning or ultraviolet fluorescence, which can help the gemologist identify a color treated diamond. However, distinguishing colored diamonds irradiated in the laboratory (versus the very rare green to blue diamonds irradiated in nature) normally requires recording visible absorption spectra (with the diamond cooled to low temperatures with cryogenic unit), as well as infrared spectra. In some cases, the distinction cannot be made between the exposure of a diamond to a source of radiation in nature or the laboratory. Recently, several companies have begun using high pressure and high temperature processes to treat the color and other characteristics of a select group of natural diamonds. Conclusive identification of these treated color diamonds requires infrared and low temperature visible spectroscopy as well as Raman spectroscopy, but a number of gemological properties provide some indication of HPHT treatment (Moses et al., 1999; Fisher and Spits, 2000); Reinitz et al, 2000).
Synthetic diamond can be grown from a molten metal alloy at high temperatures and pressures by the temperature gradient. The resulting crystals exhibit a cuboctahedral shape (Sunagawa, 1995). Distinctive color zoning, growth features, and metallic inclusions in polished synthetic diamonds can all be observed with a binocular microscope (Shigley et al., 1995). An ultraviolet fluorescence imaging system, known as the DiamondView and developed by De Beers researchers, allows the observation of the fluorescence zoning pattern that is characteristic of synthetic diamonds (Welbourn, 1996). Chemical analysis can reveal the presence of the transition metals (such as iron, nickel, and cobalt) from which the synthetic diamonds grew.
Natural pearls are relatively rare, but are still encountered in jewelry pieces. Most pearls sold today are cultured pearls. They are produced by introducing a mother-of-pearl bead and piece of mantle tissue into the oyster. The oyster is then cultivated under controlled conditions for periods of up to one year or more during which the bead is covered by nacre. In contrast, pearl imitations are usually wax-filled glass, solid glass, plastic, and mother-of-pearl (Liddicoat, 1981; Webster, 1994).
X-radiography is the best method to identify pearls. X-ray absorption images of pearls are recorded on photographic film to reveal the differing internal structures (Liddicoat, 1981; Matlins, 1995; Scarratt et al., 2000). On a radiograph, natural pearls usually show concentric rings outward from the center. Cultured pearls show a clear interface between nacre layer and the bead nucleus, while pearl imitations lack internal structure.
Cultured pearls can be colored by chemical treatments or irradiation. They may also possess a surface coating. Such treatments can often be detected by careful examination with a binocular microscope; chemical analysis may also reveal the presence of a foreign material.
Jade is a polycrystalline gem material consisting of a mixture of silicate minerals. There are two types of jade, one consisting mainly of jadeite (a pyroxene), and the other of nephrite (an amphibole). There are also other green-colored rocks that have been sold as jade, as well as imitations. Since there are a large number of grain boundaries and/or fractures in jade, several treatment processes are used to improve appearance. The most commonly used processes involve chemical bleaching of the original jade to remove brownish stains, and then impregnating it with polymers or other substances to fill surface reaching fractures (Fritsch et al., 1992; Ou Yang, 1997). In some cases, colored dyes are also used to improve the color.
A number of identification criteria for treated jade have been found, such as the peculiarities evident under magnified observation, lower specific gravity, and distinctive infrared spectra. When observed under magnification, it is often possible to see differences in texture or structure that are evidence of treatment. Since the specific gravity of untreated jade is around 3.3 to 3.5, polymer impregnated samples will float in a 3.2 specific gravity liquid because of their lighter specific gravity, whereas untreated jade will sink. Infrared absorption spectra show clear differences between natural and treated jadeite.
Ruby (corundum) is not only one of the best known colored gemstones, but it is also an important optical crystal for industrial uses. It can be synthesized by many methods, such as from a melt by the Czochralski technique, from a flux solution, and recently from a hydrothermal solution (Lu and Shigley, 1998). Synthetic ruby can often be distinguished gemologically by the observation of inclusions, color zoning, and growth features (Liddicoat, 1981; Hughes, 1997, Lu and Shigley, 1998).
When such visual characteristics are not present or cannot be seen, natural and synthetic rubies can be identified on the basis of their trace element chemistry as determined by the energy dispersive X-ray fluorescence method (Muhlmeister et al.,1998). Trace elements such as nickel, molybdenum, lanthanum, tungsten, platinum, lead, or bismuth may be detected in synthetic ruby, as a result of growth in a laboratory environment. The relative proportions of the transition metals chromium, iron, vanadium, and titanium also varies between natural and synthetic rubies, and can be used to distinguish between them.
Amethyst (quartz) is the most important gem variety of quartz, and is found in many localities worldwide. Its synthetic counterpart, grown from either alkaline or fluoride solutions, is produced in Russia, Japan, China, and other countries. The appearance and physical properties of both are very similar.
Based on our study of both natural and synthetic amethyst, we have found that there are characteristic differences in crystal morphology, twinning, inclusions, growth zoning, color banding, infrared spectra, and trace element chemistry. As noted by Lu and Sunagawa (1990), natural amethyst is usually twinned, it exhibits tiny solid inclusions, and it lacks a characteristic infrared absorption band at 2.8mm (1x10¯4 in). Synthetic amethyst grown from fluoride solution displays an unusual growth structure (a stream-like structure), color bands that parallel the seed crystal, distinct infrared spectra, and fluorine and lithium as trace elements. The synthetic amethyst grown from alkaline solution is characterized by growth sectors, color zoning, and distinct infrared spectra.
Emerald (beryl) is the final example of gem identification to be discussed here. Synthetic emerald can be grown from flux and hydrothermal solutions, and it exhibits a number of gemological properties (like synthetic ruby) by which it can be identified.
Many natural emerald crystals often contain surface reaching fractures, due to their growth conditions or perhaps to damage suffered during mining. The presence of these fractures results in an unattractive appearance. Increasingly over the past two decades, a variety of liquid substances (oils, epoxies, resins, etc.) have been used to fill these open fractures, and thus to improve emerald appearance (Kammerling et al, 1991; Johnson et al., 1999). Questions concerning the long term stability of these substances have led to the need not only to determine if an emerald has been treated in this way, but to determine the identity of the filler substance as well. The use of both infrared and Raman spectroscopies has provided new information on the detection of treated emeralds (Johnson et al., 1999).
Discussion and summary
Gem materials consist of a wide range of materials. Most of them are single crystals, usually faceted and polished (and sometimes mounted in jewelry). To support the commercial value of gemstones and the stability of the jewelry market, accurate gem identification is important. The traditional and advanced nondestructive characterization techniques used today for gem identification are based on the distinctive gemological properties of natural, synthetic, treated and imitation gem materials.
Traditional gemological methods and instruments are inexpensive and relatively easy to use. When used by a trained gemologist, they can help to identify most gem materials. In some cases, advanced analytical techniques with higher resolution and sensitivity are required to reveal the small differences in properties among natural, synthetic, and treated gem materials. Advanced techniques can also help identify the geological environment and growth conditions in which a gem material formed. They can also occasionally provide evidence on the geographic origin, which is important for high value natural colored stones such as ruby or sapphire. Although a combination of both the traditional and advanced methods helps to determine the diagnostic properties of gem materials, the development of new, relatively simple and inexpensive testing instruments for use by jewelers remains a challenge. The continued production of new synthetic and treated gem materials requires an equal effort to support practical gem identification to safeguard the jewelry industry.
(via Gemmology Queensland, Volume 4, No.9, September 2003) Taijin Lu and James E Shigley writes:
In the daily business of NDT, it is easy to lose sight of the wide range of applications for NDT techniques. In this month’s featured article, the authors have outlined the application of NDT techniques in evaluating natural and synthetic gems. It is always interesting to see in what new ways NDT is used, and how it helps diverse industries or endeavors—G.P.Singh, Associate Technical Editor, The American Society For NonDestructive Testing.
Introduction
Accurate identification is essential to maintain the commercial value of gemstones. It is also required to enable jewelers to disclose to their customers the correct identity of the gemstones they sell. In identifying and studying fashioned gemstones, any testing must be performed nondestructively without altering the gemstones shape or appearance. When presented for testing, some gemstones are mounted in jewelry, which can further complicate the testing procedure. By using standard gem testing instruments and techniques, trained gemologists can recognize most gem materials. In some instances, however, they may not be able to distinguish certain synthetic and laboratory treated gem materials, which can have almost the same visual appearance and gemological properties as their natural counterparts. Use of advanced nondestructive imaging, spectroscopic, and chemical analysis techniques helps establish criteria to distinguish gem materials. Several examples are presented of nondestructive testing techniques currently used in gemology.
Gems include a wide range of materials (natural, synthetic, treated, and imitation diamonds, colored stones, and pearls). This requires gathering observations and measurements to determine distinctive characteristics of gem materials. Such characteristics are summarized in standard reference books (Webster, 1994; Liddicoat, 1981).
With the continued development of crystal growth technology, various synthetic and imitation gem materials are increasingly encountered in the jewelry industry (Nassau, 1980; Nassau, 1983, Gubelin and Koivula, 1986; Nassau et al., 1997). For example, synthetic cubic zirconia, and synthetic moissanite (SiC-6H) have a very similar appearance to diamonds, and are used as imitation diamonds. Some of these synthetic materials, such as synthetic ruby, sapphire and emerald, can be grown by several growth techniques (hydrothermal, flux, melt).
Various processes (such as irradiation, heating, filling of open fractures or cavities, and coating) are also used to treat low quality gem materials to improve their color, appearance, or durability (Moses et al., 1999; Johnson et al., 1999; McClure et al., 1999, Reinitz et al., 2000, Nassau, 1983). Typical examples of heat treated gemstones include sapphire (corundum) and citrine (quartz). Irradiation with gamma rays, X-rays, electrons, or neutrons is used to alter the color of specimens of diamond, topaz, and quartz. Both diamonds and emeralds can have surface reaching openings filled with various substances to improve their clarity.
Since synthetic and treated gem materials are regularly seen today in the jewelry market, it is important for gemologists to be able to identify them. Although effective in many cases, traditional gem testing instruments and methods cannot always distinguish synthetic and laboratory treated gem materials from their natural counterparts. Advanced nondestructive characterization techniques enable the gemologist to find diagnostic properties to distinguish these materials. The goal of the gem research program at the Gemological Institute of America is to find relatively practical methods and/or instruments to identify gemstones based on the differences revealed by both standard and advanced nondestructive characterization. Systematic documentation of the gemological properties of various gem materials of known origin, carried out by similar research institutions and others, is also necessary to develop gem identification criteria.
In this article, characterization methods commonly used today in gemology are briefly reviewed, and examples of several methods to identify gem materials are discussed.
Nondestructive methods of gem identification
A number of instruments have been developed over the years to assist the jeweler and gemologist in the identification of gem materials. These instruments are mainly used for evaluating the appearance of gemstones. Visual characteristics such a color, luster, growth features, and inclusions are examined with a 10x magnifier (loupe) and a binocular microscope with bright and dark field illumination and polarizing functions. Refractive index and birefringence (double refraction) are determined by a refractometer. Pleochroism (dichroism) is examined with a dichroscope. Strains and optical character are observed using a polariscope. Visible absorption spectrum is examined with a hand spectroscope. Specific gravity, electric conductivity, and thermal conductivity are measured by a hydrostatic balance, conductivity meter, and thermal conductivity tester respectively. Trained gemologists are familiar with this equipment (Webster, 1994; Liddicoat, 1981).
Advanced methods
The physical and compositional differences between natural, synthetic, and treated gem materials can range from significant to minor. Thus, it is necessary to check for potentially small differences through advanced analytical methods which have sufficiently high resolution and sensitivity. To achieve better resolution and sensitivity, minor modifications had to be made to some of these instruments. These include the design of special sample holders for faceted and/or mounted gem samples, and optimizing the illumination conditions by use of, for example, an optical fiber system for microscopy and spectroscopy. Special accessories such as liquid nitrogen cryogenic unit are also used to record visible absorption spectra of diamonds at low temperature.
Use of the techniques, together with published information, allows the systematic gathering of a database of information on the gem materials to support the developments of practical gem identification criteria.
Application
In the past, a number of low cost natural minerals and man made materials have been used as imitations of colorless diamond. Since these materials differ compositionally from diamond, they have significant differences in one or more of their physical properties, which allow them to be distinguished. The most widespread diamond imitation material today is cubic zirconia (cubic zirconium oxide). Because diamond’s thermal conductivity is superior to that of imitations, jewelers can quickly distinguish diamonds from cubic zirconia and other previously used imitation materials (synthetic corundum, synthetic spinel, zircon, synthetic rutile, strontium titanate, yttrium aluminum garnet, and gadolium gallium garnet) by use of a simple thermal conductivity meter.
Within the past two years, anew near colorless diamond imitation, synthetic moissanite (SiC-6H), has been marketed for jewelry purposes. The thermal conductivity of synthetic moissanite is quite close to that of diamond, so much so that is can be mistakenly identified as diamond using a conventional thermal probe. However, it is optically anisotropic, which causes the junctions between adjacent polished facets to appear doubled when looking through a fashioned piece with a 10x magnifier or a binocular microscope. The refractive appearance of natural diamonds, on the other hand, always includes clearly single junctions between facets. Synthetic moissanite also exhibits electrical conductivity, and has quite different visible, infrared, and Raman spectra from that of diamonds (Nassau, 1983).
Some natural diamonds possess open, surface reaching cleavages which reflect light, and thus make a fashioned diamond look less attractive. During the past decade, a process has been developed to inject a high refractive index, glass-like material into these cleavages to lessen their visibility. Diamond treated in this way can be recognized by the distinctive visual appearance of the filled cracks that can be seen with 10x magnification. Confirmation of this conclusion can be obtained by X-ray radiography, where the photographic image reveals the filled crack. Chemical analysis can detect the presence of high atomic weight elements such as lead or bismuth, which are components of the glass-like filler material used to increase the refractive index (Koivula et al, 1989; Kammerling et al, 1994).
Coloration can be produced in diamond by exposing them to a source of radiation. This coloration can be modified by subsequent heat treatment. In some cases, irradiation treatment gives rise to unusual color zoning or ultraviolet fluorescence, which can help the gemologist identify a color treated diamond. However, distinguishing colored diamonds irradiated in the laboratory (versus the very rare green to blue diamonds irradiated in nature) normally requires recording visible absorption spectra (with the diamond cooled to low temperatures with cryogenic unit), as well as infrared spectra. In some cases, the distinction cannot be made between the exposure of a diamond to a source of radiation in nature or the laboratory. Recently, several companies have begun using high pressure and high temperature processes to treat the color and other characteristics of a select group of natural diamonds. Conclusive identification of these treated color diamonds requires infrared and low temperature visible spectroscopy as well as Raman spectroscopy, but a number of gemological properties provide some indication of HPHT treatment (Moses et al., 1999; Fisher and Spits, 2000); Reinitz et al, 2000).
Synthetic diamond can be grown from a molten metal alloy at high temperatures and pressures by the temperature gradient. The resulting crystals exhibit a cuboctahedral shape (Sunagawa, 1995). Distinctive color zoning, growth features, and metallic inclusions in polished synthetic diamonds can all be observed with a binocular microscope (Shigley et al., 1995). An ultraviolet fluorescence imaging system, known as the DiamondView and developed by De Beers researchers, allows the observation of the fluorescence zoning pattern that is characteristic of synthetic diamonds (Welbourn, 1996). Chemical analysis can reveal the presence of the transition metals (such as iron, nickel, and cobalt) from which the synthetic diamonds grew.
Natural pearls are relatively rare, but are still encountered in jewelry pieces. Most pearls sold today are cultured pearls. They are produced by introducing a mother-of-pearl bead and piece of mantle tissue into the oyster. The oyster is then cultivated under controlled conditions for periods of up to one year or more during which the bead is covered by nacre. In contrast, pearl imitations are usually wax-filled glass, solid glass, plastic, and mother-of-pearl (Liddicoat, 1981; Webster, 1994).
X-radiography is the best method to identify pearls. X-ray absorption images of pearls are recorded on photographic film to reveal the differing internal structures (Liddicoat, 1981; Matlins, 1995; Scarratt et al., 2000). On a radiograph, natural pearls usually show concentric rings outward from the center. Cultured pearls show a clear interface between nacre layer and the bead nucleus, while pearl imitations lack internal structure.
Cultured pearls can be colored by chemical treatments or irradiation. They may also possess a surface coating. Such treatments can often be detected by careful examination with a binocular microscope; chemical analysis may also reveal the presence of a foreign material.
Jade is a polycrystalline gem material consisting of a mixture of silicate minerals. There are two types of jade, one consisting mainly of jadeite (a pyroxene), and the other of nephrite (an amphibole). There are also other green-colored rocks that have been sold as jade, as well as imitations. Since there are a large number of grain boundaries and/or fractures in jade, several treatment processes are used to improve appearance. The most commonly used processes involve chemical bleaching of the original jade to remove brownish stains, and then impregnating it with polymers or other substances to fill surface reaching fractures (Fritsch et al., 1992; Ou Yang, 1997). In some cases, colored dyes are also used to improve the color.
A number of identification criteria for treated jade have been found, such as the peculiarities evident under magnified observation, lower specific gravity, and distinctive infrared spectra. When observed under magnification, it is often possible to see differences in texture or structure that are evidence of treatment. Since the specific gravity of untreated jade is around 3.3 to 3.5, polymer impregnated samples will float in a 3.2 specific gravity liquid because of their lighter specific gravity, whereas untreated jade will sink. Infrared absorption spectra show clear differences between natural and treated jadeite.
Ruby (corundum) is not only one of the best known colored gemstones, but it is also an important optical crystal for industrial uses. It can be synthesized by many methods, such as from a melt by the Czochralski technique, from a flux solution, and recently from a hydrothermal solution (Lu and Shigley, 1998). Synthetic ruby can often be distinguished gemologically by the observation of inclusions, color zoning, and growth features (Liddicoat, 1981; Hughes, 1997, Lu and Shigley, 1998).
When such visual characteristics are not present or cannot be seen, natural and synthetic rubies can be identified on the basis of their trace element chemistry as determined by the energy dispersive X-ray fluorescence method (Muhlmeister et al.,1998). Trace elements such as nickel, molybdenum, lanthanum, tungsten, platinum, lead, or bismuth may be detected in synthetic ruby, as a result of growth in a laboratory environment. The relative proportions of the transition metals chromium, iron, vanadium, and titanium also varies between natural and synthetic rubies, and can be used to distinguish between them.
Amethyst (quartz) is the most important gem variety of quartz, and is found in many localities worldwide. Its synthetic counterpart, grown from either alkaline or fluoride solutions, is produced in Russia, Japan, China, and other countries. The appearance and physical properties of both are very similar.
Based on our study of both natural and synthetic amethyst, we have found that there are characteristic differences in crystal morphology, twinning, inclusions, growth zoning, color banding, infrared spectra, and trace element chemistry. As noted by Lu and Sunagawa (1990), natural amethyst is usually twinned, it exhibits tiny solid inclusions, and it lacks a characteristic infrared absorption band at 2.8mm (1x10¯4 in). Synthetic amethyst grown from fluoride solution displays an unusual growth structure (a stream-like structure), color bands that parallel the seed crystal, distinct infrared spectra, and fluorine and lithium as trace elements. The synthetic amethyst grown from alkaline solution is characterized by growth sectors, color zoning, and distinct infrared spectra.
Emerald (beryl) is the final example of gem identification to be discussed here. Synthetic emerald can be grown from flux and hydrothermal solutions, and it exhibits a number of gemological properties (like synthetic ruby) by which it can be identified.
Many natural emerald crystals often contain surface reaching fractures, due to their growth conditions or perhaps to damage suffered during mining. The presence of these fractures results in an unattractive appearance. Increasingly over the past two decades, a variety of liquid substances (oils, epoxies, resins, etc.) have been used to fill these open fractures, and thus to improve emerald appearance (Kammerling et al, 1991; Johnson et al., 1999). Questions concerning the long term stability of these substances have led to the need not only to determine if an emerald has been treated in this way, but to determine the identity of the filler substance as well. The use of both infrared and Raman spectroscopies has provided new information on the detection of treated emeralds (Johnson et al., 1999).
Discussion and summary
Gem materials consist of a wide range of materials. Most of them are single crystals, usually faceted and polished (and sometimes mounted in jewelry). To support the commercial value of gemstones and the stability of the jewelry market, accurate gem identification is important. The traditional and advanced nondestructive characterization techniques used today for gem identification are based on the distinctive gemological properties of natural, synthetic, treated and imitation gem materials.
Traditional gemological methods and instruments are inexpensive and relatively easy to use. When used by a trained gemologist, they can help to identify most gem materials. In some cases, advanced analytical techniques with higher resolution and sensitivity are required to reveal the small differences in properties among natural, synthetic, and treated gem materials. Advanced techniques can also help identify the geological environment and growth conditions in which a gem material formed. They can also occasionally provide evidence on the geographic origin, which is important for high value natural colored stones such as ruby or sapphire. Although a combination of both the traditional and advanced methods helps to determine the diagnostic properties of gem materials, the development of new, relatively simple and inexpensive testing instruments for use by jewelers remains a challenge. The continued production of new synthetic and treated gem materials requires an equal effort to support practical gem identification to safeguard the jewelry industry.
Saturday, April 14, 2007
Innovative Color Enhancement
(via Gem Scoup) Simon Bruce Lockhart writes:
Like any county, and particularly like those who population sometimes sees a disproportionate amount of disadvantaged civilians, Sri Lanka enjoys its fair share of friendly, open, and utterly charming confidence tricksters. Innovative local ‘color enhancement techniques’ are employed on yellow and blue sapphires to obtain high prices. The wily rascals of Elahera roll rough sapphires around in simple carbon paper. The deep blue carbon rubs off on the rough gem yielding an ‘improved’ coloration, which exhibits top cornflower blues worth a fortune. However this trick can literally come apart in your hands as the blue carbon rubs off the gem and onto your fingers.
Another ‘color enhancement’ trick unique to Sri Lanka enhances yellow sapphires by use of a well-known indigenous tree called the ‘Goraka Tree’. Known for possessing a saffron-yellow resin, a hole is gouged into the soft three trunk and a less than honest dealer presses a pale sapphire into the tree, leaving it there for several days. After wiping clean, the whole gem is stained a rich and vivid yellow color that is extremely convincing—until cut. While practices such as these are deplorable, one can’t help being impressed with the ingenuity of these somewhat creative conmen.
Like any county, and particularly like those who population sometimes sees a disproportionate amount of disadvantaged civilians, Sri Lanka enjoys its fair share of friendly, open, and utterly charming confidence tricksters. Innovative local ‘color enhancement techniques’ are employed on yellow and blue sapphires to obtain high prices. The wily rascals of Elahera roll rough sapphires around in simple carbon paper. The deep blue carbon rubs off on the rough gem yielding an ‘improved’ coloration, which exhibits top cornflower blues worth a fortune. However this trick can literally come apart in your hands as the blue carbon rubs off the gem and onto your fingers.
Another ‘color enhancement’ trick unique to Sri Lanka enhances yellow sapphires by use of a well-known indigenous tree called the ‘Goraka Tree’. Known for possessing a saffron-yellow resin, a hole is gouged into the soft three trunk and a less than honest dealer presses a pale sapphire into the tree, leaving it there for several days. After wiping clean, the whole gem is stained a rich and vivid yellow color that is extremely convincing—until cut. While practices such as these are deplorable, one can’t help being impressed with the ingenuity of these somewhat creative conmen.
Ruby From The Vatomandry Area Of Eastern Madagascar
(via Gemmology Queensland, Vol.5, No.3, March 2004)
For about a year, Thai gem merchants have been selling considerable amounts of ruby from a recently discovered alluvial source in central eastern Madagascar. The principal source of this ruby is an area about 15km south-west of the central coastal town of Vatomandry. Ruby from this deposit has several interesting features:
- A considerable proportion of the rough does not require heat treatment.
- Some of the ruby closely resembles premium Burmese ruby in color.
In the recently published July 2001 issue of The Journal of Gemmology (pp 409-416), Schwartz & Schemetzer have described the identifying features of this ruby. The authors research has revealed that although ruby from this deposit displays the conventional properties of ruby, their fluorescence was weak to medium for LWUV and inert to very weak for SWUV (due to their 0.1-0.7 wt% content of Fe³+).
Characteristic inclusions observed in specimens that had not been treated included:
- Twin lamellae oriented in two directions.
- Intersecting twin lamellae decorated by tube to needle-like masses of white boehmite particles.
- Short needles and twinned or elongated plate-like crystals of rutile that are oriented in three directions.
- No visible growth zoning.
- Clusters of small, colorless to whitish birefringent zircon crystals.
- A few large apatite crystals.
- Healed fractures of variable shapes.
Trace element analysis of Vatomandry ruby revealed that this ruby has a higher (0.1-0.7 wt%) iron content than Burmese ruby (0.005 wt%), and it contains more vanadium (0.005-0.07 wt %) that Thai-Cambodian ruby (0.01 wt%).
Further, the authors suggest that heat treatment of this ruby at low temperature (<1450°C) to remove any purplish overtone could be difficult to detect—particularly if the rubies only had rutile and clusters of zircon as their only inclusions.
The authors conclude that this ruby’s unique trace element chemistry, combined with its lack of growth zoning, short rutile needles, and clusters of small zircon, will allow its discrimination from ruby of similar color but differing provenance such as Burma and Thailand-Cambodia.
For about a year, Thai gem merchants have been selling considerable amounts of ruby from a recently discovered alluvial source in central eastern Madagascar. The principal source of this ruby is an area about 15km south-west of the central coastal town of Vatomandry. Ruby from this deposit has several interesting features:
- A considerable proportion of the rough does not require heat treatment.
- Some of the ruby closely resembles premium Burmese ruby in color.
In the recently published July 2001 issue of The Journal of Gemmology (pp 409-416), Schwartz & Schemetzer have described the identifying features of this ruby. The authors research has revealed that although ruby from this deposit displays the conventional properties of ruby, their fluorescence was weak to medium for LWUV and inert to very weak for SWUV (due to their 0.1-0.7 wt% content of Fe³+).
Characteristic inclusions observed in specimens that had not been treated included:
- Twin lamellae oriented in two directions.
- Intersecting twin lamellae decorated by tube to needle-like masses of white boehmite particles.
- Short needles and twinned or elongated plate-like crystals of rutile that are oriented in three directions.
- No visible growth zoning.
- Clusters of small, colorless to whitish birefringent zircon crystals.
- A few large apatite crystals.
- Healed fractures of variable shapes.
Trace element analysis of Vatomandry ruby revealed that this ruby has a higher (0.1-0.7 wt%) iron content than Burmese ruby (0.005 wt%), and it contains more vanadium (0.005-0.07 wt %) that Thai-Cambodian ruby (0.01 wt%).
Further, the authors suggest that heat treatment of this ruby at low temperature (<1450°C) to remove any purplish overtone could be difficult to detect—particularly if the rubies only had rutile and clusters of zircon as their only inclusions.
The authors conclude that this ruby’s unique trace element chemistry, combined with its lack of growth zoning, short rutile needles, and clusters of small zircon, will allow its discrimination from ruby of similar color but differing provenance such as Burma and Thailand-Cambodia.
Where Did Spectacles Come From?
(via Gemmology Queensland, Vol.4, No.11, November 2003 / IIS Newsletter 80/2003)
Apparently no visual instruments existed at the time of the ancient Egyptians, Greeks, or Romans. At least this view is supported by a letter written by a prominent Roman about 100 B.C in which he stressed his resignation to old age and his complaint that he could no longer read for himself, having instead to rely on his slaves. The Roman tragedian Seneca, born in about 4 B.C is alleged to have read all the books in Rome by peering at them through a glass globe of water to produce magnification. Nero used an emerald held up to his eye while he watched gladiators fight. This is not proof that the Romans had any idea about lenses, since it is likely that Nero used the emerald because of its green color, which filtered the sunlight. Ptolemy mentions the general principle of magnification; but the lenses then available were unsuitable for use in precise magnification.
The oldest known lens was found in the ruins of ancient Nineveh and was made of polished rock crystal, an inch and one-half in diameter. Aristophanes in ‘The Clouds’ refers to a glass for burning holes in parchment and also mentions the use of burning glasses for erasing writing from wax tablets. According to Pliny, physicians used them for cauterizing wounds. Around 1000 A.D the reading stone, what we know as a magnifying glass, was developed. It was a segment of a glass sphere that could be laid against reading material to magnify the letters. It enables presbyopic (short sighted) monks to read and was probably the first reading aid.
The Venetians learned how to produce glass for reading ‘stones’, and later they constructed lenses that could be held in a frame in front of the eyes instead of directly on the reading material. Spectacles as we know them, were invented some 700 hundred years ago, presumably in Northern Italy. The oldest complete specimens date from sometime around 1350 and were found in the excavation of a nunnery near Celle in Germany. The first glasses were made out of beryl, a semi-precious stone, from which glasses obtained their name in Germanic languages, where they are called bril or brille.
The first known artistic representation of eyeglasses was painted by Tommaso da Modena in 1352. He did a series of frescoes of brothers busily reading or copying manuscripts. One holds a magnifying glass, but another has glasses perched on his nose. Once Tommaso had established the precedent, other painters placed spectacles on the noses of all sorts of subjects, probably as a symbol of wisdom and respect.
The first spectacles had quartz lenses because optical glass had not been developed. The lenses were set into bone, metal or even leather mountings, often shaped like two small magnifying glasses with handles riveted together typically in an inverted V shape that could be balanced on the bridge of the nose. The use of spectacles spread from Italy to the Low Countries, Germany, Spain, and France. In England, a Spectacle Makers Company was formed in 1629; its coat of arms showed three pairs of spectacles and a motto: ‘A blessing to the aged’.
Benjamin Franklin in the 1780’s developed the bifocal. Later he wrote, “I therefore had formerly two pairs of spectacles, which I shifted occasionally, as in traveling I sometimes read, and often wanted to regard the prospects. Finding this change troublesome, and not always sufficiently ready, I had the glasses cut and a half of each kind associated in the same circle. By this means, as I wear my own spectacles constantly, I have only to move my eyes by or down, as I want to see distinctly far or near, the proper glasses being always ready.” Modern eyeglass frames can be made of almost any material, including ivory, tortoiseshell, wood, metal, and plastic.
Apparently no visual instruments existed at the time of the ancient Egyptians, Greeks, or Romans. At least this view is supported by a letter written by a prominent Roman about 100 B.C in which he stressed his resignation to old age and his complaint that he could no longer read for himself, having instead to rely on his slaves. The Roman tragedian Seneca, born in about 4 B.C is alleged to have read all the books in Rome by peering at them through a glass globe of water to produce magnification. Nero used an emerald held up to his eye while he watched gladiators fight. This is not proof that the Romans had any idea about lenses, since it is likely that Nero used the emerald because of its green color, which filtered the sunlight. Ptolemy mentions the general principle of magnification; but the lenses then available were unsuitable for use in precise magnification.
The oldest known lens was found in the ruins of ancient Nineveh and was made of polished rock crystal, an inch and one-half in diameter. Aristophanes in ‘The Clouds’ refers to a glass for burning holes in parchment and also mentions the use of burning glasses for erasing writing from wax tablets. According to Pliny, physicians used them for cauterizing wounds. Around 1000 A.D the reading stone, what we know as a magnifying glass, was developed. It was a segment of a glass sphere that could be laid against reading material to magnify the letters. It enables presbyopic (short sighted) monks to read and was probably the first reading aid.
The Venetians learned how to produce glass for reading ‘stones’, and later they constructed lenses that could be held in a frame in front of the eyes instead of directly on the reading material. Spectacles as we know them, were invented some 700 hundred years ago, presumably in Northern Italy. The oldest complete specimens date from sometime around 1350 and were found in the excavation of a nunnery near Celle in Germany. The first glasses were made out of beryl, a semi-precious stone, from which glasses obtained their name in Germanic languages, where they are called bril or brille.
The first known artistic representation of eyeglasses was painted by Tommaso da Modena in 1352. He did a series of frescoes of brothers busily reading or copying manuscripts. One holds a magnifying glass, but another has glasses perched on his nose. Once Tommaso had established the precedent, other painters placed spectacles on the noses of all sorts of subjects, probably as a symbol of wisdom and respect.
The first spectacles had quartz lenses because optical glass had not been developed. The lenses were set into bone, metal or even leather mountings, often shaped like two small magnifying glasses with handles riveted together typically in an inverted V shape that could be balanced on the bridge of the nose. The use of spectacles spread from Italy to the Low Countries, Germany, Spain, and France. In England, a Spectacle Makers Company was formed in 1629; its coat of arms showed three pairs of spectacles and a motto: ‘A blessing to the aged’.
Benjamin Franklin in the 1780’s developed the bifocal. Later he wrote, “I therefore had formerly two pairs of spectacles, which I shifted occasionally, as in traveling I sometimes read, and often wanted to regard the prospects. Finding this change troublesome, and not always sufficiently ready, I had the glasses cut and a half of each kind associated in the same circle. By this means, as I wear my own spectacles constantly, I have only to move my eyes by or down, as I want to see distinctly far or near, the proper glasses being always ready.” Modern eyeglass frames can be made of almost any material, including ivory, tortoiseshell, wood, metal, and plastic.
Administratium
(via Gemmology Queensland, Vol.5, No.6, June 2004) Steve Sorrell writes:
The heaviest element known to science was recently discovered. The element, tentatively named Administratium , has no protons or electrons and thus has an atomic number 0. However, it does have 1 neutron, 125 assistant neutrons, 75 vice neutrons and 111 assistant vice neutrons, giving it an atomic mass of 312. These 312 particles are held together in the nucleus by a force that involves the continuous exchange of meson-like particles called morons.
Since it has no electrons, Administratium is inert. However, it can be detected chemically as it impedes every reaction with which it comes in contact. According to the discoverers, a tiny amount of Administratium caused one reaction to take over 4 days to complete when it would normally occur in less than one second.
Administratium has a normal half-life of approximately 3 years. At this time it doesn’t actually decay but instead undergoes reorganization in which assistant neutrons, vice neutrons, and assistant vice neutrons exchange places. Some studies have shown that the atomic mass actually increased after each reorganization.
Researchers at other laboratories indicated that Administratium occurs naturally in the atmosphere. It tends to concentrate at certain points such as universities, government agencies, large corporations, and schools. The element can be found in the newest, best-appointed and best-maintained buildings.
Scientists point out that Administratium is known to be toxic at any level of concentration and can easily destroy any productive reactions where it is allowed to accumulate. Attempts are being made to determine how Administratium can be controlled to prevent irreversible damage, but results are not promising.
The heaviest element known to science was recently discovered. The element, tentatively named Administratium , has no protons or electrons and thus has an atomic number 0. However, it does have 1 neutron, 125 assistant neutrons, 75 vice neutrons and 111 assistant vice neutrons, giving it an atomic mass of 312. These 312 particles are held together in the nucleus by a force that involves the continuous exchange of meson-like particles called morons.
Since it has no electrons, Administratium is inert. However, it can be detected chemically as it impedes every reaction with which it comes in contact. According to the discoverers, a tiny amount of Administratium caused one reaction to take over 4 days to complete when it would normally occur in less than one second.
Administratium has a normal half-life of approximately 3 years. At this time it doesn’t actually decay but instead undergoes reorganization in which assistant neutrons, vice neutrons, and assistant vice neutrons exchange places. Some studies have shown that the atomic mass actually increased after each reorganization.
Researchers at other laboratories indicated that Administratium occurs naturally in the atmosphere. It tends to concentrate at certain points such as universities, government agencies, large corporations, and schools. The element can be found in the newest, best-appointed and best-maintained buildings.
Scientists point out that Administratium is known to be toxic at any level of concentration and can easily destroy any productive reactions where it is allowed to accumulate. Attempts are being made to determine how Administratium can be controlled to prevent irreversible damage, but results are not promising.
The Monkey Puzzle Tree: Claimed Source Of Jet
(via Gemmology Queensland, Vol.5, No.6, June 2004)
The araucaria family (Araucariaceae) contains three remarkable genera of cone-bearing trees: Araucaria, Agathis, and Wollemia. They are tall trees native to forested regions of South America and Australia. In majestic size and beauty, they certainly rival the coniferous forests of North America and Eurasia. In fact, they are considered the southern counterpart of our northern pine forests. The type genus Araucaria is derived from ‘Arauco’, a region in central Chile where the Araucani Indians live. This is also the land of the ‘monkey puzzle’ tree (A. araucana), so named because the prickly, tangled branches would be difficult for a monkey to climb. Fossil evidence indicates that ancestral araucaria forests resembling the present day monkey puzzle date back to the age of dinosaurs. In fact, it has been suggested the tree’s armor of dagger-like leaves was designed to discourage enormous South American herbivorous dinosaurs, such as Argentinosaurus weighing and estimated 80 to 100 tons. Another ancient South American species called pino parana or parana pine (A. angustifolia) grows in southern Brazil and Argentina.
Any discussion of fossilized araucariads would be incomplete without mentioning a medieval gemstone called jet. Jet is a semi-precious gem excavated in Europe and formed by metamorphosis and anaerobic fossilization of araucaria wood buried under sediments in ancient seas. Ancestral forests that metamorphosed into jet date back to the Jurassic period, about 160 million years ago. They were similar to present day forests of monkey puzzle trees (Araucaria araucana) that grow in South America. Chemically, jet is hard, carbonized form of bituminous coal with a density similar to anthracite coal. Anthracite can be readily identified by its metallic luster. Jet takes a high polish and has been used for shiny black jewelry for thousands of years. It has a specific gravity of 1.3, almost as hard as the ironwood called lignum vitae (Guaiacum officinale). Jet became very popular during the mid 19th century England during the reign of Queen Victoria, and was often worn to ward off evil spirits and during times of mourning. In the first century AD, the Roman naturalist and writer Pliny described the magical and medicinal attributes of this beautiful mineral. The well-known analogy of ‘jet’ and ‘black’ was coined by William Shakespeare in his ‘black as jet’ from Henry VI part 2. One of the most famous areas for mining of Victorian jet is Whitby on the rugged Northeast coast of England. Although they are similar in hardness, anthracite has a metallic luster and jet is dull black. Jet takes a high polish and has been used in various carved jewelry, such as cameos and intaglios. The Victoria jet broach (circa 1890) was a popular item of jewelry during the 19th century.
The araucaria family (Araucariaceae) contains three remarkable genera of cone-bearing trees: Araucaria, Agathis, and Wollemia. They are tall trees native to forested regions of South America and Australia. In majestic size and beauty, they certainly rival the coniferous forests of North America and Eurasia. In fact, they are considered the southern counterpart of our northern pine forests. The type genus Araucaria is derived from ‘Arauco’, a region in central Chile where the Araucani Indians live. This is also the land of the ‘monkey puzzle’ tree (A. araucana), so named because the prickly, tangled branches would be difficult for a monkey to climb. Fossil evidence indicates that ancestral araucaria forests resembling the present day monkey puzzle date back to the age of dinosaurs. In fact, it has been suggested the tree’s armor of dagger-like leaves was designed to discourage enormous South American herbivorous dinosaurs, such as Argentinosaurus weighing and estimated 80 to 100 tons. Another ancient South American species called pino parana or parana pine (A. angustifolia) grows in southern Brazil and Argentina.
Any discussion of fossilized araucariads would be incomplete without mentioning a medieval gemstone called jet. Jet is a semi-precious gem excavated in Europe and formed by metamorphosis and anaerobic fossilization of araucaria wood buried under sediments in ancient seas. Ancestral forests that metamorphosed into jet date back to the Jurassic period, about 160 million years ago. They were similar to present day forests of monkey puzzle trees (Araucaria araucana) that grow in South America. Chemically, jet is hard, carbonized form of bituminous coal with a density similar to anthracite coal. Anthracite can be readily identified by its metallic luster. Jet takes a high polish and has been used for shiny black jewelry for thousands of years. It has a specific gravity of 1.3, almost as hard as the ironwood called lignum vitae (Guaiacum officinale). Jet became very popular during the mid 19th century England during the reign of Queen Victoria, and was often worn to ward off evil spirits and during times of mourning. In the first century AD, the Roman naturalist and writer Pliny described the magical and medicinal attributes of this beautiful mineral. The well-known analogy of ‘jet’ and ‘black’ was coined by William Shakespeare in his ‘black as jet’ from Henry VI part 2. One of the most famous areas for mining of Victorian jet is Whitby on the rugged Northeast coast of England. Although they are similar in hardness, anthracite has a metallic luster and jet is dull black. Jet takes a high polish and has been used in various carved jewelry, such as cameos and intaglios. The Victoria jet broach (circa 1890) was a popular item of jewelry during the 19th century.
Rare Diamond Goes Bright Pink In UV Light
(via Gemmology Queensland, Vol.5, No.7, July 2004/annanova.com 16/1/04)
A potentially unique diamond, which goes vivid pink when exposed to ultraviolet light, has been found in South Africa. The 13.7 carat diamond, being called the Tirisano Easter Diamond, was recovered from the Tirisano Diamond Mine in Ventersdorp diamond district of the Republic of South Africa.
Exposure to (presumably long wave) ultraviolet light causes the diamond to turn vibrant fluorescent pink. It’s not unusual for diamonds to change color in this way, but vivid pink is one of the rarest colors and the stone retains this hue for a period of time after UV exposure. Experts who have examined it so far consider it to be unique but the exact rarity of the stone will have to be established by a laboratory.
It is the property of mining companies Etruscan and Mountain Lake who plan to sell it by auction to a private collector. Les Meyer, a director of National Diamond Marketing, said, “I have had cause to view several million of stones but I have never come across a diamond of this nature, which leads me to believe that it is incredibly rare. It’s an exceptional piece due to the vibrant pink fluorescence and it has caused excitement amongst all who have examined it at National Diamond Marketing. Nobody can quite believe the color transition.”
A potentially unique diamond, which goes vivid pink when exposed to ultraviolet light, has been found in South Africa. The 13.7 carat diamond, being called the Tirisano Easter Diamond, was recovered from the Tirisano Diamond Mine in Ventersdorp diamond district of the Republic of South Africa.
Exposure to (presumably long wave) ultraviolet light causes the diamond to turn vibrant fluorescent pink. It’s not unusual for diamonds to change color in this way, but vivid pink is one of the rarest colors and the stone retains this hue for a period of time after UV exposure. Experts who have examined it so far consider it to be unique but the exact rarity of the stone will have to be established by a laboratory.
It is the property of mining companies Etruscan and Mountain Lake who plan to sell it by auction to a private collector. Les Meyer, a director of National Diamond Marketing, said, “I have had cause to view several million of stones but I have never come across a diamond of this nature, which leads me to believe that it is incredibly rare. It’s an exceptional piece due to the vibrant pink fluorescence and it has caused excitement amongst all who have examined it at National Diamond Marketing. Nobody can quite believe the color transition.”
Subscribe to:
Posts (Atom)