Gemstones of the mineral corundum [Ref 1] offer a rainbow of colors for the lapidarist and jewelry maker as displayed in Figure 1.
Traditionally, of these, the ruby and blue sapphire, along with diamond and emerald, are considered to be the four-membered family of precious gems. Corundum gemstones, other than the ruby and blue sapphire, are also considered sapphires, having colors ranging from green to pink.
In this blog, I’ll describe the crystallography of corundum, and the physical and optical properties of corundum, including the sources of the colors in its gemstones. I will also present a gallery of ruby and sapphire mineral specimens.
CRYSTALLOGRAPHY OF CORUNDUM [Ref 1]
Crystal System of Corundum
Corundum crystallizes in the Trigonal System, which has three axes in a plane and are arranged at 120 degrees to each other, with an axis perpendicular to the plane, as shown in Figure 2. Of the typical forms of crystals shown in the figure, corundum frequently crystallizes as a hexagonal prism, terminated by the basal pinacoid; as a bipyramid, the hexagonal prism is terminated by a bipyramid; the rhombehedron and the hexagonal prism are terminated by the rhombehedron, and the schalenohedron. Examples of corundum crystals taking these forms are shown in Figures 5-11. Figure 7 shows a diagram of a crystal exhibiting all of these forms except the rhombohedron and schalenohedron. The latter form is shown by the sapphire crystal in Figure 10.
Twinning in Corundum [Ref 1].
Multiple twinning on the rhombohedral plane with laminar structure with striations on both the basal pinacoid perpendicular to the c-axis and the hexagonal prism or on bipyramid faces, as shown by the terminated bipyrimidal sapphire crystal, shown in Figure 10 [Ref 12]. Corundum is also twinned on the hexagonal prism faces of tabular crystals exhibiting an arrowhead shape, as shown by the sapphire specimen in Figure 11[Ref 13]. The view is at the base of the arrowhead shape and pointing towards the tip. Less frequent twinning in corundum occurs on the basal pinacoid, perpendicular to the long axis of the crystal, as showing repetitive twinning along its length in Figure 12.
The view is at the base of the arrowhead shape and pointing towards the tip. Less frequent twinning in corundum occurs on the basal pinacoid, perpendicular to the long axis of the crystal, as showing repetitive twinning along its length in Figure 12.
The view is at the base of the arrowhead shape and pointing towards the tip. Less frequent twinning in corundum occurs on the basal pinacoid, perpendicular to the long axis of the crystal, as showing repetitive twinning along its length in Figure 12.
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MECHANICAL PROPERTIES OF CORUNDUM [Ref 2]
The high values of hardness and ultimate strength and its resistance to cleavage, underlie the toughness of corundum gemstones and their wide usage in rings and bracelets, both susceptible to impact while worn. Values of the strength factors of corundum are summarized in TABLE I.
TABLE I. STRENGTH FACTORS OF CORUNDUM GEMSTONES
PROPERTY | VALUE/OBSERVATION | REFERENCE |
Mohs Hardness SCALE | 9 (Member of scale) | 11 |
Ultimate Compressive Strength | 435,000 psi | 13 |
Ultimate Tensile Strength | 43,500 psi | 13 |
Flexural Strength | 58, 000 | 13 |
Tenacity | Brittle | 11 |
Fracture | Irregular/Uneven, Conchoidal | 11 |
Cleavage | None Observed | 11 |
OPTICAL PROPERTIES OF CORUNDUM [Ref 1]
The Refractive Index values of corundum lie in the ranges 1.759-1.772 depending on direction of light polarization. These values are considerably below the value of 2.418 for diamond [Ref 3], and underlies the beauty of corundum gemstones being in their vivid colors and not in brilliance or fire.
The light reflected from the surface, without penetration into gemstones is colorless, as often seen in photographs of gemstones, as in Figure 14.
Light scattering from oriented needle-like crystals of rutile, or to colloidal or other material in oriented tubules is observed in the star sapphire and star ruby as described in another blog on star rubies and sapphires [Ref 4].
SOURCES OF COLOR IN CORUNDUM GEMSTONES
Corundum is aluminum oxide, with the formula Al2O3. Each trivalent aluminum Al3+ ion is surrounded by six oxygen ions, located at the tips of an octahedron in the crystal lattice of corundum, shown in Figure 15. Defects in the forms of ions of metal impurities substituting for the aluminum ion, are responsible for the colors of corundum [Ref 5 ]. The impurity metal ions and the associated colors are summarized in Table I, shown in Figure 4. The divalent and trivalent ions substitute for the aluminum ion in the lattice of the corundum lattice.
COLOR CHANGES IN HEAT TREATED SAPPHIRES
Consideration of the various colors in natural sapphires, having different combinations and concentrations of the ions and ion pairs, before and after their heat treatment, serves to demonstrate their effects on color in corundum gemstones. The results of heat treatments are shown in Figures 16-18.
Some sapphires are heat treated to improve the attractiveness of their colors. Studies were carried out to identify changes in concentrations of ions that led to improvements in the aesthetics of the gem stone. The studies showed two major effects in the brown-toned sapphires and in the optical absorption spectrum of sample rO 4/5, red orange. The red trace of the absorption spectrum shows increased absorption due to the chromium ion, a decreased absorption due to trivalent iron ion pairs contributed from paired divalent and trivalent iron ions and single trivalent iron ions. The heat treatment resulted in an increased number of paired divalent iron ions and tetravalent titanium ions. The lessened absorption by iron ions resulted in smaller contributions to the color of the gemstone in the yellow to orange spectral range. Increased trivalent chromium ion concentration resulted in increased absorption of the blue and yellow spectral range and increased transmission in the red spectral range. Increased absorption in the yellow-orange range, due to increased absorption by paired divalent iron and tetravalent titanium ions resulted in increased transmission in the blue spectral range. The lessened transmission in the yellow-orange and increase transmission in the red and blue color ranges resulted in the cherry-pink color of the gemstone.
GALLERY OF SAPPHIRE AND RUBY SPECIMENS
Many specimens on display are from alluvial deposits where erosion of the edges and faces arose from wear against surrounding gravel and sand.
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Ref 1. https://www.mindat.org/min-1136.html
Ref 2. http://www.matweb.com/search/datasheet_print.aspx?matguid=c8c56ad547ae4cfabad15977bfb537f1
Ref 3.
https://refractiveindex.info/?shelf=3d&book=crystals&page=diamond
Ref 4. https://en.wikipedia.org/wiki/Asterism_(gemology)
Ref 5.
Ref 6.
https://www.degruyter.com/downloadpdf/j/adms.2012.12.issue-2/v10077-012-0006-3/v10077-012-0006-3.pdf
FIGURE REFERENCES
Fig 1. https://www.gia.edu/gia-gem-corundum
Fig 2.
Fig 3. http://www.orgoneproducts.eu/crystalsystem/trigonal
Fig 4. http://fredmhaynes.com/2016/06/20/july-birthstone-ruby/
Fig 5. https://m.minerals.net/RoughImage/8/25/Ruby.aspx
Fig 6. https://picclick.com/228-Gram-Natural-Ruby-Gemstone-Cab-Cabochon-Carving-372123410110.html
Fig 7. http://m.palaminerals.com/prilep/
Fig 9. https://www.healingcrystals.com/Ruby_-_Ruby_Tabular_Long_Thin___thick_Crystals__Tanzania_.html
Fig 10. http://www.galleries.com/minerals/gemstone/sapphire/sap-11.jpg
Fig 11. https://www.pinterest.com/pin/239394536426945288
Fig 12. https://www.irocks.com/minerals/specimen/45730
Fig 14. https://www.gemsociety.org/article/how-gems-are-identified/
Fig 15.
Fig16-18. https://www.degruyter.com/downloadpdf/j/adms.2012.12.issue-2/v10077-012-0006-3/v10077-012-0006-3.pdf
Figure 19.
Fig 20. https://www.mindat.org/photo-7589.html
Fig 21. https://www.spiriferminerals.com/index.php?static=127
Fig 22. http://www.atggems.com/Photos_Mineral1.htm
Fig 23.
http://www.johnbetts-fineminerals.com/jhbnyc/mineralmuseum/picshow.php?id=39563
Fig 24. https://www.pinterest.com/pin/838443655598552166/
Fig 25.
http://www.johnbetts-fineminerals.com/jhbnyc/mineralmuseum/picshow.php?id=14016
Fig 26. https://www.irocks.com/minerals/specimen/42723
Fig 27. http://www.palagems.com/gem-spectrum-v1-n2/
http://www.johnbetts-fineminerals.com/jhbnyc/mineralmuseum/picshow.php?id=37057