Diamond History and Lore

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Why We Love This Gemstone

  • These stones were actively sought by merchants thanks to their appealing ‘ice’ effect and consumers paid higher prices for diamonds with fluorescence.
  • The Gemological Institute of America (GIA) developed 11 clarity scales to decide the quality of a diamond for its sale value.
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The equilibrium pressure varies linearly with temperature, between 1.7 GPa at 0 K and 12 GPa at 5000 K , the diamond/graphite/liquid triple point,. The equilibrium pressure and temperature conditions for a transition between graphite and diamond are well established theoretically and experimentally. In graphite — the bonds between nearest neighbors are even stronger, but the bonds between parallel adjacent planes are weak, so the planes easily slip past each other. It also has a high density, ranging from 3150 to 3530 kilograms per cubic metre (over three times the density of water) in natural diamonds and 3520 kg/m3 in pure diamond. In graphite, the bonds are sp2 orbital hybrids and the atoms form in planes, with each bound to three nearest neighbors, 120 degrees apart. By demonstrating that burning diamond and graphite releases the same amount of gas, he established the chemical equivalence of these substances.

Divine intervention is credited by many cultures with the origin and creation of gemstones — such as diamonds. Methods for grading diamonds and other gemstones have been developed by gemologists in the twentieth century, focusing on characteristics that hold significant value for gems. In the 20th century (gemology experts created grading methods for diamonds and other gemstones), prioritizing the characteristics that are most critical to their value.

The science of diamond grading (which uses the 4Cs and the International Diamond Grading System™), was established by GIA and is now a global standard among jewelry professionals. A contract was made between De Beers and the government of Botswana to purchase the mine’s output, while Botswana aimed to establish its own diamond-cutting industry.

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Some jewelers provide their customers with ammonia-based cleaning kits; ultrasonic cleaners are also popular. Historically — some jewelers’ stones were misgraded because of smudges on the girdle, or dye on the culet. Today, fluorescent natural diamonds are again becoming very desirable with major diamond miners such as the world’s largest diamond producer, Alrosa, reminding the industry of the historic desirability and beauty of naturally fluorescent diamonds. These stones were actively sought by merchants thanks to their appealing ‘ice’ effect and consumers paid higher prices for diamonds with fluorescence. According to the GIA (who reviewed a random sample of 26,010 natural diamonds), 65% of the diamonds in the sample did not fluoresce.

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Diamond is thermodynamically stable at high pressures and temperatures, with the phase transition from graphite occurring at greater temperatures as the pressure increases. A similar proportion of diamonds comes from the lower mantle at depths between 660 and 800 km. They formed in eclogite but are distinguished from diamonds of shallower origin by inclusions of majorite (a form of garnet with excess silicon). Such depths occur below cratons in mantle keels, the thickest part of the lithosphere.

A diamond’s gemstone value is influenced by its color (quality), and weight. Cleaning a diamond can prove challenging (as jewelry settings might hinder the process), and oils, grease, and other hydrophobic substances tend to cling to a diamond. Channel settings position the stones in close proximity to one another, without metal separating them. Shaping a rough diamond into a polished gemstone involves both artistry and scientific techniques. The GIA has created a set of criteria known as Facetware, which serves as the industry standard for grading the cut of round brilliant diamonds. The cut is not only the most crucial aspect of a diamond’s quality as a gemstone, but it is also the most challenging to evaluate quantitatively.

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