|Crystal system||6H polytype, most common: hexagonal|
|Crystal class||6H polytype: dihexagonal pyramidal (6mm) |
H-M symbol: (6mm)
|Space group||6H polytype: P63mc|
|Color||Colorless, green, yellow|
|Crystal habit||Generally found as inclusions in other minerals|
|Fracture||Conchoidal – fractures developed in brittle materials characterized by smoothly curving surfaces, e.g., quartz|
|Mohs scale hardness||9.25|
|Luster||Adamantine to metallic|
|Refractive index||nω=2.654 nε=2.967, Birefringence 0.313 (6H form)|
|Melting point||2730 °C (decomposes)|
|Other characteristics||Not radioactive, non-magnetic|
Moissanite // is naturally occurring silicon carbide and its various crystalline polymorphs. It has the chemical formula SiC and is a rare mineral, discovered by the French chemist Henri Moissan in 1893. Silicon carbide is useful for commercial and industrial applications due to its hardness, optical properties and thermal conductivity.
The mineral moissanite was discovered by Henri Moissan while examining rock samples from a meteor crater located in Canyon Diablo, Arizona, in 1893. At first, he mistakenly identified the crystals as diamonds, but in 1904 he identified the crystals as silicon carbide. Artificial silicon carbide had been synthesized in the lab by Edward G. Acheson just two years before Moissan's discovery.
The mineral form of silicon carbide was named in honor of Moissan later on in his life. The discovery in the Canyon Diablo meteorite and other places was challenged for a long time as carborundum contamination had occurred from man-made abrasive tools.
Until the 1950s, no other source for moissanite other than meteorites had been encountered. Then, in 1958, moissanite was found in the Green River Formation in Wyoming and, the following year, as inclusions in kimberlite from a diamond mine in Yakutia. Yet the existence of moissanite in nature was questioned as late as 1986 by the American geologist Charles Milton.
In its natural form moissanite remains very rare. It has been discovered only in a few rocks in the upper mantle and in meteorites. Discoveries show that it occurs naturally as inclusions in diamonds, xenoliths, and such ultramafic rocks as kimberlite and lamproite. It has also been identified as presolar grains in carbonaceous chondrite meteorites.
Analysis of silicon carbide grains found in the Murchison meteorite has revealed anomalous isotopic ratios of carbon and silicon, indicating an extraterrestrial origin from outside the Solar System. 99% of these silicon carbide grains originate around carbon-rich asymptotic giant branch stars. Silicon carbide is commonly found around these stars, as deduced from their infrared spectra.
The crystalline structure is held together with strong covalent bonding similar to diamonds, that allows moissanite to withstand high pressures up to 52.1 gigapascals. Colors vary widely and are graded from D to K range on the diamond color grading scale.
All applications of silicon carbide today use synthetic material, as the natural material is very scarce.
The idea that a silicon-carbon bond might in fact exist in nature was first proposed by the Swedish chemist Jöns Jacob Berzelius as early as 1824, (Berzelius 1824).  In 1891, Edward Goodrich Acheson produced viable minerals that could substitute for diamond as an abrasive and cutting material. This was possible, as moissanite is one of the hardest substances known, with a hardness just below that of diamond and comparable with those of cubic boron nitride and boron. Pure synthetic moissanite can also be made from thermal decomposition of the preceramic polymer poly(methylsilyne), requiring no binding matrix, e.g., cobalt metal powder.
Single-crystalline silicon carbide, in certain forms, has been used for the fabrication of high-performance semiconductor devices. As natural sources of silicon carbide are rare, and only certain atomic arrangements are useful for gemological applications, North Carolina-based Cree Research, Inc., founded in 1987, developed a commercial process for producing large single crystals of silicon carbide. Cree is the world leader in the growth of single crystal silicon carbide, mostly for electronics use.
In 1995 C3 Inc., a company helmed by Charles Eric Hunter, formed Charles & Colvard Ltd. (later changed to Charles & Colvard) to market gem quality moissanite. Charles & Colvard was the first company to produce and sell synthetic moissanite under U.S. patent US5723391 A, first filed by C3 Inc. in North Carolina.
Moissanite was introduced to the jewelry market in 1998 after Charles & Colvard (formerly known as C3 Inc.) received patents to create and market lab-grown silicon carbide gemstones, becoming the first firm to do so. By 2018 all patents on the original process world-wide had expired. Charles & Colvard currently makes and distributes moissanite jewelry and loose gems under the trademarks Forever One, Forever Brilliant, and Forever Classic. Other manufacturers market silicon carbide gemstones under trademarked names such as Amora. In many developed countries, the use of moissanite in jewelry was controlled by the patents held by Charles & Colvard; these patents expired in August 2015 for the United States, 2016 in most other countries, and 2018 in Mexico.
Moissanite is regarded as a diamond alternative, with some optical properties exceeding those of diamond. It is marketed as a lower price alternative to diamond that does not involve the exploitative mining practices used for the extraction of natural diamonds. As some of its properties are quite similar to diamond, moissanite can be used for scams. Testing equipment based on measuring thermal conductivity in particular may give deceiving results. On the Mohs scale of mineral hardness moissanite is rated as 9.25, with diamond being 10 (by definition). In contrast to diamond, moissanite exhibits a thermochromism, such that heating it gradually will cause it to temporarily change color, starting at around 65 °C (150 °F). A more practical test is a measurement of electrical conductivity, which will show higher values for moissanite. Moissanite is birefringent (i.e., light sent through the material splits into separate beams that depend on the source polarization), which can be easily seen, and diamond is not.
Because of its hardness, it can be used in high-pressure experiments, as a replacement for diamond (see diamond anvil cell). Since large diamonds are usually too expensive to be used as anvils, moissanite is more often used in large-volume experiments. Synthetic moissanite is also interesting for electronic and thermal applications because its thermal conductivity is similar to that of diamonds. High power silicon carbide electronic devices are expected to find use in the design of protection circuits used for motors, actuators, and energy storage or pulse power systems. It also exhibits thermoluminescence, making it useful in radiation dosimetry.
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