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Cinnabar

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For the moth, see Cinnabar moth.
Cinnabar
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General
Category Mineral
Chemical formula mercury(II) sulfide, HgS
Identification
Colour Brownish-red
Crystal habit Rhombohedral to tabular. Granular to massive
Crystal system Hexagonal
Cleavage Prismatic, perfect
Fracture Uneven to subconchoidal
Mohs Scale hardness 2-2.5
Luster Adamantine to dull
Refractive index Transparent to opaque
Pleochroism N/A
Streak Scarlet
Specific gravity 8 - 8.2 g/cm3
Fusibility ?
Solubility 3.10-26 g per 100 mL water
Major varieties
None
Cinnabar, sometimes written cinnabarite, is a name applied to red mercury(II) sulfide (HgS), or native vermilion, the common ore of mercury. The name comes from the Greek - "kinnabari" - used by Theophrastus, and was probably applied to several distinct substances. Other sources say the word comes from the Persian zinjifrah, originally meaning "lost"[[Citing sources citation needed]].

Structure

HgS adopts two structures, i.e. it is dimorphous.Wells, A.F. (1984). Structural Inorganic Chemistry, Oxford: Clarendon Press. ISBN 0-19-855370-6. The more stable form is cinnabar, which has a structure akin to that for HgO: each Hg center has two short Hg-S bonds (2.36 Å), and four longer Hg---S contacts (3.10, 3.10, 3.30, 3.30 Å). The black form of HgS has the zinc blende structure.

Properties

Cinnabar is generally found in a massive, granular or earthy form and is bright scarlet to brick-red in color. It occasionally occurs, however, in crystals with a metallic adamantine luster. The crystals belong to the rhombohedral (trigonal) system, and are generally of rhombohedral habit, sometimes twinned. The twinning in cinnabar is distinctive and forms a penetration twin that is ridged with six ridges surrounding the point of a pyramid. It could be thought of as two scalahedral crystals grown together with one crystal going the opposite way of the other crystal. The hardness of cinnabar is 2 - 2.5, and its specific gravity 8.998.

Cinnabar resembles quartz in its symmetry and certain of its optical characteristics. Like quartz, it exhibits birefringence. It has the highest refractive power of any mineral. Its mean index for sodium light is 3.02, whereas the index for diamond—a substance of remarkable refraction— is 2.42 and that for GaAs is 3.93. See List of indices of refraction.

Occurrence

Cinnabar was mined by the Roman Empire for its mercury content, and it has been the main ore of mercury throughout the centuries. Some mines used by the Romans remain active today. Generally cinnabar occurs as a vein-filling mineral associated with recent volcanic activity and alkaline hot springs.

Cinnabar is found in all localities that yield mercury, notably Almaden (Spain), New Almaden (California), Idrija (Slovenia), New Idria (California), Landsberg, near Ober-Moschel in the Palatinate, Ripa, at the foot of the Apuan Alps (Tuscany), the mountain Avala (Serbia), Huancavelica (Peru), Terlingua (Texas), and the province of Guizhou in China, where fine crystals have been obtained. Cinnabar is still being deposited at the present day from the hot waters of Sulphur Bank, in California, and Steamboat Springs, Nevada.

Extraction of mercury from ore

To produce liquid (quicksilver) mercury, crushed cinnabar ore is roasted in rotary furnaces. Pure mercury separates from sulfur in this process and easily evaporates. A condensing column is used to collect the liquid mercury, which is most often shipped in iron flasks. Abandoned mercury mine processing sites often contain very hazardous waste piles of roasted cinnabar calcines.

Other forms of cinnabar

References

External links

  • For a full list of external links to MSDSs, spectroscopic data, commercial chemicals suppliers etc. for this compound, see [Chemical sources].

See also

 


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