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cinnabar

 
Dictionary: cin·na·bar   (sĭn'ə-bär') pronunciation
n.
  1. A heavy reddish mercuric sulfide, HgS, that is the principal ore of mercury.
  2. Red mercuric sulfide used as a pigment.
  3. See vermilion (sense 2).

[Middle English cinabare, from Latin cinnabaris, from Greek kinnabari.]

cinnabarine cin'na·bar'ine (-bär'ĭn, -īn, -bə-rīn') adj.

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Cinnabar from Red Devil Mine, north of Homer, Alaska
(click to enlarge)
Cinnabar from Red Devil Mine, north of Homer, Alaska (credit: Courtesy of the MacFall Collection; photograph, Mary A. Root)
Mercury sulfide (HgS), the chief ore mineral of mercury. It is commonly encountered with pyrite, marcasite, and stibnite in veins near recent volcanic rocks and in hot-springs deposits. It has been used as a bright orange-red pigment in stage makeup (now known to be toxic), painting, and Chinese lacquerwork.

For more information on cinnabar, visit Britannica.com.

Sci-Tech Encyclopedia: Cinnabar
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A mineral of composition HgS, crystallizing in the hexagonal system. Crystals are rare, usually of rhombohe-dral habit and often in penetration twins. Cinnabar most commonly occurs in fine, granular, massive form. It has perfect prismatic cleavage, a Mohs hardness of 2.0–2.5, and a density of 8.09. It has either an adamantine luster and vermilion red color or a dull luster and brownish-red color.

Cinnabar is deposited from hydrothermal solutions in veins and as impregnations near recent volcanic rocks and hot springs. It is the principal ore of mercury. Notable occurrences are Almaden, Spain; Idria, Italy; near Belgrade, Yugoslavia; Kweichow and Hunan provinces, China; Soviet Turkistan; New Almaden and New Idria, California; Terlingua, Texas; and several localities in Utah, Nevada, New Mexico, Oregon, and Idaho. See also Mercury (element).



[Ma]

Mercury sulphide (HgS) occurring as a red ore that was used in ancient times as a colouring agent.

 
Columbia Encyclopedia: cinnabar
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cinnabar (sĭn'əbär), mineral, the sulfide of mercury, HgS. Deep red in color, it is used as a pigment (see vermilion), but principally it is a source of the metal mercury. It is mined in Spain, Italy, and in the United States in California. The mercury is obtained from it by roasting, the sulfur combining with oxygen and passing off as sulfur dioxide.


Science Q&A: What is cinnabar?
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Cinnabar is the main ore of the mineral mercury. Its cinnamon to scarlet-red color makes it a colorful mineral. It is produced primarily in the United States (California, Oregon, Texas and Arkansas), Spain, Italy, and Mexico. It is often used as a pigment.

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Rock & Mineral Guide: cinnabar
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HgS
Hexagonal -- Trapezohedral

Environment

In shallow veins and rock impregnations, very often in a quartzite (Almaden, Spain) or serpentine (California).

Crystal description

Well-individualized crystals are rare, crystallized crusts and complex intergrowths fairly common. Twinned intergrowths of steep rhombohedrons found at several localities. Also massive, powdery, and granular, sometimes in capillary needles.

Physical properties

Bright red to brick red to almost black. Luster adamantine; hardness 2Ɖ; specific gravity 8.1; fracture subconchoidal; streak red; cleavage very perfect prismatic. Easily bruised and crushed; translucent to transparent.

Composition

Mercuric sulfide (86.2% Hg, 13.8% S).

Tests

Volatilizes completely on charcoal. In open tube produces sulfur fumes; forms black ring and above this a thin deposit of metallic droplets. This "mercury mirror" can be resolved into drops by scratching over its surface with a needle.

Distinguishing characteristics

Likely to be confused with realgar, cuprite, and possibly "ruby jack" sphalerite or hematite. Easily distinguished by the open-tube test.

Occurrence

Cinnabar, the only ore of mercury, is deposited by epithermal ascending solutions (those near surface and not too hot) far removed from their igneous source. It is associated with native mercury, stibnite, realgar, opal, quartz, and barite. The richest occurrences are on Mt. Avala, Idria, near Belgrade, Serbia; Almadén, Spain; Italy; and Mexico. Historically, the best crystals, including the penetrating rhombohedron type, have been found as scattered individuals up to 2 in. (4-5 cm) in a white calcite matrix in Hunan Province, China. Loose 1-2 in. (3-6 cm) crystals come from the Nikitovka Mine in Ukraine. Briefly, in the late 1920s, the Kirby Mine, Pike Co., Arkansas, had good twins on an iron-stained quartz matrix and enclosed in quartz crystals with hairs of stibnite. Waterworn cinnabar nuggets are found in the Tempati River, Surinam. American deposits are not extensive; the best are in California, with one in Alaska. Smaller quantities have been found in Nevada.



Wikipedia: Cinnabar
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Cinnabar

Cinnabar on Dolomite
General
Category Mineral
Chemical formula mercury(II) sulfide, HgS
Identification
Color Brownish-red
Crystal habit Rhombohedral to tabular. Granular to massive
Crystal system Trigonal - Trapezohedral
Cleavage Prismatic, perfect
Fracture Uneven to subconchoidal
Mohs scale hardness 2-2.5
Luster Adamantine to dull
Streak Scarlet
Specific gravity 8.176
Optical properties Uniaxial (+)
Refractive index nω = 2.905 nε = 3.256
Birefringence δ = 0.351
Solubility 1.04 x 10-25 g per 100 ml water (Ksp at 25°C = 2 x 10-32)[1]
References [2][3][4]

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, a word of uncertain origin. In Latin it was sometimes known as minium, meaning also "red lead", though both of these terms now refer uniquely to lead tetroxide.

Contents

Structure

HgS adopts two structures, i.e. it is dimorphous.[5] 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.[6] It occasionally occurs, however, in crystals with a non-metallic adamantine luster. Cinnabar has a rhombohedral bravais lattice, and belongs to the hexagonal crystal system, trigonal division. Its crystals grow usually in a massive habit, though they are 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 8.1.

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 3.08,[7] whereas the index for diamond—a substance of remarkable refraction— is 2.42 and that for gallium (III) arsenide (GaAs) is 3.93.

Cinnabar Mercury ore from Nevada, USA

Occurrence

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 Puerto Princesa (Philippines); Almadén (Spain); New Almaden (California); Hastings Mine and St. John's Mine, Vallejo, California;[8] Idrija (Slovenia); New Idria (California); Giza,Egypt; Landsberg, near Obermoschel in the Palatinate; Ripa, at the foot of the Apuan Alps (Tuscany); the mountain Avala (Serbia); Laaren, the Netherlands[citation needed]; Huancavelica (Peru); Murfreesboro, Arkansas 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 Mine, in California, and Steamboat Springs, Nevada.

Mining and extraction of mercury

Cinnabar crystals on dolomite from China.

Cinnabar was mined by the Roman Empire both as a pigment (Vitruvius, DA VII; IV-V) (Pliny, HN; XXXIII, XXXVI-XLII) and for its mercury content (Pliny HN; XXXIII, XLI), and it has been the main source of mercury throughout the centuries.

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 metal, which is most often shipped in iron flasks.

Decorative use

Cinnabar has been used for its color in the new world since the Olmec culture.[9] Cinnabar was often used in royal burial chambers during the peak of Mayan civilization. The red stone was inserted into limestone sarcophagi, both as a decoration and, more importantly, to deter vandals and thieves with its well-known toxicity.[10]

The most popularly known use of cinnabar is in Chinese carved lacquerware, a technique that apparently originated in the Song Dynasty.[11] The danger of mercury poisoning may be reduced in ancient lacquerware by entraining the powdered pigment in lacquer,[12] but could still pose an environmental hazard if the pieces were accidentally destroyed. In the modern jewelry industry, the toxic pigment is replaced by a resin-based polymer that approximates the appearance of pigmented lacquer.

In the Byzantine Empire, the Emperor and certain privileged bishops (such as the Ecumenical Patriarch and the Archbishop of Cyprus) were allowed the exclusive right of signing their names with ink colored vermilion by the addition of cinnabar.[citation needed]

Medicinal use

Despite its toxicity, cinnabar has historically been used in traditional Chinese medicine, where it is called zhūshā (朱砂).

Other forms of cinnabar

  • Hepatic cinnabar is an impure variety from the mines of Idrija in the Carniola region of Slovenia, in which the cinnabar is mixed with bituminous and earthy matter.
  • Metacinnabarite is a black-colored form of HgS, which crystallizes in the cubic form.
  • Synthetic cinnabar is produced by treatment of Hg(II) salts with hydrogen sulfide to precipitate black, synthetic metacinnabarite, which is then heated in water. This conversion is promoted by the presence of sodium sulfide.[13]
  • Hypercinnabar, crystallise in the hexagonal form.

See also

References

  1. ^ Meyers, J., Chem. Ed. 63: 689, 1986 
  2. ^ Mineral Handbook
  3. ^ Mindat
  4. ^ Webmineral
  5. ^ Wells, A.F. (1984). Structural Inorganic Chemistry, Oxford: Clarendon Press. ISBN 0-19-855370-6.
  6. ^ King, R. J.. "Minerals explained 37: Cinnabar". Geology Today 18 (5): 195–199. doi:10.1046/j.0266-6979.2003.00366.x. 
  7. ^ Schumann, Walter (1997). Gemstones of the World. New York: Sterling. ISBN 0806994614. 
  8. ^ C.Michael Hogan, Marc Papineau et al., Environmental Assessment of the columbus Parkway Widening between Ascot Parkway and the Northgate Development, Vallejo, Earth Metrics Inc. Report 7853, California State Clearinghouse, Sept, 1989
  9. ^ New World's Oldest, in Time Magazine, Monday, Jul. 29, 1957
  10. ^ Cinnabar-covered ruin.
  11. ^ http://www.askasia.org/teachers/images/image.php?no=659
  12. ^ http://www.cst.cmich.edu/users/dietr1rv/cinnabar.htm R. V. Dietrich, 2005
  13. ^ Holleman, A. F.; Wiberg, E. "Inorganic Chemistry" Academic Press: San Diego, 2001. ISBN 0-12-352651-5.

Other references

  • Martín-Gil, J; Martín-Gil, FJ; Delibes-de-Castro, G; Zapatero-Magdaleno, P; Sarabia-Herrero, FJ (1995). The first use of vermillion. Cellular and Molecular Life Sciences, 51(8):759-761

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