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Name | Talc |
---|---|
Category | Silicate mineral |
Caption | Three pieces of Talc. |
Formula | Mg3Si4O10(OH)2 |
Symmetry | Either monoclinic 2m or triclinic |
Cleavage | Perfect on {001} basal cleavage |
Fracture | Flat surfaces (not cleavage), fracture in an uneven pattern |
Tenacity | Sectile |
Mohs | 1 (defining mineral) |
Luster | Waxlike or pearly |
Refractive | nα = 1.538 – 1.550 nβ = 1.589 – 1.594 nγ = 1.589 – 1.600 |
Opticalprop | Biaxial (-) |
Birefringence | δ = 0.051 |
Pleochroism | Weak in dark varieties |
Streak | White to very pearly green |
Gravity | 2.58 to 2.83 |
Diaphaneity | Translucent |
Fluorescence | Short UV=orange yellow, long UV=yellow |
References |
Talc (derived from the Persian tālk (تالک ) via Arabic talk (تلك)) is a mineral composed of hydrated magnesium silicate with the chemical formula H2Mg3(SiO3)4 or Mg3Si4O10(OH)2. In loose form, it is the widely-used substance known as talcum powder. It occurs as foliated to fibrous masses, its crystals being so rare as to be almost unknown. It has a perfect basal cleavage, and the folia are non-elastic, although slightly flexible. It is the softest known mineral and listed as 1 on the Mohs hardness scale. It can be easily scratched by a fingernail. It is also sectile (can be cut with a knife). It has a specific gravity of 2.5–2.8, a clear or dusty luster, and is translucent to opaque. Talc is not soluble in water, but it is slightly soluble in dilute mineral acids. Its colour ranges from white to grey or green and it has a distinctly greasy feel. Its streak is white.
Soapstone is a metamorphic rock composed predominantly of talc.
Talc is a metamorphic mineral resulting from the metamorphism of magnesian minerals such as serpentine, pyroxene, amphibole, olivine, in the presence of carbon dioxide and water. This is known as talc carbonation or steatization and produces a suite of rocks known as talc carbonates.
Talc is primarily formed via hydration and carbonation of serpentine, via the following reaction;
:serpentine + carbon dioxide → talc + magnesite + water :2 Mg3Si2O5(OH)4 + 3CO2 → Mg3Si4O10(OH)2 + 3 MgCO3 + 3 H2O
Talc can also be formed via a reaction between dolomite and silica, which is typical of skarnification of dolomites via silica-flooding in contact metamorphic aureoles;
:dolomite + silica + water → talc + calcite + carbon dioxide :3 CaMg(CO3)2 + 4 SiO2 + H2O → Mg3Si4O10(OH)2 + 3 CaCO3 + 3 CO2
Talc can also be formed from magnesian chlorite and quartz in blueschist and eclogite metamorphism via the following metamorphic reaction:
:chlorite + quartz → kyanite + talc + water
In this reaction, the ratio of talc and kyanite is dependent on aluminium content with more aluminous rocks favoring production of kyanite. This is typically associated with high-pressure, low-temperature minerals such as phengite, garnet, glaucophane within the lower blueschist facies. Such rocks are typically white, friable, and fibrous, and are known as whiteschist.
Talc is a tri-octahedral layered mineral; its structure is similar to that of pyrophyllite, but with magnesium in the octahedral sites of the composite layers.
Talc is also used as food additive or in pharmaceutical products as a glidant. In medicine talc is used as a pleurodesis agent to prevent recurrent pleural effusion or pneumothorax. In the European Union the additive number is E553b.
Talc is widely used in the ceramics industry in both bodies and glazes. In low-fire artware bodies it imparts whiteness and increases thermal expansion to resist crazing. In stonewares, small percentages of talc are used to flux the body and therefore improve strength and vitrification. It is a source of MgO flux in high temperature glazes (to control melting temperature). It is also employed as a matting agent in earthenware glazes and can be used to produce magnesia mattes at high temperatures.
ISO standard for quality (ISO 3262)
Patents are pending on the use of magnesium silicate as a cement substitute. Its production requirements are less energy-intensive than ordinary Portland cement at around 650 °C, while it absorbs far more carbon dioxide as it hardens. This results in a negative carbon footprint overall, as the cement removes 0.6 tonnes of CO2 per tonne used. This contrasts with a carbon footprint of 0.4 tonne per tonne of conventional cement.
Talc is sometimes used as an adulterant to illegal heroin, to expand volume and weight and thereby increase its street value. With intravenous use, it may lead to talcosis, a granulomatous inflammation in the lungs.
The studies reference, by subject: pulmonary issues, lung cancer, skin cancer and ovarian cancer. One of these, published in 1993, was a US National Toxicology Program report, which found that cosmetic grade talc containing no asbestos-like fibres was correlated with tumour formation in rats (animal testing) forced to inhale talc for 6 hours a day, five days a week over at least 113 weeks.
The US Food and Drug Administration (FDA) considers talc (magnesium silicate) to be generally recognized as safe (GRAS) for use as an anti-caking agent in table salt in concentrations smaller than 2%.
Category:Phyllosilicates Category:Magnesium minerals Category:Symbols of Vermont Category:Cosmetics chemicals Category:Excipients Category:IARC Group 3 carcinogens Category:Clay minerals group Category:Arabic words and phrases Category:Monoclinic minerals
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