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Graphite

Graphite
General
Category Native mineral
Chemical formula Carbon, C
Identification
Colour Steel black, to grey.
Crystal habit Tabular, six-sided foliated masses, granular to compacted masses.
Crystal system Trigonal
Cleavage Perfect in one direction.
Fracture Flaky, otherwise rough when not on clevage
Mohs Scale hardness 1 - 2
Luster Dull metallic, earthy
Refractive index Opaque
Pleochroism None
Streak Black
Density 2.09–2.23 g/cm³
Fusibility ?
Solubility Molten Ni
Major varieties
Diamond Another allotrope of carbon


Graphite (named by Abraham Gottlob Werner in 1789, from the Greek γραφειν: "to draw/write", for its use in pencils) is one of the allotropes of carbon. (See also allotropes of carbon.) Unlike diamond, graphite is a conductor, and can be used, for instance, as the material in the electrodes of an electrical arc lamp.

Each carbon atom possesses an sp2 orbital hybridisation. The pi orbital electrons delocalized across the hexagonal atomic sheets of carbon contribute the graphite's conductivity. In an oriented piece of graphite, conductivity parallel to these sheets is greater than that perpendicular to these sheets.

The acoustic and thermal properties of graphite are also highly anisotropic, since phonons propagate very quickly along the tightly-bound planes, but are slower to travel from one plane to another.

The loose coupling among the sheets in graphite contributes to another industrially important property -- graphite powder is used as a dry lubricant. Recent studies suggest that an effect called superlubricity can also account for this effect.

It is not often used in pure form as a structural material (with the exception of RCC) due to its brittleness, but the mechanical properties of carbon fiber composites and grey cast iron are strongly influenced by the role of graphite in these materials.

Graphite also finds use as a matrix and moderator within nuclear reactors. Its low neutron cross section also recommends it for use in proposed fusion reactors.

Physical characteristics

Associated minerals include: quartz, calcite, micas, iron meteorites and tourmalines.

Other characteristics: thin flakes are flexible but inelastic, mineral can leave black marks on hands and paper, conducts electricity, and displays superlubricity.

Notable occurrences include New York and Texas, USA; Russia; Mexico; Greenland and India.

Best field indicators are softness, luster, density and streak.

See allotropes of carbon for a comparison with diamond.

The unit cell dimensions are a = b = 245.6 picometres, c = 669.4 pm. The carbon-carbon bond length in the bulk form is 141.8 pm, and the interlayer spacing is c/2 = 334.7 pm.

See also

External links

03-10-2013 05:06:04
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