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Graphite is a crystalline, low density and soft allotrope of carbon.
Composition: Carbon
Color: Dark gray to black
Streak (color when crushed to a powder): Black gray
Luster: Metallic to dull
Crystal structure: Hexagonal
Cleavage: Basal in direction 1,1
Fracture: Conchoidal (smooth shell-like)
Density: 119 - 144 lb/ft³ (1.9*10³ - 2.3*10³ kg/m³)
Hardness: 1 - 2 Mohs
Melting temperature: about 6420°F (3550°C)
Name Origin: from the Ancient Greek graphein (to write).
Other distinctive characteristics:
The crystalline structure of graphite consists of hexagonal rings forming thin parallel plates (graphenes). Each carbon atom is covalently bonded to three other atoms in the plate (the angle between two bonds is 120°). The outermost electron shell of a carbon atom has four valence electrons, three of which are used by the covalent bonds. The forth valence electron does not take part in covalent bonds and may be easily displaced from the electron shell by an electric field. These elctrons provide electrical conductivity of graphite.
The graphenes are bonded to each other by weak Van der Waals forces. The layered structure of graphite allows sliding movement of the parallel graphene plates. Weak bonding between the plates determines softness and self-lubricating properties of graphite.
Graphite is rarely found in form of monocrystals. Most of graphite occurs in form of flakes or lumps. Graphite material having fine Grain structure is sometimes named amorphous graphite, however it is not really amorphous but microcrystalline.
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Graphite properties determine the variety of the areas of its applications in industry, transport, energetics, defence, medicine, science.
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