Graphite is a crystalline form of carbon, typically occurring in metamorphic rocks as flakes or crystalline layers. It is formed by the metamorphosis of carbonaceous sediments. In nature, it is also found in igneous rocks, meteorites, and the mineral plumbago. Artificially, it can be prepared by heating powdered coke mixed with some sand and ferric oxide.
Graphite is a covalent solid as its constituent carbon atoms are held strongly by covalent bonds. It is the most stable form of carbon, and when subjected to high pressure and temperature, it can turn into a diamond, but that takes millions of years. The properties of graphite differ from other covalent solids because of its structure.
Although graphite is a form of pure carbon, a non-metal, it displays the properties of both a metal and a nonmetal. The properties of graphite can be attributed to its crystalline structure.
Graphite has a two-dimensional planar structure where each carbon is sp2 hybridised. In a single layer, each individual carbon atom is bonded to three of its neighbouring carbon atoms through covalent bonds forming hexagonal planer rings. The last free valence electron of each atom is free to move between different layers. In the rings, the Carbon–Carbon covalent bond length is 141.5 pm which indicates a strong bonding. Thus, graphite has two-dimensional sheet-like polymeric rings. Each sheet or layer may be regarded as a fused system of benzene rings. Any two successive sheets are about 340 pm apart. This large distance between two successive layers does not permit the formation of covalent bonds. Successive layers are able to slide one over the other due to weak Van der Waals forces holding them.
Graphite is a greyish black, opaque substance with a metallic lustre. It marks a black stain on the paper. Although graphite is flexible, it is not elastic. Graphite’s structure, as discussed above, can be used to explain the characteristic properties of graphite as follows:
The following are the chemical properties of graphite:
C + ½ O2 → CO
C + O2 → CO2
The properties of graphite make it a unique material that has extensive use in the following fields :-
The uniqueness of graphite can be attributed to its crystalline structure. Graphite, or black lead, is a greyish black opaque covalent crystalline solid made purely of carbon. Although it is non-metal, graphite has a metallic lustre and is slippery. It has a low density, high melting point, and it is a coefficient of thermal expansion. Unlike other non-metals, it has high thermal and electrical conductivity. Chemically, graphite is inert, resistant to heat, pressure, and does not react with water or air at standard temperature. However, at very high temperatures and strong oxidising atmospheres, graphite undergoes oxidation to form carbon dioxide. In bulk form, it is non-flammable but combustible. It acts as a reducing agent, reacting violently with strong oxidising agents.
Due to its distinct properties, graphite is used as a lubricant in the making of pencil leads, electrodes for electrical furnaces, high thermal applications, in the steel and glass industry, and in nuclear reactors.