Carbon can be found naturally in two crystalline forms: graphite and diamond. Both are chemically similar but quite different in physical properties and crystal structure. Graphite is a crystalline and soft form of carbon. It is a distinct substance that possesses both metal and non-metal qualities.
Graphite is named from the Greek word ‘graphein’, which means ‘to write’. It can be found in igneous and metamorphic rocks. It is usually found in a greyish-black colour. It is opaque and has a shiny black sheen. It has low specific gravity and is a soft mineral. When carbon is exposed to heat and pressure in the Earth’s crust, graphite is formed.
There are two types of graphite: natural and synthetic.
It is a mineral naturally found in the Earth’s crust. It is made up of graphite and carbon. This form of graphite is mined. If it is combined with other minerals, it is extracted. Mineral processes, such as flotation and filtering, are required for its extraction.
Natural graphite is a good heat and electricity conductor and can withstand a wide range of temperatures.
On the basis of crystallinity, this mineral can be divided into three categories:
Synthetic graphite can be produced from coke and pitch. It is not as crystalline as natural graphite but is purer than the latter.
There are two types of synthetic graphite:
Graphite has a covalent structure, which implies that each carbon atom in the graphite molecule is connected by covalent bonds to three other carbon atoms. The carbon atoms are organised hexagonally to form a sheet-like structure. This structure is held in place by weak forces.
Multiple sheets of carbon atoms are parallelly arranged. The atoms in graphite show sp2 hybridization. Graphene refers to the individual layers of graphite. The carbon atoms in each layer are organised in a honeycomb lattice, with 0.142 nm bond length and 0.335 nm plane separation. Atoms in each layer are separated by 2.5 times the space between them.
In the structure of graphite, each carbon atom uses three electrons to create simple connections with the electrons of its three nearest neighbours. At the bonding level, the fourth electron remains. This ‘spare’ electron in each carbon becomes delocalized across the entire sheet of atoms in one layer.
Graphite is a crystalline form of carbon, apart from diamond. It is a soft and naturally occurring mineral form of carbon. The structure of graphite is interconnected hexagonal sheets. There are two kinds of graphite, natural and synthetic. The colour of graphite is greyish black. It is found naturally in the earth’s crust from where it is extracted. Graphite is used in metallurgy, coating, and paint manufacture, among other things.