Graphite
Graphite, like diamond, is an allotrope of carbon. They are very similar to each other but the different structures of the molecule affect the chemical and physical properties. Graphite is made of layers of carbon atoms. These layers can slide over each other very easily. This means that it is very soft. It is a dull gray in appearance. Due to the delocalized electrons between the layers, it can conduct electricity very well.
Graphite can be formed from coal put under high heat and pressure. Also, graphite can be turned into diamond with enough heat and pressure. This is how synthetic (man-made) diamonds are made.
Most graphite comes from mines in northeastern China. It is also found in Sri Lanka, Canada and the United States. It is also called Lead Black because it looks like the metal lead. It was named by Abraham Gottlob Werner in 1789 originating from the Greek language.
It can be used as a lubricant to make mechanical devices run smoother. The most common use of graphite is the "lead" in a pencil, which also has clay.
High-purity graphite is used as a neutron moderator in some nuclear reactors, such as RBMKs and AGRs.
Graphite Media
Theoretically predicted phase diagram of carbon
Molar volume against pressure at room temperature
Graphite plates and sheets, 10–15 cm high; mineral specimen from Kimmirut, Canada
Advert for Crane's Black Lead, c. 1905
HB graphite pencils
Structure of Ca-intercalated graphite CaC6
Large graphite specimen. Naturalis Biodiversity Center, Leiden, Netherlands.
This bubble map shows the global distribution of graphite output in 2005 as a percentage of the top producer (China - 1,650,000 tonnes).*This map is consistent with incomplete set of data too as long as the top producer is known. It resolves the accessibility issues faced by colour-coded maps that may not be properly rendered in old computer screens.*Data was extracted on 2nd June 2007. Source -
Scanning tunneling microscope image of graphite surface
