Graphite
Carbon in stacked sheets — soft, slippery, electrically conductive, and chemically identical to diamond.
Graphite is carbon in flat hexagonal sheets, strongly bonded within each sheet and only weakly held between them. Those weak interlayer forces are the reason it is soft, why it marks paper, and why it works as a dry lubricant: the sheets slide over one another with very little resistance.
Everything that makes graphite useful and everything that makes diamond useful comes from the same element in a different arrangement. It is the clearest available demonstration that composition alone does not determine a material's properties.
Why it behaves as it does
Graphite is soft and conducts electricity for the same structural reason, and both follow from how the carbon is bonded. The atoms lie in flat hexagonal sheets, strongly bonded within each sheet and held to the sheets above and below only by weak forces. The sheets slide over one another under almost no load, which is why graphite feels slippery, marks paper, and works as a dry lubricant.
Within each sheet, one electron per atom is not tied up in the bonds and is free to move across the plane. That is what makes graphite an electrical conductor while diamond, which uses all four of each atom's electrons in fixed bonds, is an insulator. The two are the same element in different arrangements, and every difference between them comes from that.
Name origin
From Greek graphein, 'to write' — named in 1789, well after the substance had been in use for writing for two centuries under the mistaken name plumbago.
How it forms
Graphite forms when carbon-bearing sediment is metamorphosed. Organic matter buried in mud is progressively stripped of hydrogen and oxygen by heat and pressure until only carbon remains, and given enough of both it orders itself into the layered structure that makes graphite what it is.
The best flake graphite comes from high-grade metamorphic rocks — marble, schist and gneiss — where the process ran to completion. Graphite also crystallises directly from carbon-bearing fluids in veins, and small amounts occur in some igneous rocks, but the metamorphosed-sediment route accounts for essentially all commercial production.
How we know: checked recently · only one source, so there is nothing to cross-check it against · stated directly by the source.
How this connects
Where a connection has been confirmed by an outside reference, that reference is named beside it.
is a polymorph of
- Diamond — mineral · both pure carbon; cubic versus hexagonal layered structure Wikidata
contains
- Carbon — element Wikidata
is used as
- Electrical conduction — application
is commonly confused with
- Diamond — mineral · identical composition, opposite properties — the standard illustration of why structure matters
- Molybdenite — mineral · the reason molybdenite is named after lead: it, graphite and galena were long taken for one substance
is a component of
- Schist — rock · in metamorphosed carbon-rich sediments, and the source of flake graphite — the form batteries and refractories want
- Refractory brick — material · in magnesia-carbon brick for steel ladles, where the carbon stops the slag wetting the grain and is why the lining survives the pour
is an alternative to
- Molybdenite — mineral · as a dry lubricant. Both are layered structures that shear easily, and molybdenite keeps working in vacuum where graphite fails — graphite needs adsorbed water to be slippery at all, which is why it stopped working on spacecraft
is used in
- Lithium-ion cell — object · the anode, unglamorous and the largest component by mass after the cathode
- Pencil — object · the core, and it marks paper because the carbon sheets shear off under almost no pressure — the same property that makes it a lubricant
is associated with
- The wartime materials programmes — event · reactor-grade graphite pure enough not to absorb neutrons, which the German programme could not obtain and which sent it down a slower route
is a source for
- Battery graphite — material · the natural route: flake graphite floated, rounded into potato-shaped particles at a yield of 30 to 50 per cent, purified and coated
Sources
- Material WorldOur own writing
- Wikimedia Foundation · Creative Commons CC0 1.0 Universal (public domain dedication)
- COD Advisory Board / Vilnius University · CC0 — contributors place data in the public domain