Cementite
| Iron alloy phases |
|---|
|
| Steel classes |
|
| Other iron-based materials |
|
Cementite, also known as iron carbide, is a chemical compound of iron and carbon, with the formula Fe3C (or Fe2C:Fe). By weight, it is 6.67% carbon and 93.3% iron. It has an orthorhombic crystal structure.[1] It is a hard, brittle material,[1] normally classified as a ceramic in its pure form, though it is more important in metallurgy.
Contents |
[edit] Metallurgy
In the iron–carbon system (i.e. plain-carbon steels and cast irons) it is a common constituent because ferrite contains at most 0.02wt% of carbon. Therefore, in carbon steels and cast irons that are slowly cooled a portion of the elements is in the form of cementite.[2] It forms directly from the melt in the case of white cast iron. In carbon steel, it either forms from austenite during cooling or from martensite during tempering. An intimate mixture with ferrite, the other product of austenite, forms a lamellar structure called pearlite.
[edit] Pure form
Cementite changes from ferromagnetic to paramagnetic at its Curie temperature of approximately 480 K.[3]
A natural iron carbide (containing minor amounts of nickel and cobalt) occurs in iron meteorites and is called cohenite after the German mineralogist Emil Cohen, who first described it.[4]
[edit] References
- ^ a b Smith & Hashemi 2006, p. 363.
- ^ Smith & Hashemi 2006, pp. 366–372.
- ^ S.W.J. Smith; W. White; S.G. Barker (1911). "The Magnetic Transition Temperature of Cementite". Proc. Phys. Soc. London 24 (1): 62–69. doi:10.1088/1478-7814/24/1/310.
- ^ Vagn F. Buchwald, Handbook of Iron Meteorites, University of California Press 1975.
[edit] Bibliography
- Smith, William F.; Hashemi, Javad (2006). Foundations of Materials Science and Engineering (4th ed.). McGraw-Hill. ISBN 0-07-295358-6.
