Lonsdaleite

Lonsdaleite (named in honour of Kathleen Lonsdale), also called hexagonal diamond in reference to the crystal structure, is an allotrope of carbon with a hexagonal lattice, as opposed to the cubical lattice of conventional diamond. It is found in nature in meteorite debris; when meteors containing graphite strike the Earth, the immense heat and stress of the impact transforms the graphite into diamond, but retains graphite's hexagonal crystal lattice. Lonsdaleite was first identified in 1967 from the Canyon Diablo meteorite, where it occurs as microscopic crystals associated with ordinary diamond.

Lonsdaleite
Crystal structure of lonsdaleite
General
CategoryMineral
Formula
(repeating unit)
C
IMA symbolLon
Strunz classification1.CB.10b
Crystal systemHexagonal
Crystal classDihexagonal dipyramidal (6/mmm)
H-M symbol: (6/m 2/m 2/m)
Space groupP63/mmc
Unit cella = 2.51 Å, c = 4.12 Å; Z = 4
Structure
Jmol (3D)Interactive image
Identification
ColorGray in crystals, pale yellowish to brown in broken fragments
Crystal habitCubes in fine-grained aggregates
Mohs scale hardness7–8 (for impure specimens)
LusterAdamantine
DiaphaneityTransparent
Specific gravity3.2
Optical propertiesUniaxial (+/−)
Refractive indexn = 2.404
References

It is translucent and brownish-yellow and has an index of refraction of 2.40–2.41 and a specific gravity of 3.2–3.3 . Its hardness is theoretically superior to that of cubic diamond (up to 58% more), according to computational simulations, but natural specimens exhibited somewhat lower hardness through a large range of values (from 7–8 on Mohs hardness scale). The cause is speculated as being due to the samples having been riddled with lattice defects and impurities.

In addition to meteorite deposits, hexagonal diamond has been synthesized in the laboratory (1966 or earlier; published in 1967) by compressing and heating graphite either in a static press or using explosives.

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.