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Names | |
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Preferred IUPAC name
Picene[2] | |
Other names
Dibenzo[a,i]phenanthrene
3,4-Benzchrysene β,β-Binaphthylene ethene | |
Identifiers | |
3D model (JSmol)
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1912414 | |
ChEBI | |
ChemSpider | |
ECHA InfoCard | 100.005.381 |
KEGG | |
PubChem CID
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UNII | |
CompTox Dashboard (EPA)
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Properties | |
C22H14 | |
Molar mass | 278.33 g/mol |
Density | ? g/cm3 |
Melting point | 366 to 367 °C (691 to 693 °F; 639 to 640 K) |
Boiling point | 518 to 520 °C (964 to 968 °F; 791 to 793 K) |
Hazards | |
GHS labelling: | |
Warning | |
H371 | |
P260, P264, P270, P309+P311, P405, P501 | |
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
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Picene is a hydrocarbon found in the pitchy residue obtained in the distillation of peat tar and of petroleum. This is distilled to dryness and the distillate repeatedly recrystallized from cymene. It may be synthetically prepared by the action of anhydrous aluminium chloride on a mixture of naphthalene and 1,2-dibromoethane, or by distilling a-dinaphthostilbene. It crystallizes in large colorless plates which possess a blue fluorescence. It is soluble in concentrated sulfuric acid with a green color. Chromic acid in glacial acetic acid solution oxidizes it to picene-quinone, picene-quinone carboxylic acid, and finally to phthalic acid.
When intercalated with potassium or rubidium and cooled to below 18 K, picene has been reported to exhibit superconductive properties.[3] However, due to the apparent inability to reproduce this work,[4] the superconducting nature of doped picene has been met with heavy scepticism.[5]
Picene is also a major constituent of the hydrocarbon mineral idrialite.
public domain: Chisholm, Hugh, ed. (1911). "Picene". Encyclopædia Britannica. Vol. 21 (11th ed.). Cambridge University Press. p. 581.
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