< 1911 Encyclopædia Britannica

PICENE, C22H14, 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 ethylene dibromide (R. Lespieau, Bull. soc. chim., 1891, (3), 6, p. 238), or by distilling α-dinaphthostilbene (T. Hirn, Ber., 1800, 32, p. 3341). It crystallizes in large colourless plates wi hich possess a blue fluorescence It is soluble in concentrated sulphuric acid with a green colour. Chromic acid in glacial acetic acid solution oxidizes it to picene-quinone, picene-quinone carboxylic acid, and finally to phthalic acid. When heated with hy driodic acid and phosphorus it forms hydrides of composition C22H34 and C22H36 (see F. Bamberger and F.D. Chattaway, Ann., 1805, 284, p. 61).

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