Homogeneous gas-phase oxychlorination of benzene has been examined in
a flow system between 722 and 1174K. Experiments were performed at atm
ospheric pressure with nitrogen as an inert carrier gas, containing ab
out equal molar amounts of oxygen, HCl and benzene. Apart from chlorob
enzene, substantial amounts of o- and p-chlorophenol are produced. Usi
ng benzonitrile rather than benzene, the three isomers of ClC6H4CN are
formed in about equal amounts. These findings suggest a homolytic mec
hanism with aryl radicals as key intermediates. Thermokinetic analysis
points to formation of chlorophenols via reaction of phenoxyl (formed
from phenyl and oxygen) with HOCl. Chlorination, C6H6 --> C6H5Cl, is
explained by reaction between phenyl radicals and HOCl. With increasin
g temperature (and, therefore, oxygen consumption), slow combustion is
replaced by pyrolysis as the major reaction channel. As a result, abo
ve ca. 1000K, the production of chlorobenzene diminishes, [C6H5Cl] ult
imately being governed by the equilibrium: C6H6 + HCl half arrow right
over half arrow left C6H5Cl + H-2.