An experimental and theoretical study of dimethyl carbonate synthesis on cu-y zeolite

FUEL 90

A. T. Bell, bell@cchem.berkeley.edu, Department of Chemical Engineering, University of California, Berkeley, CA 94720-1462
Experimental and theoretical studies were carried out to define the mechanism and kinetics of the oxidative carbonylation of methanol to dimethyl carbonate (DMC) on Cu-Y. Cu is exchanged into H-Y zeolite by high-temperature reaction with CuCl vapor. Brønsted acid protons are completely exchanged by Cu+, as confirmed by IR spectroscopy, XANES and EXAFS. Upon contact with CH3OH and O2, mono-and di-methoxide species bound to Cu+ cations are formed rapidly. The rate-limiting step in DMC formation is the reaction of CO with mono-methoxide species to form mono-methyl carbonate species, which then react rapidly with methanol to form DMC. An alternate route is the addition of CO to di-methoxide species to form DMC directly. The reaction mechanism, the rate of DMC formation, and the associated activation energy predicted theoretically are in very good agreement with experiment.