We have studied the adiabatic and autothermal oxidative coupling of me
thane over Pt on alpha-Al2O3 monoliths at space velocities above 10(5)
h(-1). The selectivity to Ct hydrocarbons (primarily acetylene) reach
es a maximum of around 20% at low fuel to oxygen ratios, low dilution,
and high space velocities. These conditions promote a large temperatu
re gradient in the monolith, with an exit temperature of nearly 1500 d
egrees C and an entrance temperature of less than 200 degrees C. This
temperature gradient appears to be the driving force far C-2 hydrocarb
on formation under these conditions. Both homogeneous and heterogeneou
s reactions may be involved in producing coupling products, and a comb
ustion model predicts C-2 selectivities similar to those observed.