The RADM1 gas-phase chemical mechanism was improved by updating rate consta
nts, introducing photodissociation, incorporating the permutation reactions
of organic peroxy radicals, and replacing the lumped NO3 + N2O5 reaction r
ates expressions with explicit ones. Both the original RADM1 and the revise
d RADM1 chemical mechanism were compared with the explicit Master Mechanism
of NCAR (National Center for Atmospheric Research, USA) using the trace ga
s concentrations observed at the China Regional Background Atmospheric Obse
rvatory as model initial conditions. It was shown that the revised RADM1 ch
emical mechanism was much better than the original in modeling atmospheric
chemistry, especially on ozone, for the China region.