Chemical
kinetics plays a fundamental role in the understanding
and modeling of tropospheric chemical processes, one of the most important
being the atmospheric degradation of volatile organic compounds. These
potentially harmful molecules are emitted into the troposphere by
natural and anthropogenic sources and are chemically removed by undergoing
oxidation processes, most frequently initiated by reaction with OH
radicals, the atmosphere’s “detergent”. Obtaining
the respective rate constants is therefore of critical importance,
with calculations based on transition state theory (TST) often being
the preferred choice. However, for molecules with rich conformational
variety, a single-conformer method such as lowest-conformer TST is
unsuitable while state-of-the-art TST-based methodologies easily become
unmanageable. In this Feature Article, the author reviews his own
cost-effective protocol for the calculation of bimolecular rate constants
of OH-initiated reactions in the high-pressure limit based on multiconformer
transition state theory. The protocol, which is easily extendable
to other oxidation reactions involving saturated organic molecules,
is based on a variety of freeware and open-source software and tested
against a series of oxidation reactions of hydrofluoropolyethers,
computationally very challenging molecules with potential environmental
relevance. The main features, advantages and disadvantages of the
protocol are presented, along with an assessment of its predictive
utility based on a comparison with experimental rate constants.