Based on a global average of the OH and NO3 free radial concentration in th
e troposphere, the lifetime of organic chemicals can be calculated from the
rate constant of their reaction with the free radicals. Various models for
estimating the reactivity of organic compounds with the tropospheric free
radicals allow a rapid estimation of their degradability. An overview on th
e existing models - empirical, quantitative structure-activity relationship
s (QSAR) with measured physico-chemical descriptors, QSAR with semiempirica
l quantum-chemical descriptors as well as ab initio molecular orbital calcu
lations - is described and their limitations and range of applicability to
estimate the tropospheric lifetime of an organic compound is discussed.