1)A sink is defi ned here as an irreversible chemical, photochemical or biochemical reaction which removes a molecule from the environment; a perfect sink leads to mineralization. Within this defi nition, the transfer to and the temporary fi xation in another compartment (e.g., soil, vegetation or water) without chemical modifi cation is not considered to be a sink [1].2 Photo-degradation in the Homogenous Gas Phase of the Troposphere Chapter 2: Abiotic Degradation in the Atmosphere 28 k OH (T) = (2.25 + 0.46 -0.39) × 10 -18 T 2 exp{(-910 ± 56)/T} cm 3 molecule -1 s -1 k OH (298 K) = 9.43 × 10 -15 cm 3 molecule -1 s -1More interesting for the average OH lifetime is k OH at the (weighted or effective) average temperature of the troposphere. This temperature has been estimated by Warneck [15] in an analysis of the tropospheric CH 4 + OH reaction as eff = 280 K. According to an earlier estimate, based on the lifetime of chlorinated hydrocarbons [34], this temperature may be as low as 260 K. Using the more recent estimate by Warneck, we obtain k OH (280 K) = 6.84 × 10 -15 cm 3 molecule -1 s -1The average tropospheric OH lifetimes of MCF is calculated to be τ OH = 9.3 a This value is higher than the average residence times calculated for MCF, which are based on long-term measurements of MCF concentrations and estimates of the amounts emitted yearly (see Section 5).MCF is photolysed at wavelengths around 200 nm [28] and can therefore act as a source of chlorine atoms in the stratosphere and contribute to ozone destruction. It has been phased out as a result of the Protocol of Montreal and its follow-up agreements.An up-to-date data collection of OH-reaction rate constants can be found in Chapter 3. Earlier critical data collections are mostly attributable to Roger Atkinson, whose group also measured many substances for the fi rst time