Theoretical Study of the Hydroxyl-Radical-Initiated Degradation Mechanism, Kinetics, and Subsequent Evolution of Methyl and Ethyl Iodides in the Atmosphere.

The degradation and transformation of iodinated alkanes are crucial in the iodine chemical cycle in the marine boundary layer. In this study, MP2 and CCSD(T) methods were adopted to study the atmospheric transformation mechanism and degradation kinetic properties of CH I and CH CH I mediated by ⋅OH radical. The results show that there are three reaction mechanisms including H-abstraction, I-substitution and I-abstraction. The H-abstraction channel producing ⋅CH I and CH C ⋅ HI radicals are the main degradation pathways of CH I and CH CH I, respectively. By means of the variational transition state theory and small curvature tunnel correction method, the rate constants and branching ratios of each reaction are calculated in the temperature range of 200-600 K. The results show that the tunneling effect contributes more to the reaction at low temperatures. Theoretical reaction rate constants of CH I and CH CH I with ⋅OH are calculated to be 1.42×10 and 4.44×10  cm  molecule  s at T=298 K, respectively, which are in good agreement with the experimental values. The atmospheric lifetimes of CH I and CH CH I are evaluated to be 81.51 and 26.07 day, respectively. The subsequent evolution mechanism of ⋅CH I and CH C ⋅ HI in the presence of O , NO and HO indicates that HCHO, CH CHO, and I-atom are the main transformation end-products. This study provides a theoretical basis for insight into the diurnal conversion and environmental implications of iodinated alkanes.