Nitramine and nitrosamine formation is a minor pathway in the atmospheric oxidation of methylamine: A theoretical kinetic study of the CH3NH + O2 reaction

The atmospheric oxidation of amines proceeds via initial radical attack at C–H or N–H bonds to form carbon- and nitrogen-centered radicals, respectively. It is conventionally assumed that nitrogen-centered aminyl radicals react slowly with oxygen in the troposphere and associate predominantly with the radicals ^•NO and NO₂^• to form toxic nitrosamines and nitramines. We have used theoretical kinetic modeling techniques to study the prototypical CH₃N^•H + O₂ reaction and have shown that it proceeds to CH₂NH + HO₂^• under tropospheric conditions with a rate coefficient of 3.6 × 10⁻¹⁷ cm³ molecule⁻¹ s⁻¹. Although this value is low compared to the competing NO_x reactions (∼10⁻¹¹ cm³ molecule⁻¹ s⁻¹), the much higher concentration of O₂ versus NO_x in air makes it the dominant process in the atmospheric oxidation of methylamine for NO_x concentrations below 100 ppb. The mechanism identified here is available to amines with primary, secondary, and tertiary α carbons and suggests that they may be less likely to form nitramines and nitrosamines than is currently thought.