Abstract

Organic hydroperoxides (ROOHs) are ubiquitous, reactive oxygen species that play central roles in atmospheric, environmental, and biological chemistry. Because atmospheric ROOHs possess not only −OOH but in most cases other functionalities such as −C(═O) and −OH, they are expected to reside in condensed phases such as aerosols, fog and cloud droplets, and wet films of leaves and soils. Here, we report a study of the kinetics of the liquid-phase decomposition of multifunctionalized C12 α-alkoxyalkyl hydroperoxides (α-AHs) that possessed an ether, a carbonyl, a hydroperoxide, and two hydroxy groups. We derived the rate coefficients (k) from single exponential decays of the α-AH signal in water/ethylene glycol solutions acidified by acids found in the atmosphere. Our discovery that the k of the decomposition of the α-AHs increased exponentially from pH 5.1 to 3.9 but independently of the properties of the acid provided firm evidence that the decomposition was catalyzed by H+. The temperature dependence of k and an Arrhenius plot yielded an activation energy (Ea) of 15.0 ± 0.3 kcal mol–1 for the decomposition of C12 α-AHs in solution. The proposed H+-catalyzed decomposition of ROOHs may be a general process that provides H2O2 and multifunctionalized compounds to atmospheric condensed phases that are acidic in nature.

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