Environmental Science & Technology · 2024 · 11 citations · 66 references
Natural SciencesChemistryEarth SciencesAnalytical ChemistryAtmospheric ChemistryAtmospheric ScienceAerosol ChemistryAir Pollution ChemistryAtmospheric Oxidation ProcessesAtmospheric Radical ChemistryReactive Oxygen SpeciesStratospheric ChemistryHeterogeneous OxidationHydrogen-deuterium ExchangeHydrogen-deuterium Exchange Mass SpectrometryHydrogen-deuterium Exchange SpectroscopyOrganic AerosolsOxidationOxygenated Organic AerosolsPeroxy Radical Chemistry
Heterogeneous oxidative aging of organic aerosols (OA) occurs ubiquitously in the atmosphere, initiated by oxidants, such as the hydroxyl radicals ( • OH). Hydroperoxyl radicals (HO 2 • ) are also an important oxidant in the troposphere, and its gas-phase chemistry has been well studied. However, the role of HO 2 • in heterogeneous OA oxidation remains elusive. Here, we carry out • OH-initiated heterogeneous oxidation of several OA model systems under different HO 2 • conditions in a flow tube reactor and characterize the molecular oxidation products using a suite of mass spectrometry instrumentation. By using hydrogen–deuterium exchange (HDX) with thermal desorption iodide-adduct chemical ionization mass spectrometry, we provide direct observation of organic hydroperoxide (ROOH) formation from heterogeneous HO 2 • and peroxy radicals (RO 2 • ) reactions for the first time. The ROOH may contribute substantially to the oxidation products, varied with the parent OA chemical structure. Furthermore, by regulating RO 2 • reaction pathways, HO 2 • also greatly influence the overall composition of the oxidized OA. Last, we suggest that the RO 2 • + HO 2 • reactions readily occur at the OA particle interface rather than in the particle bulk. These findings provide new mechanistic insights into the heterogeneous OA oxidation chemistry and help fill the critical knowledge gap in understanding atmospheric OA oxidative aging.
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Aerosols, Climate, and the Hydrological Cycle
V. Ramanathan, Paul J. Crutzen, J. T. Kiehl et al. · Science · 2001 · 4.1K citations