Probing the dynamics and bottleneck of the key atmospheric SO oxidation reaction by the hydroxyl radical.

SO (Sulfur dioxide) is the major precursor to the production of sulfuric acid (HSO), contributing to acid rain and atmospheric aerosols. Sulfuric acid formed from SO generates light-reflecting sulfate aerosol particles in the atmosphere. This property has prompted recent geoengineering proposals to inject sulfuric acid or its precursors into the Earth's atmosphere to increase the planetary albedo to counteract global warming. SO oxidation in the atmosphere by the hydroxyl radical HO to form HOSO is a key rate-limiting step in the mechanism for forming acid rain. However, the dynamics of the HO + SO → HOSO reaction and its slow rate in the atmosphere are poorly understood to date. Herein, we use photoelectron spectroscopy of cryogenically cooled HOSO anion to access the neutral HOSO radical near the transition state of the HO + SO reaction. Spectroscopic and dynamic calculations are conducted on the first ab initio-based full-dimensional potential energy surface to interpret the photoelectron spectra of HOSO and to probe the dynamics of the HO + SO reaction. In addition to the finding of a unique pre-reaction complex (HO⋯SO) directly connected to the transition state, dynamic calculations reveal that the accessible phase space for the HO + SO → HOSO reaction is extremely narrow, forming a key reaction bottleneck and slowing the reaction rate in the atmosphere, despite the low reaction barrier. This study underlines the importance of understanding the full multidimensional potential energy surface to elucidate the dynamics of complex bimolecular reactions involving polyatomic reactants.