A21B-0115
Investigation of Organic Peroxy Radical Photolysis as a Source of OH

Tuesday, 15 December 2015
Poster Hall (Moscone South)
Robert F Hansen1, Mark A Blitz1,2, Dwayne E Heard1, Trevor Ingham3, Paul W Seakins1,3 and Lisa K Whalley4, (1)University of Leeds, School of Chemistry, Leeds, United Kingdom, (2)National Centre for Atmospheric Science, Leeds, United Kingdom, (3)National Centre for Atmospheric Science, University of Leeds, Leeds, United Kingdom, (4)University of Leeds, Leeds, United Kingdom
Abstract:
In some environments, models of atmospheric chemistry calculate values of ambient OH concentrations that reasonably (within a factor of 2) agree with measured OH concentrations. However, it has been found in forested environments (low [NOx], high [BVOC]) that models have been less successful in calculating OH concentrations, with measured to modeled ratios of up to 10 reported. Enhanced measured to modelled OH concentrations (a factor of 4) have also been observed in more anthropogenically influenced environments with low concentrations of NOx. These discrepancies suggest the presence of an unknown source of OH. Two candidates for this source are the production of OH following the fast isomerization of organic peroxy (RO2) radicals and the reaction of RO2 with hydroperoxy radicals.

The photolysis of RO2 radicals at ambient wavelengths to yield OH is another possible source of OH that has not been investigated. This process can be quantified by the absorption cross-section of RO2 radicals for OH production (σRO2, OH), which is the product of the total absorption cross-section and the quantum yield of OH. In experiments using a three-laser flash photolysis setup, we have measured σRO2, OH for RO2 derived from isoprene, ethylene, and methacrolein at wavelengths in the near UV (λ=300–360 nm). The measured values of σRO2, OH (ranging from 0.05–1.00 x 10-19 cm-2) over this wavelength range suggest that RO2 photolysis is a significant pathway for OH production. To determine the impact of the OH production from RO2 photolysis on ambient OH concentrations, OH concentrations were calculated with a box model, constrained to the conditions of the OP-3 field campaign in Borneo, that incorporates RO2 photolysis rates derived from measurements of σRO2, OH. It was found that RO2 photolysis increased OH concentrations by approximately 10% over base model chemistry at midday. Measured values of σRO2, OH and the impact on ambient OH concentrations derived from the modeling will be presented and discussed.