A13E-0382
OH radical reactivity in an Indiana Forest: Measurements and model comparisons
OH radical reactivity in an Indiana Forest: Measurements and model comparisons
Monday, 14 December 2015
Poster Hall (Moscone South)
Abstract:
The hydroxyl (OH) radicals plays an important role in the chemistry of the atmosphere. OH radical reactions initiate the oxidation of volatile organic compounds (VOCs) which can lead to the production of ozone and secondary organic aerosols in the atmosphere. In addition, reactions of OH radicals controls the lifetime of methane and other greenhouse gases that affect the radiative balance of the atmosphere. Previous measurements of total hydroxyl radical reactivity in forest environments have found discrepancies between measured values and those calculated from collocated measurements of biogenic VOC (BVOC) concentrations. Additional measurements of total OH reactivity together with measurements of BVOCs are needed to understand the source of this missing reactivity and to further constrain atmospheric chemistry models.Total hydroxyl radical (OH) reactivity was measured using a turbulent flow reactor were made during summer 2015 as part of the Indiana Radical, Reactivity and Ozone Production Intercomparison (IRRONIC). This campaign took place in a forested area at the Indiana Research and Teaching Preserve (IURTP) near the Bloomington campus characterized by high mixing ratios of isoprene and low mixing ratios of NOx. Measurements of a suite of VOCs and oxygenated VOCs was also conducted at the site, allowing a comparison of the observed reactivity with the expected OH reactivity from these measurements.