New Constraints On The Mechanism Of Isoprene Oxidation By OH: Laboratory And Field Observations For DC3, SOAS, And SEAC4RS

Paul O Wennberg1, John D Crounse2, Jason Michael St Clair2, Tran Nguyen3, Alex Teng2 and DC3, SEAC4RS, and SOAS Science Teams, (1)California Institute of Technology, Division of Geological and Planetary Sciences, Pasadena, United States, (2)California Institute of Technology, Pasadena, CA, United States, (3)California Institute of Technology, Pasadena, United States
Abstract:
Measurements of the oxidation products of isoprene in both the laboratory and in the field provide a wealth of new information on the mechanism of isoprene degradation. In particular measurements of hydroperoxides and nitrates provide a key constraints on the flow of carbon via NO, HO2, and unimolecular chemistry.

In the field, we observe transitions from NO-dominated chemistry to oxidation dominated by HO2 and isomerization due to spatial and temporal variability in NOx. This transition maps onto the rate of oxidant production and consumption. We show that the Southeastern US is now undergoing a rapid transition from the former to the latter. Implications for ozone and aerosol formation will be described.

Back to: Atmospheric Gas-Phase and Aerosol Chemistry over the Southeastern United States I