4.8 Article

Light-Absorbing Oligomer Formation in Secondary Organic Aerosol from Reactive Uptake of Isoprene Epoxydiols

Journal

ENVIRONMENTAL SCIENCE & TECHNOLOGY
Volume 48, Issue 20, Pages 12012-12021

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/es503142b

Keywords

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Funding

  1. U.S. Environmental Protection Agency (EPA) [835404]
  2. Electric Power Research Institute (EPRI)
  3. National Oceanic and Atmospheric Administration (NOAA) Climate Program Office's AC4 program [NA13OAR4310064]
  4. Towson University
  5. Camille and Henry Dreyfus Postdoctoral Program in Environmental Chemistry
  6. Office for Undergraduate Research at the University of North Carolina at Chapel Hill
  7. Donald and Linda Raspet Undergraduate Research Fellowship

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Secondary organic aerosol (SOA) produced from reactive uptake and multiphase chemistry of isoprene epoxydiols (IEPOX) has been found to contribute substantially (upward of 33%) to the fine organic aerosol mass over the Southeastern U.S. Brown carbon (BrC) in rural areas of this region has been linked to secondary sources in the summer when the influence of biomass burning is low. We demonstrate the formation of light-absorbing (290 < lambda < 700 nm) SOA constituents from reactive uptake of trans-beta-IEPOX onto preexisting sulfate aerosols as a potential source of secondary BrC. IEPOX-derived BrC generated in controlled chamber experiments under dry, acidic conditions has an average mass absorption coefficient of similar to 300 cm(2) g(-1). Chemical analyses of SOA constituents using UV-visible spectroscopy and high-resolution mass spectrometry indicate the presence of highly unsaturated oligomeric species with molecular weights separated by mass units of 100 (C5H8O2) and 82 (C5H6O) coincident with the observations of enhanced light absorption, suggesting such oligomers as chromophores, and potentially explaining one source of humic-like substances (HULIS) ubiquitously present in atmospheric aerosol. Similar light-absorbing oligomers were identified in fine aerosol collected in the rural Southeastern U.S., supporting their atmospheric relevance and revealing a previously unrecognized source of oligomers derived from isoprene that contributes to ambient fine aerosol mass.

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