4.8 Article

Molecular Composition and Volatility of Organic Aerosol in the Southeastern US: Implications for IEPDX Derived SOA

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ENVIRONMENTAL SCIENCE & TECHNOLOGY
卷 50, 期 5, 页码 2200-2209

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AMER CHEMICAL SOC
DOI: 10.1021/acs.est.5b04769

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资金

  1. U.S. Department of Energy through Atmospheric System Research (DOE) program [DE-SC0006867]
  2. U.S. Department of Energy through SBIR program [DE-SC0004577]
  3. NSF [AGS-1243354]
  4. EPRI
  5. Directorate For Geosciences
  6. Div Atmospheric & Geospace Sciences [1243354] Funding Source: National Science Foundation
  7. Division Of Chemistry
  8. Direct For Mathematical & Physical Scien [1404573] Funding Source: National Science Foundation
  9. Division Of Chemistry
  10. Direct For Mathematical & Physical Scien [1404644] Funding Source: National Science Foundation

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We present measurements as part of the Southern Oxidant and Aerosol Study (SOAS) during which atmospheric aerosol particles were comprehensively characterized. We present results utilizing a Filter Inlet for Gases and AEROsol coupled to a chemical ionization mass spectrometer (CIMS). We focus on the volatility and composition of isoprene derived organic aerosol tracers and of the bulk organic aerosol. By utilizing the online volatility and molecular composition information provided by the FIGAERO-CIMS, we show that the vast majority of commonly reported molecular tracers of isoprene epoxydiol (IEPDX) derived secondary organic aerosol (SOA) is derived from thermal decomposition of accretion products or other low volatility organics having effective saturation vapor concentrations <10(-3) mu g m(-3). In addition, while accounting for up to 30% of total submicrometer organic aerosol mass, the IEPDX-derived SOA has a higher volatility than the remaining bulk. That IEPDX-SOA, and more generally bulk organic aerosol in the Southeastern U.S. is comprised of effectively nonvolatile material has important implications for modeling SOA derived from isoprene, and for mechanistic interpretations of molecular tracer measurements. Our results show that partitioning theory performs well for 2-methyltetrols, once accretion product decomposition is taken into account. No significant partitioning delays due to aerosol phase or viscosity are observed, and no partitioning to particle-phase water or other unexplained mechanisms are needed to explain our results.

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