Photochemical Cloud Processing of Primary Wildfire Emissions as a Potential Source of Secondary Organic Aerosol

  • Sophie Tomaz
  • , Tianqu Cui
  • , Yuzhi Chen
  • , Kenneth G. Sexton
  • , James M. Roberts
  • , Carsten Warneke
  • , Robert J. Yokelson
  • , Jason D. Surratt
  • , Barbara J. Turpin

Research output: Contribution to journalArticlepeer-review

59 Scopus citations

Abstract

We investigated the gas-phase chemical composition of biomass burning (BB) emissions and their role in aqueous secondary organic aerosol (aqSOA) formation through photochemical cloud processing. A high-resolution time-of-flight chemical ionization mass spectrometer using iodide reagent ion chemistry detected more than 100 gas-phase compounds from the emissions of 30 different controlled burns during the 2016 Fire Influence on Regional and Global Environments Experiment (FIREX) at the Fire Science Laboratory. Compounds likely to partition to cloudwater were selected based on high atomic oxygen-to-carbon ratio and abundance. Water solubility was confirmed by detection of these compounds in water after mist chamber collection during controlled burns and analysis using ion chromatography and electrospray ionization interfaced to high-resolution time-of-flight mass spectrometry. Known precursors of aqSOA were found in the primary gaseous BB emissions (e.g., phenols, acetate, and pyruvate). Aqueous OH oxidation of the complex biomass burning mixtures led to rapid depletion of many compounds (e.g., catechol, levoglucosan, methoxyphenol) and formation of others (e.g., oxalate, malonate, mesoxalate). After 150 min of oxidation (approximatively 1 day of cloud processing), oxalate accounted for 13-16% of total dissolved organic carbon. Formation of known SOA components suggests that cloud processing of primary BB emissions forms SOA.

Original languageEnglish
Pages (from-to)11027-11037
Number of pages11
JournalEnvironmental Science and Technology
Volume52
Issue number19
DOIs
StatePublished - Oct 2 2018

Funding

This work was supported by the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office’s AC4 program, award no. NA16OAR4310106. The UNC Biomarker Mass Spectrometry Facility is funded, in part, by the National Institute of Environmental Health Sciences (grant no. P30ES010126). We are thankful to Dr. Zhenfa Zhang for IEPOX synthesis and to Leonard Collins for his help with the ESI-QTOF-MS. We are also thankful to Karen Rossignol, Betsy Abare, and Dr. Hans W. Paerl for nutrient analyses. This work was supported by the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office's AC4 program, award no. NA16OAR4310106. The UNC Biomarker Mass Spectrometry Facility is funded, in part, by the National Institute of Environmental Health Sciences (grant no. P30ES010126). We are thankful to Dr. Zhenfa Zhang for IEPOX synthesis and to Leonard Collins for his help with the ESI-QTOF-MS. We are also thankful to Karen Rossignol, Betsy Abare and Dr. Hans W. Paerl for nutrient analyses.

FundersFunder number
P30ES010126
National Oceanic and Atmospheric AdministrationNA16OAR4310106

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