4.7 Article

Oligomers, organosulfates, and nitrooxy organosulfates in rainwater identified by ultra-high resolution electrospray ionization FT-ICR mass spectrometry

Journal

ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 9, Issue 7, Pages 2533-2542

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-9-2533-2009

Keywords

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Funding

  1. WHOI FT-MS Users' Facility [OCE-0619608]
  2. US Department of Commerce's National Oceanic and Atmospheric Administration (NOAA) [NA07OAR4310279]
  3. US Department of Agriculture Hatch Funds
  4. National Center for Environmental Research
  5. US Environmental Protection Agency's Science to Achieve Results (STAR) Program [R833751]
  6. United States Environmental Protection Agency
  7. EPA [150141, R833751] Funding Source: Federal RePORTER

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Wet deposition is an important removal mechanism for atmospheric organic matter, and a potentially important input for receiving ecosystems, yet less than 50% of rainwater organic matter is considered chemically characterized. Precipitation samples collected in New Jersey, USA, were analyzed by negative ion ultra-high resolution electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS). Elemental compositions of 552 unique molecular species were determined in the mass range 50-500 Da in the rainwater. Four main groups of organic compounds were identified: compounds containing carbon, hydrogen, and oxygen (CHO) only, sulfur (S) containing CHOS compounds, nitrogen (N) containing CHON compounds, and S- and N-containing CHONS compounds. Organic acids commonly identified in precipitation were detected in the rainwater. Within the four main groups of compounds detected in the rainwater, oligomers, organosulfates, and nitrooxy-organosulfates were assigned based on elemental formula comparisons. The majority of the compounds identified are products of atmospheric reactions and are known contributors to secondary organic aerosol (SOA) formed from gas phase, aerosol phase, and in-cloud reactions in the atmosphere. It is suggested that the large uncharacterized component of SOA is the main contributor to the large uncharacterized component of rainwater organic matter.

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