The ozonolysis of primary aliphatic amines in single and multicomponent fine particles

• Published in: Atmospheric chemistry and physics discussions Vol. 7; no. 5; pp. 14603 - 14638
• Main Authors: Zahardis, J, Geddes, S, Petrucci, G A
• Format: Journal Article
• Language: English
• Published: European Geosciences Union 15.10.2007
• Subjects: Ocean, Atmosphere; Sciences of the Universe
• ISSN: 1680-7367; 1680-7375

The oxidative processing by ozone of the particulate amines octadecylamine (ODA) and hexadecylamine (HDA) is reported. Ozonolysis of these amines resulted in strong NO sub(2) super(− ) and NO sub(3) super(− ) ion signals that increased with ozone exposure as monitored by photoelectron resonance capture ionization aerosol mass spectrometry. These products suggest a mechanism of progressive oxidation of the particulate amines to nitro alkanes. Additionally, a strong ion signal at 125 m/z is assigned to the ion NO sub(3) super(− ) (HNO sub(3)). For ozonized mixed particles containing ODA or HDA + oleic acid (OL), with p sub(O3) greater than or equal to 310 super(&m inus; 7) atm, imine, secondary amide, and tertiary amide products were measured. These products most likely arise from reactions of amines with aldehydes (for imines) and stabilized Criegee intermediates (SCI) or secondary ozonides (for amides) from the fatty acid. The routes to amides via SCI and/or secondary ozonides was shown to be more important than comparable amide forming reactions between amines and organic acids, using azelaic acid as a test compound. Finally, direct evidence is provided for the formation of a surface barrier in the ODA + OL reaction system that resulted in the retention of OL at high ozone exposures (up to 10 super(− 3) atm for 17 s). This effect was not observed in HDA + OL or single component OL particles, suggesting that it may be a species-specific surfactant effect from an in situ generated amide or imine. Implications to tropospheric chemistry, including particle bound amines as sources of oxidized gas phase nitrogen species (e.g. NO sub(2), NO sub(3)), formation of nitrogen enriched HULIS via ozonolysis of amines and source apportionment are discussed.