Abstract
The interaction between nitrogen monoxide (NO) and organic peroxy radicals (RO2) greatly impacts the formation of highly oxygenated organic molecules (HOM), the key precursors of secondary organic aerosols. It has been thought that HOM production can be significantly suppressed by NO even at low concentrations. Here, we perform dedicated experiments focusing on HOM formation from monoterpenes at low NO concentrations (0 – 82 pptv). We demonstrate that such low NO can enhance HOM production by modulating the RO2 loss and favoring the formation of alkoxy radicals that can continue to autoxidize through isomerization. These insights suggest that HOM yields from typical boreal forest emissions can vary between 2.5%-6.5%, and HOM formation will not be completely inhibited even at high NO concentrations. Our findings challenge the notion that NO monotonically reduces HOM yields by extending the knowledge of RO2-NO interactions to the low-NO regime. This represents a major advance towards an accurate assessment of HOM budgets, especially in low-NO environments, which prevails in the pre-industrial atmosphere, pristine areas, and the upper boundary layer. © 2023, The Author(s).
Original language | English |
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Article number | 3347 |
Journal | Nature Communications |
Volume | 14 |
Issue number | 1 |
DOIs | |
Publication status | Published - 2023 |
Subject classification (UKÄ)
- Meteorology and Atmospheric Sciences
Free keywords
- Aerosols
- Atmosphere
- Monoterpenes
- Nitric Oxide
- Oxidation-Reduction
- monoterpene
- nitric oxide
- organic nitrate
- oxygen
- peroxy radical
- boreal forest
- concentration (composition)
- hydroxyl radical
- nitrous oxide
- organic matter
- oxygenation
- radical
- terpene
- air pollution control
- Article
- atmosphere
- autooxidation
- boundary layer
- chemical environment
- circadian rhythm
- comparative study
- concentration (parameter)
- isomerization
- mass spectrometry
- ozone depletion
- ozonolysis
- relative humidity
- secondary organic aerosol
- stratosphere
- taiga
- temperature
- aerosol
- oxidation reduction reaction