Comprehensive assessment of atmospheric interactions between Criegee intermediate and simplest Imine (CH2NH) in gas and aqueous phase environments

The simplest Criegee intermediate (CH<sub>2</sub>OO), produced through the ozonolysis (O<sub>3</sub>) of ethylene in the Earth's troposphere, plays a crucial role as a precursor in new particle formation (NPF) and secondary organic aerosols (SOA). Recent experimental and theoretical findings suggest that Criegee intermediate (CI) with organic acid, carbonyl, and amines is important for organic aerosol formation. However, the reaction of CI with imine, especially methanimine (CH<sub>2</sub>NH), has not been reported so far. The mechanism for CH<sub>2</sub>OO + CH<sub>2</sub>NH and CH<sub>2</sub>OO + CH<sub>2</sub>NH (+ H<sub>2</sub>O) was studied using ab initio/MD. Our results indicate that the rate constants for the CH₂OO + CH₂NH reaction fall within the range of CH<sub>2</sub>OO + CH<sub>2</sub>O and CH<sub>2</sub>OO + CH<sub>2</sub>CH<sub>2</sub> reaction systems. The product branching ratio analysis indicates that cy-H<sub>2</sub>C(OO)NCH<sub>2</sub> (IM<sub>n</sub>) and formimidic acid (NHCHOH) are the primary products in the gas phase reaction of CH<sub>2</sub>OO + CH<sub>2</sub>NH, irrespective of temperature. Notably, the involvement of water in the reaction facilitates the formation of significant pressure-dependent products, such as N-(hydroxymethyl)formamide (HMF<sub>n)</sub> and IM<sub>n</sub>. Born-Oppenheimer Molecular Dynamics (BOMD) simulations provide strong evidence for IM<sub>n</sub> formation in both the gas phase and the air-water interface, with the reaction proceeding more at the interface. Furthermore, BOMD simulations of CH<sub>2</sub>OO and CH<sub>2</sub>NH interactions on water droplet surfaces highlight the generation of water-mediated loop-structured products, including N-hydroxyethanimine (H<sub>2</sub>C = N-CH<sub>2</sub>-OOH) and HMHP (OH-CH<sub>2</sub>-OOH). This study highlights the potential significance of Criegee-Imine interactions in driving secondary aerosol formation, particularly in areas with elevated nitrogen-based emissions. The findings of this study may offer valuable insights into the CI-imine chemical processes in these regions.

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Journal
Scientific Reports
Published
2025-11-27
DOI
https://doi.org/10.1038/s41598-025-26286-5
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
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article

Comprehensive assessment of atmospheric interactions between Criegee intermediate and simplest Imine (CH2NH) in gas and aqueous phase environments

Manas Ranjan Dash, Mohamad Akbar Ali, Naga Venkateswara Rao Nulakani
Scientific Reports
Atmospheric chemistry and aerosols
article

Comprehensive assessment of atmospheric interactions between Criegee intermediate and simplest Imine (CH2NH) in gas and aqueous phase environments

Manas Ranjan Dash, Mohamad Akbar Ali, Naga Venkateswara Rao Nulakani
article en

Abstract

The simplest Criegee intermediate (CH<sub>2</sub>OO), produced through the ozonolysis (O<sub>3</sub>) of ethylene in the Earth's troposphere, plays a crucial role as a precursor in new particle formation (NPF) and secondary organic aerosols (SOA). Recent experimental and theoretical findings suggest that Criegee intermediate (CI) with organic acid, carbonyl, and amines is important for organic aerosol formation. However, the reaction of CI with imine, especially methanimine (CH<sub>2</sub>NH), has not been reported so far. The mechanism for CH<sub>2</sub>OO + CH<sub>2</sub>NH and CH<sub>2</sub>OO + CH<sub>2</sub>NH (+ H<sub>2</sub>O) was studied using ab initio/MD. Our results indicate that the rate constants for the CH₂OO + CH₂NH reaction fall within the range of CH<sub>2</sub>OO + CH<sub>2</sub>O and CH<sub>2</sub>OO + CH<sub>2</sub>CH<sub>2</sub> reaction systems. The product branching ratio analysis indicates that cy-H<sub>2</sub>C(OO)NCH<sub>2</sub> (IM<sub>n</sub>) and formimidic acid (NHCHOH) are the primary products in the gas phase reaction of CH<sub>2</sub>OO + CH<sub>2</sub>NH, irrespective of temperature. Notably, the involvement of water in the reaction facilitates the formation of significant pressure-dependent products, such as N-(hydroxymethyl)formamide (HMF<sub>n)</sub> and IM<sub>n</sub>. Born-Oppenheimer Molecular Dynamics (BOMD) simulations provide strong evidence for IM<sub>n</sub> formation in both the gas phase and the air-water interface, with the reaction proceeding more at the interface. Furthermore, BOMD simulations of CH<sub>2</sub>OO and CH<sub>2</sub>NH interactions on water droplet surfaces highlight the generation of water-mediated loop-structured products, including N-hydroxyethanimine (H<sub>2</sub>C = N-CH<sub>2</sub>-OOH) and HMHP (OH-CH<sub>2</sub>-OOH). This study highlights the potential significance of Criegee-Imine interactions in driving secondary aerosol formation, particularly in areas with elevated nitrogen-based emissions. The findings of this study may offer valuable insights into the CI-imine chemical processes in these regions.

Scientific ReportsVol. 15(1)
Khalifa University of Science and Technology (AE), Vellore Institute of Technology University (IN)
Khalifa University of Science, Technology and Research
Openalex Percentile: Top 59%
Atmospheric chemistry and aerosols
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