Preprints
https://doi.org/10.5194/egusphere-2026-4450
https://doi.org/10.5194/egusphere-2026-4450
13 Aug 2026
 | 13 Aug 2026
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Highly oxygenated organic molecule formation from 2,5-dimethylfuran oxidation by O3 and OH: an experimental and computational study

Rabbia Asgher, Sakshi Jha, Avinash Kumar, Shawon Barua, Prasenjit Seal, Sana Farhoudian, Siddharth Iyer, and Matti Rissanen

Abstract. The gas-phase oxidation of 2,5-dimethylfuran (2,5-DMF) by ozone (O3) and hydroxyl radicals (OH) was investigated in flow reactors at atmospheric pressure and room temperature using nitrate chemical ionization orbitrap mass spectrometry. At a residence time of 0.8 s, highly oxygenated organic molecules (HOM) with up to nine oxygen atoms were detected in the ozonolysis channel, and eight oxygen atoms in the OH channel. These observations demonstrate that sequential intramolecular hydrogen-shift autoxidation is sufficiently rapid to form products with up to nine oxygen atoms on sub-second timescales. At 7 s, C10–C12 accretion products form through different combinations of C5 and C6 alkyl peroxy (RO2) radicals. Quantum chemical calculations using density functional theory and coupled-cluster methods identified a distinct Criegee intermediate geometry (Anti-CI-2A) that provides a plausible route to HOM species containing up to nine oxygen atoms. Its different methyl/hydrogen orientation relative to the conventional Syn and Anti conformers enables a rapid 1,6-H shift, facilitating autoxidation toward O9 formation and suggesting that primary ozonide decomposition in structurally complex ozonolysis systems may access reactive Criegee intermediate geometries beyond the conventional Syn and Anti forms. For OH-initiated oxidation, the proposed mechanism accounts for HOM monomer formation up to O6, with rapid termination and radical recycling limiting further autoxidation. Overall, 2,5-DMF produces low-volatility oxidation products from both ozonolysis and OH-initiated pathways with implications for secondary organic aerosol formation.

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Rabbia Asgher, Sakshi Jha, Avinash Kumar, Shawon Barua, Prasenjit Seal, Sana Farhoudian, Siddharth Iyer, and Matti Rissanen

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Rabbia Asgher, Sakshi Jha, Avinash Kumar, Shawon Barua, Prasenjit Seal, Sana Farhoudian, Siddharth Iyer, and Matti Rissanen
Rabbia Asgher, Sakshi Jha, Avinash Kumar, Shawon Barua, Prasenjit Seal, Sana Farhoudian, Siddharth Iyer, and Matti Rissanen
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Short summary
Furans and substituted furans released by biomass burning react rapidly with ozone and hydroxyl (OH) radicals in the atmosphere. Our laboratory experiments on 2,5-dimethylfuran show that these reactions produce low-volatility, highly oxygenated organic molecules within a fraction of a second through autoxidation. Quantum chemical calculations elucidate the rapid oxidation pathways leading to the formation of these low-volatility vapors that can contribute to atmospheric particle formation.
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