Highly oxidized products from the atmospheric reaction of hydroxyl radicals with isoprene

Isoprene (C<sub>5</sub>H<sub>8</sub>) globally accounts for half of the non-methane hydrocarbon flux into Earth´s atmosphere. Its degradation is mainly initiated by the gas-phase reaction with OH radicals yielding a complex system of RO<sub>2</sub> radicals. Subsequent product formation is not conclusively understood yet. Here we report the observation of C<sub>4</sub>- and C<sub>5</sub>-products from OH + isoprene bearing at least two functional groups. Their production is initiated either by the reaction of initially formed δ-RO<sub>2</sub> radicals with NO or by 1,6 H-shift isomerization of Z-δ-RO<sub>2</sub> radicals. Both reaction channels also form highly oxygenated molecules (HOMs), which could be important for the generation of secondary organic aerosol. C<sub>5</sub>H<sub>9</sub>O<sub>8</sub> and C<sub>5</sub>H<sub>9</sub>O<sub>9</sub> radicals represent the main precursors of closed-shell HOMs. Global simulations revealed that the isoprene-derived HOM-RO<sub>2</sub> production is comparable with that of α-pinene, currently regarded as very important HOM source. This study provides a more complete insight into isoprene´s degradation process including the HOM formation.

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Publication Details

Journal
Nature Communications
Published
2025-02-28
DOI
https://doi.org/10.1038/s41467-025-57336-1
Citations
9
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
11.71
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article

Highly oxidized products from the atmospheric reaction of hydroxyl radicals with isoprene

Hartmut Herrmann, Torsten Berndt, Andreas Tilgner, Erik H. Hoffmann
9 citations
Nature Communications
Atmospheric chemistry and aerosols
11.71
article

Highly oxidized products from the atmospheric reaction of hydroxyl radicals with isoprene

Hartmut Herrmann, Torsten Berndt, Andreas Tilgner, Erik H. Hoffmann
article en
9 citations

Abstract

Isoprene (C<sub>5</sub>H<sub>8</sub>) globally accounts for half of the non-methane hydrocarbon flux into Earth´s atmosphere. Its degradation is mainly initiated by the gas-phase reaction with OH radicals yielding a complex system of RO<sub>2</sub> radicals. Subsequent product formation is not conclusively understood yet. Here we report the observation of C<sub>4</sub>- and C<sub>5</sub>-products from OH + isoprene bearing at least two functional groups. Their production is initiated either by the reaction of initially formed δ-RO<sub>2</sub> radicals with NO or by 1,6 H-shift isomerization of Z-δ-RO<sub>2</sub> radicals. Both reaction channels also form highly oxygenated molecules (HOMs), which could be important for the generation of secondary organic aerosol. C<sub>5</sub>H<sub>9</sub>O<sub>8</sub> and C<sub>5</sub>H<sub>9</sub>O<sub>9</sub> radicals represent the main precursors of closed-shell HOMs. Global simulations revealed that the isoprene-derived HOM-RO<sub>2</sub> production is comparable with that of α-pinene, currently regarded as very important HOM source. This study provides a more complete insight into isoprene´s degradation process including the HOM formation.

Nature CommunicationsVol. 16(1)
Leibniz Institute for Tropospheric Research (DE)
Clean water and sanitation
Openalex Percentile: Top 1%
Atmospheric chemistry and aerosols
11.71
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