Photophysical oxidation of HCHO produces HO2 radicals

Formaldehyde, HCHO, is the highest-volume carbonyl in the atmosphere. It absorbs sunlight at wavelengths shorter than 330 nm and photolyses to form H and HCO radicals, which then react with O 2 to form HO 2 . Here we show HCHO has an additional HO 2 formation pathway. At photolysis energies below th...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Nature chemistry 2023-10, Vol.15 (10), p.1350-1357
Hauptverfasser: Welsh, Blair A., Corrigan, Maggie E., Assaf, Emmanuel, Nauta, Klaas, Sebastianelli, Paolo, Jordan, Meredith J. T., Fittschen, Christa, Kable, Scott H.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Formaldehyde, HCHO, is the highest-volume carbonyl in the atmosphere. It absorbs sunlight at wavelengths shorter than 330 nm and photolyses to form H and HCO radicals, which then react with O 2 to form HO 2 . Here we show HCHO has an additional HO 2 formation pathway. At photolysis energies below the energetic threshold for radical formation we directly detect HO 2 at low pressures by cavity ring-down spectroscopy and indirectly detect HO 2 at 1 bar by Fourier-transform infrared spectroscopy end-product analysis. Supported by electronic structure theory and master equation simulations, we attribute this HO 2 to photophysical oxidation (PPO): photoexcited HCHO relaxes non-radiatively to the ground electronic state where the far-from-equilibrium, vibrationally activated HCHO molecules react with thermal O 2 . PPO is likely to be a general mechanism in tropospheric chemistry and, unlike photolysis, PPO will increase with increasing O 2 pressure. In the atmosphere, photolysis of formaldehyde generates H and HCO radicals, which then react with O 2 to form HO 2 (important in converting atmospheric carbon to CO 2 ). Now it has been shown that internally excited formaldehyde can also react with atmospheric O 2 to make HO 2 in a direct, one-step ‘photophysical oxidation’, a mechanism likely to be general in the troposphere.
ISSN:1755-4330
1755-4349
DOI:10.1038/s41557-023-01272-4