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  The effect of viscosity and diffusion on the HO2 uptake by sucrose and secondary organic aerosol particles

Lakey, P. S. J., Berkemeier, T., Krapf, M., Dommen, J., Steimer, S. S., Whalley, L. K., et al. (2016). The effect of viscosity and diffusion on the HO2 uptake by sucrose and secondary organic aerosol particles. Atmospheric Chemistry and Physics, 16(20), 13035-13047. doi:10.5194/acp-16-13035-2016.

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Lakey, Pascale S. J.1, Autor           
Berkemeier, Thomas2, Autor
Krapf, Manuel2, Autor
Dommen, Josef2, Autor
Steimer, Sarah S.2, Autor
Whalley , Lisa K.2, Autor
Ingham, Trevor2, Autor
Baeza-Romero, Maria T.2, Autor
Pöschl, U.1, Autor           
Shiraiwa, M.1, Autor           
Ammann, Markus2, Autor
Heard, Dwayne E.2, Autor
Affiliations:
1Multiphase Chemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_1826290              
2external, ou_persistent22              

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 Zusammenfassung: We report the first measurements of HO2 uptake coefficients, gamma, for secondary organic aerosol (SOA) particles and for the well-studied model compound sucrose which we doped with copper(II). Above 65% relative humidity (RH), gamma for copper(II)-doped sucrose aerosol particles equalled the surface mass accommodation coefficient alpha = 0.22 +/- 0.06, but it decreased to gamma = 0.012 +/- 0.007 upon decreasing the RH to 17 %. The trend of gamma with RH can be explained by an increase in aerosol viscosity and the contribution of a surface reaction, as demonstrated using the kinetic multilayer model of aerosol surface and bulk chemistry (KM-SUB). At high RH the total uptake was driven by reaction in the near-surface bulk and limited by mass accommodation, whilst at low RH it was limited by surface reaction. SOA from two different precursors, alpha-pinene and 1,3,5-trimethylbenzene (TMB), was investigated, yielding low uptake coefficients of gamma < 0.001 and gamma = 0.004 +/- 0.002, respectively. It is postulated that the larger values measured for TMB-derived SOA compared to alpha-pinene-derived SOA are either due to differing viscosity, a different liquid water content of the aerosol particles, or an HO2 + RO2 reaction occurring within the aerosol particles.

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 Datum: 2016
 Publikationsstatus: Erschienen
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 Identifikatoren: ISI: 000386770100003
DOI: 10.5194/acp-16-13035-2016
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Titel: Atmospheric Chemistry and Physics
Genre der Quelle: Zeitschrift
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Ort, Verlag, Ausgabe: Katlenburg-Lindau, Germany : European Geosciences Union
Seiten: - Band / Heft: 16 (20) Artikelnummer: - Start- / Endseite: 13035 - 13047 Identifikator: ISSN: 1680-7316
CoNE: https://pure.mpg.de/cone/journals/resource/111030403014016