The effect of viscosity and diffusion on the HO.sub.2 uptake by sucrose and secondary organic aerosol particles

We report the first measurements of HO.sub.2 uptake coefficients, γ, 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), γ for copper(II)-doped sucrose aerosol particles equalled the su...

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Veröffentlicht in:Atmospheric chemistry and physics 2016-10, Vol.16 (20), p.13035
Hauptverfasser: Lakey, Pascale S. J, Berkemeier, Thomas, Krapf, Manuel, Dommen, Josef, Steimer, Sarah S, Whalley, Lisa K, Ingham, Trevor, Baeza-Romero, Maria T, Pöschl, Ulrich, Shiraiwa, Manabu, Ammann, Markus, Heard, Dwayne E
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Sprache:eng
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Zusammenfassung:We report the first measurements of HO.sub.2 uptake coefficients, γ, 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), γ for copper(II)-doped sucrose aerosol particles equalled the surface mass accommodation coefficient α  =  0.22 ± 0.06, but it decreased to γ  =  0.012 ± 0.007 upon decreasing the RH to 17 %. The trend of γ 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, α-pinene and 1,3,5-trimethylbenzene (TMB), was investigated, yielding low uptake coefficients of γ  
ISSN:1680-7316
1680-7324