T. Moise et Y. Rudich, Reactive uptake of ozone by proxies for organic aerosols: Surface versus bulk processes, J GEO RES-A, 105(D11), 2000, pp. 14667-14676
Uptake measurements of ozone were conducted with two types of proxies for a
tmospheric organic aerosols: organic liquids and self-assembled organic mon
olayers. Alkanes and terminal alkenes were used. The monolayer surface was
characterized, prior to and after reaction, using IR spectroscopy. Uptake e
xperiments were conducted using a flow tube reactor coupled to a chemical i
onization mass spectrometer. The reactive uptake coefficient, gamma, is sho
wn to be due to reaction with the double bond. For the monolayers, gamma is
composed solely of a surface reactive component and is smaller by at least
an order of magnitude than values obtained for a liquid of the same chain
length. Uptake by the liquids is higher due to solubility and reaction ill
the bulk. The phase of the atmospheric organic aerosol will determine the a
ppropriate use of a bulk or surface uptake probability in atmospheric model
s. Since the aerosol surface is processed and sites are consumed, gamma is
time variant. We define a parameter gamma' as the surface uptake probabilit
y per reactive site and determine its value as 9 x 10(-19) cm(2) molecule(-
1). This enables the modeling of surface reactions as surface site concentr
ations diminish following interaction with the gaseous species.