Multiphase reactions of OH radicals are among the most important pathways of chemical aging of organic aerosols in the atmosphere. Reactive uptake of OH by organic compounds has been observed in a number of studies, but the kinetics of mass transport and chemical reaction are still not fully understood. Here we apply the kinetic multilayer model of gas−particle interactions (KM-GAP) to experimental data from OH exposure studies of levoglucosan and abietic acid, which serve as surrogates and molecular markers of biomass burning aerosol (BBA). The model accounts for gas-phase diffusion within a cylindrical coatedwall flow tube, reversible adsorption of OH, surface-bulk exchange, bulk diffusion, and chemical reactions at the surface and in the bulk of the condensed phase. The nonlinear dependence of OH uptake coefficients on reactant concentrations and time can be reproduced by KM-GAP. We find that the bulk diffusion coefficient of the organic molecules is approximately 10 −16 cm 2 s −1, reflecting an amorphous semisolid state of the organic substrates. The OH uptake is governed by reaction at or near the surface and can be kinetically limited by surface-bulk exchange or bulk diffusion of the organic reactants. Estimates of the chemical half-life of levoglucosan in 200 nm particles in a biomass burning plume increase from 1 day at high relative humidity to 1 week under dry conditions. In BBA particles transported to the free troposphere, the chemical half-life of levoglucosan can exceed 1 month due to slow bulk diffusion in a glassy matrix at low temperature.
■ INTRODUCTIONBiomass burning is one of the largest sources of primary organic aerosols, black carbon, 1 and trace gases in the Earth's atmosphere with a source strength comparable to fossil fuel burning.2−4 Biomass burning aerosol (BBA) has a significant impact on climate and public health. BBAs are ubiquitous and via pyro-convection can also reach the upper troposphere and lower stratosphere regions of the atmosphere. 5−9 They scatter or absorb solar radiation and can serve as cloud condensation nuclei and ice nuclei affecting cloud microphysical and radiative properties. 10,11 Black and brown carbon produced from incomplete combustion are important contributors to the radiative forcing, 12,13 and polycyclic aromatic hydrocarbons (PAHs) associated with BBA can cause adverse health effects such as oxidative stress.
14−16Several field campaigns and remote sensing studies have been performed to investigate the impact of biomass burning on local, regional, and global scales.17−21 The contribution of biomass burning emissions to field-collected particles is typically evaluated by applying chemical receptor-based models, which utilize source-specific molecules, also termed biomolecular markers, found in the particles to identify the source and estimate aerosol source strength. 22 Levoglucosan (1,6-anhydro-β-D-glucopyranose, C 6 H 10 O 5 ) and abietic acid (1-phenanthrenecarboxylic acid, C 20 H 30 O 2 ) are produced during lignin and hemicellulose combust...