Multiphase Chemical Kinetics of NO3 Radicals Reacting with Organic Aerosol Components from Biomass Burning

被引:45
|
作者
Shiraiwa, Manabu [2 ]
Poeschl, Ulrich [2 ]
Knopf, Daniel A. [1 ]
机构
[1] SUNY Stony Brook, Inst Terr & Planetary Atmospheres, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA
[2] Max Planck Inst Chem, Biogeochem Dept, D-55128 Mainz, Germany
基金
日本学术振兴会; 美国国家科学基金会;
关键词
GAS-PARTICLE INTERACTIONS; POLYCYCLIC AROMATIC-HYDROCARBONS; CLOUD SURFACE-CHEMISTRY; DOUBLE-LAYER MODEL; HETEROGENEOUS OXIDATION; OLEIC-ACID; SOURCE APPORTIONMENT; BULK CHEMISTRY; DIFFUSION; O-3;
D O I
10.1021/es300677a
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Multiphase reactions with nitrate radicals are among the most important chemical aging processes of organic aerosol particles in the atmosphere especially at nighttime. Reactive uptake of NO3 by organic compounds has been observed in a number of studies, but the pathways of mass transport and chemical reaction remained unclear. Here we apply kinetic flux models to experimental NO3 exposure studies. The model accounts for gas phase diffusion within a cylindrical flow tube, reversible adsorption of NO3, surface-bulk exchange, bulk diffusion, and chemical reactions from the gas-condensed phase interface to the bulk. We resolve the relative contributions of surface and bulk reactions to the uptake of NO3 by levoglucosan and abietic acid, which serve as surrogates and molecular markers of biomass burning aerosol (BBA). Applying the kinetic flux model, we provide the first estimate of the diffusion coefficient of NO3 in amorphous solid organic matrices (10(-8)-10(-7) cm(2) s(-1)) and show that molecular markers are well-conserved in the bulk of solid BBA particles but undergo rapid degradation upon deliquescence/liquefaction at high relative humidity, indicating that the observed concentrations and subsequent apportionment of the biomass burning source could be significantly underestimated.
引用
收藏
页码:6630 / 6636
页数:7
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