GSTDTAP  > 地球科学
DOI10.5194/acp-17-13187-2017
Kinetic modeling studies of SOA formation from alpha-pinene ozonolysis
Gatzsche, Kathrin1; Iinuma, Yoshiteru1,2; Tilgner, Andreas1; Mutzel, Anke1; Berndt, Torsten1; Wolke, Ralf1
2017-11-08
发表期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
ISSN1680-7316
EISSN1680-7324
出版年2017
卷号17期号:21
文章类型Article
语种英语
国家Germany; Japan
英文摘要

This paper describes the implementation of a kinetic gas-particle partitioning approach used for the simulation of secondary organic aerosol (SOA) formation within the SPectral Aerosol Cloud Chemistry Interaction Model (SPACCIM). The kinetic partitioning considers the diffusion of organic compounds into aerosol particles and the subsequent chemical reactions in the particle phase. The basic kinetic partitioning approach is modified by the implementation of chemical backward reaction of the solute within the particle phase as well as a composition-dependent particle-phase bulk diffusion coefficient. The adapted gasphase chemistry mechanism for alpha-pinene oxidation has been updated due to the recent findings related to the formation of highly oxidized multifunctional organic compounds (HOMs). Experimental results from a LEAK (Leipziger Aerosolkammer) chamber study for alpha-pinene ozonolysis were compared with the model results describing this reaction system.


The performed model studies reveal that the particle-phase bulk diffusion coefficient and the particle-phase reactivity are key parameters for SOA formation. Using the same particle-phase reactivity for both cases, we find that liquid particles with higher particle-phase bulk diffusion coefficients have 310 times more organic material formed in the particle phase compared to higher viscous semi-solid particles with lower particle-phase bulk diffusion coefficients. The model results demonstrate that, even with a moderate particle-phase reactivity, about 61% of the modeled organic mass consists of reaction products that are formed in the liquid particles. This finding emphasizes the potential role of SOA processing. Moreover, the initial organic aerosol mass concentration and the particle radius are of minor importance for the process of SOA formation in liquid particles. A sensitivity study shows that a 22-fold increase in particle size merely leads to a SOA increase of less than 10 %.


Due to two additional implementations, allowing backward reactions in the particle phase and considering a composition-dependent particle-phase bulk diffusion coefficient, the potential overprediction of the SOA mass with the basic kinetic approach is reduced by about 40 %. HOMs are an important compound group in the early stage of SOA formation because they contribute up to 65% of the total SOA mass at this stage. HOMs also induce further SOA formation by providing an absorptive medium for SVOCs (semivolatile organic compounds). This process contributes about 27% of the total organic mass. The model results are very similar to the LEAK chamber results. Overall, the sensitivity studies demonstrate that the particle reactivity and the particle-phase bulk diffusion require a better characterization in order to improve the current model implementations and to validate the assumptions made from the chamber simulations. The successful implementation and testing of the current kinetic gas-particle partitioning approach in a box model framework will allow further applications in a 3-D model for regional-scale process investigations.


领域地球科学
收录类别SCI-E
WOS记录号WOS:000414691700001
WOS关键词SECONDARY ORGANIC AEROSOL ; SELF-DIFFUSION COEFFICIENTS ; PARTICLE-PHASE CHEMISTRY ; ATMOSPHERIC AEROSOLS ; MULTIPHASE CHEMISTRY ; PARTICULATE MATTER ; MULTILAYER MODEL ; BETA-PINENE ; TRANSLATIONAL DIFFUSION ; CHEMICAL-COMPOSITION
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/23852
专题地球科学
作者单位1.Leibniz Inst Tropospher Res TROPOS, Leipzig, Germany;
2.Okinawa Inst Sci & Technol Grad Univ OIST, Okinawa, Japan
推荐引用方式
GB/T 7714
Gatzsche, Kathrin,Iinuma, Yoshiteru,Tilgner, Andreas,et al. Kinetic modeling studies of SOA formation from alpha-pinene ozonolysis[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2017,17(21).
APA Gatzsche, Kathrin,Iinuma, Yoshiteru,Tilgner, Andreas,Mutzel, Anke,Berndt, Torsten,&Wolke, Ralf.(2017).Kinetic modeling studies of SOA formation from alpha-pinene ozonolysis.ATMOSPHERIC CHEMISTRY AND PHYSICS,17(21).
MLA Gatzsche, Kathrin,et al."Kinetic modeling studies of SOA formation from alpha-pinene ozonolysis".ATMOSPHERIC CHEMISTRY AND PHYSICS 17.21(2017).
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