期刊
ENVIRONMENTAL SCIENCE & TECHNOLOGY
卷 56, 期 2, 页码 804-813出版社
AMER CHEMICAL SOC
DOI: 10.1021/acs.est.1c06373
关键词
alpha-pinene; pinic acid; beta-caryophyllenic acid; MBTCA; secondary organic aerosol; nitrate radical
资金
- National Institutes of Health [R01 ES029509]
- Natural Science Foundation of China [21177031, 91543130]
The CMAQ model was modified to simulate the formation of secondary organic aerosols (SOA) from different species. The study demonstrates the importance of considering the contribution of various oxidation pathways in accurately estimating organic aerosols. Additionally, equations linking tracer concentrations to SOA concentrations were proposed for better estimation of environmental organic aerosols.
The community multiscale air quality (CMAQ) model was modified to simulate secondary organic aerosol (SOA) formation from five explicit (alpha-pinene, beta-pinene, D-limonene, Delta(3)-carene, and sabinene) and one lumped monoterpene (MT) species and sesquiterpenes (SQTs). The contribution of each oxidation pathway [including OH, O-3, NO3, and O(P-3)] was explicitly tracked in the SOA module. Three MT SOA tracers (pinic acid, PA; pinonic acid, PNA; and 3-methyl-1,2,3-butanetricarboxylic acid, MBTCA) and one SQT SOA tracer (beta-caryophyllinic acid, BCARYA) were modeled to assess the tracer-to-SOA ratios (f(SOA)) for ambient SOA estimation. Good model performance for BCARYA and MBTCA and reasonable agreement between model predictions and observations of PA and PNA were achieved. The modeled daily f(SOA) showed significant variations, suggesting that using the chamber-derived constant f(SOA) could lead to large errors in estimating terpene SOA. Among the four tracers, MBTCA and BCARYA were more appropriate for tracking MT and SQT SOA due to their nonvolatility. Their f(SOA) values mainly depend on the organic aerosol loading and could be approximated using simple power-law equations. In addition, equations directly linking the tracer concentrations to the corresponding SOA concentrations were proposed and could lead to good SOA estimations. This work provides new insights into the formation of the key MT and SQT SOA tracers and would allow better assessments of the biogenic emissions to regional and global aerosol burden.
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