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DOI10.1016/j.atmosenv.2020.118164
Carbon isotope seasonal characteristics of fine carbonaceous aerosol in Jinzhong City; Shanxi Province; China
Bai H.; Liu X.; Liu X.; Zhang C.; Mu L.; Peng L.
发表日期2021
ISSN1352-2310
卷号246
英文摘要Stable carbon isotope signatures were observed in organic carbon (OC) and elemental carbon (EC) fractions of fine carbonaceous aerosol (PM2.5) sampled in spring, summer, and winter (December 2013 to August 2014) in Jinzhong in Shanxi Province. The stable carbon isotope composition of EC (δ13CEC) varied from −25.93‰ to −22.20‰ during the sampling (mean value of −24.35 ± 1.11‰), with depletion in summer (−25.44 ± 0.32‰) and enrichment in winter (−23.04 ± 0.71‰). The contribution of vehicle exhaust was 65% in summer, and the contribution of fossil fuel combustion was 92% in winter based on carbon isotope mass balance model. The stable carbon isotope compositions of OC (δ13COC) over the whole sampling period ranged from −29.75‰ to −22.87‰ (mean value of −25.10 ± 1.47‰), with enrichment in winter (−24.12 ± 0.88‰) and depletion in spring (−26.40 ± 1.50‰). Compared with δ13CEC, the δ13COC in spring is depleted in 13C (Δ13COC-EC = δ13COC − δ13CEC = −1.55‰) because of the formation of secondary OC (SOC) from the photo-oxidation reactions. Summertime δ13COC (−24.52 ± 0.28‰) is more positive than δ13CEC because of the strong photochemical aging. The negative value of Δ13COC-EC in winter may be attributed to a complex set of reasons, including the unfavorable meteorological conditions (e.g., low temperature, low boundary layer height, and frequent temperature inversions), coal combustion, vehicle exhaust, gaseous fuel burning, and SOC formation from photo-oxidation reactions of volatile organic compounds (VOCs) caused by fossil fuel combustion. The seasonal variation of δ13CTC was consistent with that of δ13COC, and the annual average δ13CTC (−24.80 ± 1.12‰) implicated fossil fuels combustion. This study highlights that the isotope signatures of EC can be used for source apportionment, reveals the strong influence of atmospheric processing on the isotope signature of OC (e.g., SOC formation and photochemical aging), and suggests the potential application of isotope technology in air pollution research. © 2020 Elsevier Ltd
英文关键词Aerosols; Air pollution; Atmospheric temperature; Boundary layer flow; Boundary layers; Fossil fuels; Isotopes; Organic carbon; Volatile organic compounds; Boundary layer heights; Carbonaceous aerosol; Fossil fuel combustion; Meteorological condition; Seasonal characteristics; Stable carbon isotope compositions; Stable carbon isotopes; Temperature inversions; Coal combustion; carbon; fossil fuel; isotope; organic carbon; volatile organic compound; air quality; atmospheric pollution; carbon isotope; chemical mass balance; combustion; elemental carbon; organic compound; seasonal variation; traffic emission; aerosol; Article; boundary layer; China; city; combustion; controlled study; depletion; low temperature; meteorology; particulate matter 2.5; photochemistry; photooxidation; priority journal; seasonal variation; spring; summer; temperature; winter; China; Jinzhong; Shanxi; Shanxi
语种英语
来源期刊Atmospheric Environment
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/169052
作者单位College of Environmental Science and Engineering, Taiyuan University of Technology, Taiyuan, 030024, China; Shanxi Environmental Protection Institute of Transport (co.,LTD), Taiyuan, 030006, China; College of Civil Engineering, Taiyuan University of Technology, Taiyuan, 030024, China; School of Environment and Chemical Engineering, North China Electric Power University, Beijing, 102206, China
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Bai H.,Liu X.,Liu X.,et al. Carbon isotope seasonal characteristics of fine carbonaceous aerosol in Jinzhong City; Shanxi Province; China[J],2021,246.
APA Bai H.,Liu X.,Liu X.,Zhang C.,Mu L.,&Peng L..(2021).Carbon isotope seasonal characteristics of fine carbonaceous aerosol in Jinzhong City; Shanxi Province; China.Atmospheric Environment,246.
MLA Bai H.,et al."Carbon isotope seasonal characteristics of fine carbonaceous aerosol in Jinzhong City; Shanxi Province; China".Atmospheric Environment 246(2021).
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