中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Sources and formation of carbonaceous aerosols in Xi'an, China: primary emissions and secondary formation constrained by radiocarbon

文献类型:期刊论文

作者Ni, Haiyan1,3,4; Huang, Ru-Jin2,4; Cao, Junji4; Guo, Jie4; Deng, Haoyue1; Dusek, Ulrike1
刊名ATMOSPHERIC CHEMISTRY AND PHYSICS
出版日期2019-12-20
卷号19期号:24页码:15609-15628
ISSN号1680-7316
DOI10.5194/acp-19-15609-2019
通讯作者Huang, Ru-Jin(rujin.huang@ieecas.cn)
英文摘要To investigate the sources and formation mechanisms of carbonaceous aerosols, a major contributor to severe particulate air pollution, radiocarbon (C-14) measurements were conducted on aerosols sampled from November 2015 to November 2016 in Xi'an, China. Based on the C-14 content in elemental carbon (EC), organic carbon (OC) and water-insoluble OC (WIOC), contributions of major sources to carbonaceous aerosols are estimated over a whole seasonal cycle: primary and secondary fossil sources, primary biomass burning, and other non-fossil carbon formed mainly from secondary processes. Primary fossil sources of EC were further sub-divided into coal and liquid fossil fuel combustion by complementing C-14 data with stable carbon isotopic signatures. The dominant EC source was liquid fossil fuel combustion (i.e., vehicle emissions), accounting for 64 % (median; 45 %-74 %, interquartile range) of EC in autumn, 60 % (41 %-72 %) in summer, 53 % (33 %-69 %) in spring and 46 % (29 %-59 %) in winter. An increased contribution from biomass burning to EC was observed in winter (similar to 28 %) compared to other seasons (warm period; similar to 15 %). In winter, coal combustion (similar to 25 %) and biomass burning equally contributed to EC, whereas in the warm period, coal combustion accounted for a larger fraction of EC than biomass burning. The relative contribution of fossil sources to OC was consistently lower than that to EC, with an annual average of 47 +/- 4 %. Non-fossil OC of secondary origin was an important contributor to total OC (35 +/- 4 %) and accounted for more than half of non-fossil OC (67 +/- 6 %) throughout the year. Secondary fossil OC (SOCfossil) concentrations were higher than primary fossil OC (POCfossil) concentrations in winter but lower than POCfossil in the warm period. Fossil WIOC and water-soluble OC (WSOC) have been widely used as proxies for POCfossil and SOCfossil, respectively. This assumption was evaluated by (1) comparing their mass concentrations with POCfossil and SOCfossil and (2) comparing ratios of fossil WIOC to fossil EC to typical primary OC-to-EC ratios from fossil sources including both coal combustion and vehicle emissions. The results suggest that fossil WIOC and fossil WSOC are probably a better approximation for primary and secondary fossil OC, respectively, than POCfossil and SOCfossil estimated using the EC tracer method.
WOS关键词NON-FOSSIL SOURCES ; PM2.5 CHEMICAL-COMPOSITION ; REGIONAL BACKGROUND SITE ; SOLUBLE ORGANIC-CARBON ; WINTER HAZE EPISODE ; SOURCE APPORTIONMENT ; ELEMENTAL CARBON ; ATMOSPHERIC AEROSOLS ; SEASONAL-VARIATIONS ; PARTICULATE MATTER
资助项目National Key Research and Development Program of China[2017YFC0212701] ; National Natural Science Foundation of China[91644219] ; National Natural Science Foundation of China[41877408] ; National Natural Science Foundation of China[41925015] ; KNAW project[530-5CDP30]
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000504010900002
出版者COPERNICUS GESELLSCHAFT MBH
资助机构National Key Research and Development Program of China ; National Natural Science Foundation of China ; KNAW project
源URL[http://ir.ieecas.cn/handle/361006/13107]  
专题地球环境研究所_粉尘与环境研究室
第四纪科学与全球变化卓越创新中心
通讯作者Huang, Ru-Jin
作者单位1.Univ Groningen, Ctr Isotope Res CIO, ESRIG, NL-9747 AG Groningen, Netherlands
2.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Shaanxi, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Ctr Excellence Quaternary Sci & Global Change, Inst Earth Environm,Key Lab Aerosol Chem & Phys, Xian 710061, Shaanxi, Peoples R China
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Ni, Haiyan,Huang, Ru-Jin,Cao, Junji,et al. Sources and formation of carbonaceous aerosols in Xi'an, China: primary emissions and secondary formation constrained by radiocarbon[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2019,19(24):15609-15628.
APA Ni, Haiyan,Huang, Ru-Jin,Cao, Junji,Guo, Jie,Deng, Haoyue,&Dusek, Ulrike.(2019).Sources and formation of carbonaceous aerosols in Xi'an, China: primary emissions and secondary formation constrained by radiocarbon.ATMOSPHERIC CHEMISTRY AND PHYSICS,19(24),15609-15628.
MLA Ni, Haiyan,et al."Sources and formation of carbonaceous aerosols in Xi'an, China: primary emissions and secondary formation constrained by radiocarbon".ATMOSPHERIC CHEMISTRY AND PHYSICS 19.24(2019):15609-15628.

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来源:地球环境研究所

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