Fossil and Non-fossil Fuel Sources of Organic and Elemental Carbonaceous Aerosol in Beijing, Shanghai, and Guangzhou: Seasonal Carbon Source Variation

Abstract We measured the radiocarbon isotope signals in various fractions of carbonaceous aerosols sampled across four seasons (Oct 2013−Jul 2014) in three megacities of China, viz., Beijing, Shanghai, and Guangzhou. The contributions of fossil fuel (FF) and non-fossil fuel (NF) to the carbonaceous...

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Main Authors: Di Liu, Matthias Vonwiller, Jun Li, Junwen Liu, Sönke Szidat, Yanlin Zhang, Chongguo Tian, Yinjun Chen, Zhineng Cheng, Guangcai Zhong, Pingqing Fu, Gan Zhang
Format: Article
Language:English
Published: Springer 2020-06-01
Series:Aerosol and Air Quality Research
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Online Access:https://doi.org/10.4209/aaqr.2019.12.0642
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author Di Liu
Matthias Vonwiller
Jun Li
Junwen Liu
Sönke Szidat
Yanlin Zhang
Chongguo Tian
Yinjun Chen
Zhineng Cheng
Guangcai Zhong
Pingqing Fu
Gan Zhang
author_facet Di Liu
Matthias Vonwiller
Jun Li
Junwen Liu
Sönke Szidat
Yanlin Zhang
Chongguo Tian
Yinjun Chen
Zhineng Cheng
Guangcai Zhong
Pingqing Fu
Gan Zhang
author_sort Di Liu
collection DOAJ
description Abstract We measured the radiocarbon isotope signals in various fractions of carbonaceous aerosols sampled across four seasons (Oct 2013−Jul 2014) in three megacities of China, viz., Beijing, Shanghai, and Guangzhou. The contributions of fossil fuel (FF) and non-fossil fuel (NF) to the carbonaceous aerosol were estimated based on the radiocarbon content in the organic carbon (OC), water-soluble organic carbon (WSOC), water-insoluble organic carbon (WIOC), and elemental carbon (EC). Although NF generated the primary share (> 55%) during autumn in all of the cities, the seasonal contributions of the sources differed by location during the rest of the year. During winter, FF emissions constituted the majority of the carbonaceous pollution (64%) in Beijing, probably as a result of increased coal combustion for heating. On average, the EC, WSOC, and WIOC generated by FF composed ~10%, 35%, and 19% of the total carbon (TC). Overall, NF was identified as the largest source of carbonaceous aerosol in Guangzhou (63%), whereas FF was the largest source, contributing slightly more than NF, in Shanghai (54%). During spring and summer, FF played a greater role than NF in Beijing (~55%) and Guangzhou (~63%); additionally, based on our limited number of samples, it contributed 71% in Shanghai during the latter season, with a significant portion due to fuel combustion (i.e., industrial, vehicular, fishing-boat, and large-vessel emissions).
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institution Kabale University
issn 1680-8584
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language English
publishDate 2020-06-01
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record_format Article
series Aerosol and Air Quality Research
spelling doaj-art-9a0a3b55043641fbbf6a457660fdf8262025-02-09T12:19:05ZengSpringerAerosol and Air Quality Research1680-85842071-14092020-06-0120112495250610.4209/aaqr.2019.12.0642Fossil and Non-fossil Fuel Sources of Organic and Elemental Carbonaceous Aerosol in Beijing, Shanghai, and Guangzhou: Seasonal Carbon Source VariationDi Liu0Matthias Vonwiller1Jun Li2Junwen Liu3Sönke Szidat4Yanlin Zhang5Chongguo Tian6Yinjun Chen7Zhineng Cheng8Guangcai Zhong9Pingqing Fu10Gan Zhang11State Key Laboratory of Organic Geochemistry and Guangdong province Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of SciencesDepartment of Chemistry and Biochemistry & Oeschger Centre for Climate Change Research, University of BernState Key Laboratory of Organic Geochemistry and Guangdong province Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of SciencesInstitute for Environmental and Climate Research, Jinan UniversityDepartment of Chemistry and Biochemistry & Oeschger Centre for Climate Change Research, University of BernYale-NUIST Center on Atmospheric Environment, International Joint Laboratory on Climate and Environment Change (ILCEC), Nanjing University of Information Science and TechnologyKey Laboratory of Coastal Environmental Processes and Ecological Remediation, Yantai Institute of Coastal Zone Research, Chinese Academy of SciencesState Key Laboratory of Pollution Control and Resources Reuse, Key Laboratory of Cities’ Mitigation and Adaptation to Climate Change, College of Environmental Science and Engineering, Tongji UniversityState Key Laboratory of Organic Geochemistry and Guangdong province Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of SciencesState Key Laboratory of Organic Geochemistry and Guangdong province Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of SciencesInstitute of Surface-Earth System Science, Tianjin UniversityState Key Laboratory of Organic Geochemistry and Guangdong province Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of SciencesAbstract We measured the radiocarbon isotope signals in various fractions of carbonaceous aerosols sampled across four seasons (Oct 2013−Jul 2014) in three megacities of China, viz., Beijing, Shanghai, and Guangzhou. The contributions of fossil fuel (FF) and non-fossil fuel (NF) to the carbonaceous aerosol were estimated based on the radiocarbon content in the organic carbon (OC), water-soluble organic carbon (WSOC), water-insoluble organic carbon (WIOC), and elemental carbon (EC). Although NF generated the primary share (> 55%) during autumn in all of the cities, the seasonal contributions of the sources differed by location during the rest of the year. During winter, FF emissions constituted the majority of the carbonaceous pollution (64%) in Beijing, probably as a result of increased coal combustion for heating. On average, the EC, WSOC, and WIOC generated by FF composed ~10%, 35%, and 19% of the total carbon (TC). Overall, NF was identified as the largest source of carbonaceous aerosol in Guangzhou (63%), whereas FF was the largest source, contributing slightly more than NF, in Shanghai (54%). During spring and summer, FF played a greater role than NF in Beijing (~55%) and Guangzhou (~63%); additionally, based on our limited number of samples, it contributed 71% in Shanghai during the latter season, with a significant portion due to fuel combustion (i.e., industrial, vehicular, fishing-boat, and large-vessel emissions).https://doi.org/10.4209/aaqr.2019.12.0642Carbonaceous aerosolFine aerosolSource apportionment
spellingShingle Di Liu
Matthias Vonwiller
Jun Li
Junwen Liu
Sönke Szidat
Yanlin Zhang
Chongguo Tian
Yinjun Chen
Zhineng Cheng
Guangcai Zhong
Pingqing Fu
Gan Zhang
Fossil and Non-fossil Fuel Sources of Organic and Elemental Carbonaceous Aerosol in Beijing, Shanghai, and Guangzhou: Seasonal Carbon Source Variation
Aerosol and Air Quality Research
Carbonaceous aerosol
Fine aerosol
Source apportionment
title Fossil and Non-fossil Fuel Sources of Organic and Elemental Carbonaceous Aerosol in Beijing, Shanghai, and Guangzhou: Seasonal Carbon Source Variation
title_full Fossil and Non-fossil Fuel Sources of Organic and Elemental Carbonaceous Aerosol in Beijing, Shanghai, and Guangzhou: Seasonal Carbon Source Variation
title_fullStr Fossil and Non-fossil Fuel Sources of Organic and Elemental Carbonaceous Aerosol in Beijing, Shanghai, and Guangzhou: Seasonal Carbon Source Variation
title_full_unstemmed Fossil and Non-fossil Fuel Sources of Organic and Elemental Carbonaceous Aerosol in Beijing, Shanghai, and Guangzhou: Seasonal Carbon Source Variation
title_short Fossil and Non-fossil Fuel Sources of Organic and Elemental Carbonaceous Aerosol in Beijing, Shanghai, and Guangzhou: Seasonal Carbon Source Variation
title_sort fossil and non fossil fuel sources of organic and elemental carbonaceous aerosol in beijing shanghai and guangzhou seasonal carbon source variation
topic Carbonaceous aerosol
Fine aerosol
Source apportionment
url https://doi.org/10.4209/aaqr.2019.12.0642
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