Primary biogenic and anthropogenic sources of organic aerosols in Beijing, China: Insights from saccharides and n-alkanes
Creators
- 1. State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing, 100875 (China)
- 2. Institute of Surface-Earth System Science, Tianjin University, Tianjin, 300072 (China)
- 3. College of Earth Sciences, University of Chinese Academy of Sciences, Beijing, 100049 (China)
- 4. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029 (China)
- 5. Chubu Institute for Advanced Studies, Chubu University, Kasugai, 487-8501 (Japan)
- 6. Department of Civil and Environmental Engineering, Louisiana State University, Baton Rouge, LA, 70803 (United States)
Description
Highlights: • Biomass burning contributes significantly to PM2.5 during the whole year, particularly in cold seasons. • n-Alkanes mainly originate from plant waxes in spring while from fossil fuel combustion in heating season. • Dust storms in spring account for high atmospheric levels of fine organic matter. Sugars and n-alkanes are important organic constituents of atmospheric fine particulate matter (PM2.5). For better understanding their sources and seasonal variations in urban atmosphere, sugar compounds (anhydrosugars, sugars and sugar alcohols) and homologue n-alkanes (C18–C37) were studied in PM2.5 samples collected from September 2013 to July 2014 in Beijing, China. In general, all measured compounds showed the lowest levels in summer. Higher concentrations of sugar compounds and n-alkanes were observed in winter, probably due to elevated combustion emissions (e.g., coal, biofuel and agricultural residue burning) and stable meteorological conditions during heating season. Levoglucosan was the major sugar species in all seasons particularly in autumn and winter, highlighting the significant contribution of biomass burning to fine organic aerosols throughout the whole year especially in cold seasons. Plant waxes contributed to n-alkanes the most in late spring (54.5%) and the least in winter (11.6%); while fossil fuel combustion had the largest contribution in winter (385 ng m−3). The weak odd-carbon predominance of n-alkanes in wintertime aerosols also suggests fossil fuel combustion as the important source of organic aerosols in the heating season. Soil resuspension, fossil fuel combustion and biomass burning, and secondary sources are the main sources of OC in PM2.5 at Beijing. The seasonal variation in source contributions indicates that meteorological condition is a key factor in controlling PM2.5 levels. Furthermore, dust storms in spring can strongly enhance the atmospheric level of fine organic matter in Beijing.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.envpol.2018.09.118Additional details
Identifiers
- DOI
- 10.1016/j.envpol.2018.09.118;
- PII
- S0269749118324059;
Publishing Information
- Journal Title
- Environmental Pollution (1987)
- Journal Volume
- 243
- Journal Page Range
- p. 1579-1587
- ISSN
- 0269-7491
- CODEN
- ENPOEK
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 54075604
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- AEROSOLS; AGRICULTURAL WASTES; ALCOHOLS; ALKANES; BIOFUELS; BIOMASS; CARBON; CHINA; COAL; COMBUSTION; DUSTS; ECOLOGICAL CONCENTRATION; METEOROLOGY; ORGANIC MATTER; PARTICLE RESUSPENSION; PARTICULATES; SACCHAROSE; SEASONAL VARIATIONS; SEASONS; SOILS; URBAN AREAS; WAXES
- Descriptors DEC
- ALTERNATIVE FUELS; ASIA; CARBOHYDRATES; CARBONACEOUS MATERIALS; CHEMICAL REACTIONS; COLLOIDS; DISACCHARIDES; DISPERSIONS; ELEMENTS; ENERGY SOURCES; FOSSIL FUELS; FUELS; HYDROCARBONS; HYDROXY COMPOUNDS; MATERIALS; MATTER; NONMETALS; OLIGOSACCHARIDES; ORGANIC COMPOUNDS; ORGANIC WASTES; OTHER ORGANIC COMPOUNDS; OXIDATION; PARTICLES; RENEWABLE ENERGY SOURCES; SACCHARIDES; SOLS; THERMOCHEMICAL PROCESSES; VARIATIONS; WASTES
Optional Information
- Copyright
- Copyright (c) 2018 Elsevier Ltd. All rights reserved.