Impacts of springtime biomass burning in the northern Southeast Asia on marine organic aerosols over the Gulf of Tonkin, China
- 1. LAPC, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 (China)
- 2. School of Environment and Energy, South China University of Technology, Guangzhou 510006 (China)
- 3. State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012 (China)
- 4. College of Earth Sciences, University of Chinese Academy of Sciences, Beijing 100049 (China)
Description
Highlights: • Primary and secondary organic tracers were quantified in marine aerosols over the Gulf of Tonkin. • Levoglucosan was the dominant organic species in the fine aerosols. • Different sources and composition of organic aerosols were observed during different biomass-burning episodes. Fine particles (PM2.5) samples, collected at Weizhou Island over the Gulf of Tonkin on a daytime and nighttime basis in the spring of 2015, were analyzed for primary and secondary organic tracers, together with organic carbon (OC), elemental carbon (EC), and stable carbon isotopic composition (δ13C) of total carbon (TC). Five organic compound classes, including saccharides, lignin/resin products, fatty acids, biogenic SOA tracers and phthalic acids, were quantified by gas chromatography/mass spectrometry (GC/MS). Levoglucosan was the most abundant organic species, indicating that the sampling site was under strong influence of biomass burning. Based on the tracer-based methods, the biomass-burning-derived fraction was estimated to be the dominant contributor to aerosol OC, accounting for 15.7% ± 11.1% and 22.2% ± 17.4% of OC in daytime and nighttime samples, respectively. In two episodes E1 and E2, organic aerosols characterized by elevated concentrations of levoglucosan as well as its isomers, sugar compounds, lignin products, high molecular weight (HMW) fatty acids and β-caryophyllinic acid, were attributed to the influence of intensive biomass burning in the northern Southeast Asia (SEA). However, the discrepancies in the ratios of levoglucosan to mannosan (L/M) and OC (L/OC) as well as the δ13C values suggest the type of biomass burning and the sources of organic aerosols in E1 and E2 were different. Hardwood and/or C4 plants were the major burning materials in E1, while burning of softwood and/or C3 plants played important role in E2. Furthermore, more complex sources and enhanced secondary contribution were found to play a part in organic aerosols in E2. This study highlights the significant influence of springtime biomass burning in the northern SEA to the organic molecular compositions of marine aerosols over the Gulf of Tonkin.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.envpol.2018.01.089Additional details
Identifiers
- DOI
- 10.1016/j.envpol.2018.01.089;
- PII
- S0269749117346912;
Publishing Information
- Journal Title
- Environmental Pollution (1987)
- Journal Volume
- 237
- Journal Page Range
- p. 285-297
- ISSN
- 0269-7491
- CODEN
- ENPOEK
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 54068768
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- AEROSOLS; BIOMASS; CARBON; CARBON 13; CHINA; ECOLOGICAL CONCENTRATION; FINE PARTICLES; GAS CHROMATOGRAPHY; ISLANDS; ISOMERS; ISOTOPE RATIO; LIGNIN; MASS SPECTROSCOPY; MOLECULAR WEIGHT; PHTHALIC ACID; PLANTS; RESINS; SACCHAROSE; SAMPLING; SEAS
- Descriptors DEC
- ASIA; CARBOHYDRATES; CARBON ISOTOPES; CARBOXYLIC ACIDS; CHROMATOGRAPHY; COLLOIDS; DICARBOXYLIC ACIDS; DIMENSIONLESS NUMBERS; DISACCHARIDES; DISPERSIONS; ELEMENTS; ENERGY SOURCES; EVEN-ODD NUCLEI; ISOTOPES; LIGHT NUCLEI; NONMETALS; NUCLEI; OLIGOSACCHARIDES; ORGANIC ACIDS; ORGANIC COMPOUNDS; ORGANIC POLYMERS; PARTICLES; PETROCHEMICALS; PETROLEUM PRODUCTS; POLYMERS; POLYSACCHARIDES; RENEWABLE ENERGY SOURCES; SACCHARIDES; SEPARATION PROCESSES; SOLS; SPECTROSCOPY; STABLE ISOTOPES; SURFACE WATERS
Optional Information
- Copyright
- Copyright (c) 2018 Elsevier Ltd. All rights reserved.