Inorganic markers, carbonaceous components and stable carbon isotope from biomass burning aerosols in Northeast China

被引:69
|
作者
Cao, Fang [1 ,2 ]
Zhang, Shi-Chun [3 ]
Kawamura, Kimitaka [2 ]
Zhang, Yan-Lin [1 ,2 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Yale NUIST Ctr Atmospher Environm, Nanjing 10044, Jiangsu, Peoples R China
[2] Hokkaido Univ, Inst Low Temp Sci, Kita Ku, N19 W08, Sapporo, Hokkaido 0600819, Japan
[3] Chinese Acad Sci, Northeast Inst Geog & Agroecol, 4888 Shengbei Rd, Changchun 130102, Peoples R China
关键词
Aerosol; Biomass burning; Stable carbon isotope; Source; Potassium; SOUTH CHINA; ATMOSPHERIC AEROSOLS; KETOCARBOXYLIC ACIDS; DICARBOXYLIC-ACIDS; ALPHA-DICARBONYLS; ORGANIC AEROSOLS; BACKGROUND SITE; RIVER DELTA; PARTICLES; EMISSIONS;
D O I
10.1016/j.scitotenv.2015.09.099
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
To better characterize the chemical compositions and sources of fine particulate matter (i.e. PM2.5) in Sanjiang Plain, Northeast China, total carbon (TC), organic carbon (OC), elemental carbon (EC), water-soluble organic carbon( WSOC), and inorganic ions as well as stable carbon isotopic composition (delta C-13) were measured in this study. Intensively open biomass burning episodes are identified from late September to early October by satellite fire and aerosol optical depth maps. During the biomass-burning episode, concentrations of PM2.5, OC, EC, and WSOC are increased by a factor of 4-12 compared to those during the non-biomass-burning period. Non-sea-salt potassium is strongly correlated with PM2.5, OC, EC and WSOC, demonstrating an important contribution from biomass-burning emissions. The enrichment in both the non-sea-salt potassium and chlorine is significantly larger than other inorganic species, suggesting that biomass-burning aerosols in Sanjiang Plain are mostly fresh and less aged. In addition, the WSOC-to-OC ratio is lower than that reported in biomass-burning aerosols in tropical regions, further supporting that biomass-burning aerosols in Sanjiang Plain are mostly primary and secondary organic aerosols may be not significant. A lower average delta C-13 value (-26.2 parts per thousand) is observed during the biomass-burning period, indicating a dominant contribution from combustion of C3 plants in the studied region. (C) 2015 Elsevier B. V. All rights reserved.
引用
收藏
页码:1244 / 1251
页数:8
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