Effect of ambient humidity on the light absorption amplification of black carbon in Beijing during January 2013

被引:64
|
作者
Wu, Yunfei [1 ]
Zhang, Renjian [1 ,2 ]
Tian, Ping [1 ]
Tao, Jun [3 ]
Hsu, S-C [4 ]
Yan, Peng [5 ]
Wang, Qiyuan [6 ]
Cao, Junji [6 ]
Zhang, Xiaoling [7 ]
Xia, Xiangao [8 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, RCE TEA, Beijing 100029, Peoples R China
[2] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing 210044, Jiangsu, Peoples R China
[3] Minist Environm Protect, South China Inst Environm Sci, Guangzhou 510655, Guangdong, Peoples R China
[4] Acad Sinica, Res Ctr Environm Changes, Taipei 115, Taiwan
[5] Meteorol Observat Ctr CMA, CAWAS, Beijing 100081, Peoples R China
[6] Chinese Acad Sci, Inst Earth Environm, Key Lab Aerosol, SKLLQG, Xian 710075, Peoples R China
[7] Chinese Meteorol Adm, Inst Urban Meteorol, Beijing 100089, Peoples R China
[8] Chinese Acad Sci, Inst Atmospher Phys, LAGEO, Beijing 100029, Peoples R China
基金
中国国家自然科学基金;
关键词
Haze; Black carbon; Light absorption; Ambient humidity; PARTICLE SOOT PHOTOMETER; YANGTZE-RIVER DELTA; MIXING STATE; OPTICAL-PROPERTIES; AEROSOL CHARACTERIZATION; EVOLUTION PROCESSES; CHINA IMPLICATIONS; AIR-POLLUTION; WINTER HAZE; GUANGZHOU;
D O I
10.1016/j.atmosenv.2015.04.041
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Black carbon (BC) and its mixing state were measured with a ground-based single particle soot photometer in urban Beijing during the extremely polluted winter of w2013. Up to 70 +/- 14% of the BC-containing particles were thickly-coated during periods of haze, compared to 37 +/- 9% on non-hazy days. The thickly-coated number fraction (NFBC-thick) increased with increasing BC, reaching a plateau at similar to 80-90% when BC concentrations were >= 15 mu g m(-3) and visibility was <= 2 km. Regional inflows brought more aged, highly thickly-coated BC to Beijing during haze. The absorption coefficient showed a distinct linear correlation with BC concentration; the mass absorption efficiency (MAE) of BC was acquired, with an overall mean of 4.2 +/- 0.01 m(2) g(-1) at 870 nm. The MAE of BC amplified with increasing ambient relative humidity. This was largely explained by the increase in NFBC-thick, which was likely due to the enhanced production of secondary aerosol under humid conditions. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:217 / 223
页数:7
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