Characterization of new particle and secondary aerosol formation during summertime in Beijing, China

被引:66
|
作者
Zhang, Y. M. [1 ,2 ]
Zhang, X. Y. [1 ]
Sun, J. Y. [1 ]
Lin, W. L. [1 ]
Gong, S. L. [3 ]
Shen, X. J. [1 ]
Yang, S. [4 ]
机构
[1] China Meteorol Adm, Chinese Acad Meteorol Sci, Ctr Atmosphere Watch & Serv, Key Lab Atmospher Chem, Beijing 100081, Peoples R China
[2] Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
[3] Environm Canada, Sci & Technol Branch, Air Qual Res Div, Toronto, ON M3H 5T4, Canada
[4] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
来源
基金
中国国家自然科学基金;
关键词
NUCLEATION MODE PARTICLES; POSITIVE MATRIX FACTORIZATION; OXYGENATED ORGANIC AEROSOLS; MASS-SPECTROMETER; SIZE DISTRIBUTION; HYDROCARBON-LIKE; MEGA-CITY; GROWTH; RATES; PITTSBURGH;
D O I
10.1111/j.1600-0889.2011.00533.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Size-resolved aerosol number and mass concentrations and the mixing ratios of O-3 and various trace gases were continuously measured at an urban station before and during the Beijing Olympic and Paralympic Games (5 June to 22 September, 2008). 23 new particle formation (NPF) events were identified; these usually were associated with changes in wind direction and/or rising concentrations of gas-phase precursors or after precipitation events. Most of the NPF events started in the morning and continued to noon as particles in the nucleation mode grew into the Aitken mode. From noon to midnight, the aerosols grew into the accumulation mode through condensation and coagulation. Ozone showed a gradual rise starting around 10:00 local time, reached its peak around 15:00 and then declined as the organics increased. The dominant new particle species were organics (40-75% of PM1) and sulphate; nitrate and ammonium were more minor contributors.
引用
收藏
页码:382 / 394
页数:13
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