Title of article
Potential contribution of new particle formation to cloud condensation nuclei in Beijing
Author/Authors
Yue، نويسنده , , D.L. and Hu، نويسنده , , M. and Zhang، نويسنده , , R.Y. and Wu، نويسنده , , Z.J. and Su، نويسنده , , H. and Wang، نويسنده , , Z.B. and Peng، نويسنده , , J.F. and He، نويسنده , , L.Y. and Huang، نويسنده , , X.F. and Gong، نويسنده , , Y.G. and Wiedensohler، نويسنده , , A.، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 2011
Pages
8
From page
6070
To page
6077
Abstract
New particle formation (NPF) events have been recognized as an important process contributing to the cloud condensation nuclei (CCN) formation. In this study, measurement of NPF and predicted number concentrations of CCN using κ-Köhler theory were analyzed to assess the contribution of NPF to possible CCN. The particle growth rates of NPF events were categorized to two types: sulfur-rich (condensation and neutralization of sulfuric acid dominating net growth rate) and sulfur-poor cases. The growth rates for the sulfur-poor events were about 80% larger than those of the sulfur-rich cases on average. NPF events increased the CCN number concentrations by 0.4–6 times in the megacity area of Beijing. The enhancement ratios (the ratio of CCN number concentrations when obvious particle growth ended to that when it started during NPF events) were high for large supersaturation (S). For example, it was about 30–50% higher under S = 0.86% than under S = 0.07%. The enhancement ratios exhibited similar seasonal variation as the growth rates with a larger value in summer than other seasons, which suggested that growth rate was a key factor in the conversion of NPF to possible CCN. The enhancement ratios were higher during the sulfur-poor NPF events with larger growth rates mainly contributed by organic species, indicating that organic species were the dominant chemical contributor in facilitating the conversion of newly formed particles to possible CCN in the Beijing Megacity.
Keywords
cloud condensation nuclei , Number concentration , new particle formation , particle growth
Journal title
Atmospheric Environment
Serial Year
2011
Journal title
Atmospheric Environment
Record number
2238168
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