GSTDTAP  > 地球科学
DOI10.5194/acp-17-12659-2017
A new balance formula to estimate new particle formation rate: reevaluating the effect of coagulation scavenging
Cai, Runlong; Jiang, Jingkun
2017-10-25
发表期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
ISSN1680-7316
EISSN1680-7324
出版年2017
卷号17期号:20
文章类型Article
语种英语
国家Peoples R China
英文摘要

A new balance formula to estimate new particle formation rate is proposed. It is derived from the aerosol general dynamic equation in the discrete form and then converted into an approximately continuous form for analyzing data from new particle formation (NPF) field campaigns. The new formula corrects the underestimation of the coagulation scavenging effect that occurred in the previously used formulae. It also clarifies the criteria for determining the upper size bound in measured aerosol size distributions for estimating new particle formation rate. An NPF field campaign was carried out from 7 March to 7 April 2016 in urban Beijing, and a diethylene glycol scanning mobility particle spectrometer equipped with a miniature cylindrical differential mobility analyzer was used to measure aerosol size distributions down to similar to 1 nm. Eleven typical NPF events were observed during this period. Measured aerosol size distributions from 1 nm to 10 mu m were used to test the new formula and the formulae widely used in the literature. The previously used formulae that perform well in a relatively clean atmosphere in which nucleation intensity is not strong were found to underestimate the comparatively high new particle formation rate in urban Beijing because of their underestimation or neglect of the coagulation scavenging effect. The coagulation sink term is the governing component of the estimated formation rate in the observed NPF events in Beijing, and coagulation among newly formed particles contributes a large fraction to the coagulation sink term. Previously reported formation rates in Beijing and in other locations with intense NPF events might be underestimated because the coagulation scavenging effect was not fully considered; e.g., estimated formation rates of 1.5 nm particles in this campaign using the new formula are 1.3-4.3 times those estimated using the formula neglecting coagulation among particles in the nucleation mode.


领域地球科学
收录类别SCI-E
WOS记录号WOS:000413669000002
WOS关键词AEROSOL-SIZE DISTRIBUTIONS ; DIFFERENTIAL MOBILITY ANALYZER ; NUCLEATION MODE PARTICLES ; ATMOSPHERIC SULFURIC-ACID ; NORTH CHINA PLAIN ; GROWTH-RATES ; BOUNDARY-LAYER ; MU-M ; 3 NM ; MECHANISMS
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/26145
专题地球科学
作者单位Tsinghua Univ, State Key Joint Lab Environm Simulat & Pollut Con, Sch Environm, Beijing 100084, Peoples R China
推荐引用方式
GB/T 7714
Cai, Runlong,Jiang, Jingkun. A new balance formula to estimate new particle formation rate: reevaluating the effect of coagulation scavenging[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2017,17(20).
APA Cai, Runlong,&Jiang, Jingkun.(2017).A new balance formula to estimate new particle formation rate: reevaluating the effect of coagulation scavenging.ATMOSPHERIC CHEMISTRY AND PHYSICS,17(20).
MLA Cai, Runlong,et al."A new balance formula to estimate new particle formation rate: reevaluating the effect of coagulation scavenging".ATMOSPHERIC CHEMISTRY AND PHYSICS 17.20(2017).
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