Evolution of particle number size distribution in an urban atmosphere during episodes of heavy pollution and new particle formation
This study discusses the evolution of particle number size distribution during episodes of heavy pollution and new particle formation in the urban atmosphere of Beijing to quantify the effects of dynamic processes (coagulation and condensation) on the particle number size distribution. During a heav...
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description | This study discusses the evolution of particle number size distribution during episodes of heavy pollution and new particle formation in the urban atmosphere of Beijing to quantify the effects of dynamic processes (coagulation and condensation) on the particle number size distribution. During a heavy-pollution event, an extremely low number concentration of 3-10 nm particles (on average 46 cm-3) was observed. This is because nucleation-mode particles were easily removed by strong coagulational scavenging of larger particles under this condition. In addition, a large condensation sink (on average 0.13 s-1) restrained nucleation, which is one of the major sources of nucleation-mode particles. Conversely, during a new-particle formation event, the small condensation sink (0.01 s-1) of precursor facilitated nucleation. At the same time, preexisting particles had little ability to scavenge newly formed particles (around 1 nm) and allowed them to grow to a detectable size (larger than 3 nm currently). We suggest that the effects of dynamic processes (coagulation and condensation) on particle size distribution should be stressed under some extreme conditions of the relatively polluted urban atmosphere in addition to traffic and meteorological factors. |
doi_str_mv | 10.1007/s11430-011-4227-9 |
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During a heavy-pollution event, an extremely low number concentration of 3-10 nm particles (on average 46 cm-3) was observed. This is because nucleation-mode particles were easily removed by strong coagulational scavenging of larger particles under this condition. In addition, a large condensation sink (on average 0.13 s-1) restrained nucleation, which is one of the major sources of nucleation-mode particles. Conversely, during a new-particle formation event, the small condensation sink (0.01 s-1) of precursor facilitated nucleation. At the same time, preexisting particles had little ability to scavenge newly formed particles (around 1 nm) and allowed them to grow to a detectable size (larger than 3 nm currently). We suggest that the effects of dynamic processes (coagulation and condensation) on particle size distribution should be stressed under some extreme conditions of the relatively polluted urban atmosphere in addition to traffic and meteorological factors.</description><identifier>ISSN: 1674-7313</identifier><identifier>EISSN: 1869-1897</identifier><identifier>DOI: 10.1007/s11430-011-4227-9</identifier><language>eng</language><publisher>Heidelberg: SP Science China Press</publisher><subject>Air pollution ; Atmosphere ; Atoms & subatomic particles ; Coagulation ; Condensing ; Dynamics ; Earth and Environmental Science ; Earth Sciences ; Evolution ; Evolutionary biology ; Nucleation ; Particle size distribution ; Pollution ; Pollution abatement ; Research Paper ; Urban areas ; Urban atmosphere ; 分布动态 ; 城市大气污染 ; 大小分布 ; 气氛 ; 演变 ; 粒子数分布 ; 粒子数浓度 ; 粒度分布</subject><ispartof>Science China. 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Earth sciences</title><addtitle>Sci. China Earth Sci</addtitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><description>This study discusses the evolution of particle number size distribution during episodes of heavy pollution and new particle formation in the urban atmosphere of Beijing to quantify the effects of dynamic processes (coagulation and condensation) on the particle number size distribution. During a heavy-pollution event, an extremely low number concentration of 3-10 nm particles (on average 46 cm-3) was observed. This is because nucleation-mode particles were easily removed by strong coagulational scavenging of larger particles under this condition. In addition, a large condensation sink (on average 0.13 s-1) restrained nucleation, which is one of the major sources of nucleation-mode particles. Conversely, during a new-particle formation event, the small condensation sink (0.01 s-1) of precursor facilitated nucleation. At the same time, preexisting particles had little ability to scavenge newly formed particles (around 1 nm) and allowed them to grow to a detectable size (larger than 3 nm currently). We suggest that the effects of dynamic processes (coagulation and condensation) on particle size distribution should be stressed under some extreme conditions of the relatively polluted urban atmosphere in addition to traffic and meteorological factors.</description><subject>Air pollution</subject><subject>Atmosphere</subject><subject>Atoms & subatomic particles</subject><subject>Coagulation</subject><subject>Condensing</subject><subject>Dynamics</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Evolution</subject><subject>Evolutionary biology</subject><subject>Nucleation</subject><subject>Particle size distribution</subject><subject>Pollution</subject><subject>Pollution abatement</subject><subject>Research Paper</subject><subject>Urban areas</subject><subject>Urban atmosphere</subject><subject>分布动态</subject><subject>城市大气污染</subject><subject>大小分布</subject><subject>气氛</subject><subject>演变</subject><subject>粒子数分布</subject><subject>粒子数浓度</subject><subject>粒度分布</subject><issn>1674-7313</issn><issn>1869-1897</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNqNkk9rHSEUxYfSQkKaD9Cd7abdTOpVxz_LEtI2EOgmWYtPnTzDjE50JiXd9ovXYR4JdBHiQi_c3zlX9DTNB8BngLH4WgAYxS0GaBkholVvmmOQXLUglXhbay5YKyjQo-a0lDtcF60dIo6bvxcPaVjmkCJKPZpMnoMdPIrLuPMZlfDHIxfKnMNug0JEJqIl7-pu5jGVae9zZZYc4i3yUyjJ-bJ67b15eERTGg72JjoU_e_nGX3Ko1lb75t3vRmKPz2cJ83N94vr85_t1a8fl-ffrlrLBMxt73ouHJHWMeBEAeU7aoD0ihBJnSFGMmk773AHztLeG-I6bAUxVnaMU0lPms-b75TT_eLLrMdQrB8GE31ailaES9kphl9BUoKZAqjklxdJEJwAEVLwV6IM4_Wmn_5D79KSY30crTBWGAQjFYINsjmVkn2vpxxGkx81YL3mQm-50DUXes2FVlVDNk2Z1g_z-dn4JdHHw6B9irf3Vfc0iSpZwwUd_QdW2cZu</recordid><startdate>20111101</startdate><enddate>20111101</enddate><creator>WU 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urban atmosphere during episodes of heavy pollution and new particle formation</title><author>WU ZhiJun, HU Min YUE DingLi Birgit WEHNER Alfred WIEDENSOHLER</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c471t-fdf67d28cd41629136b3a12f92283da2a848c5ed051dc3fea2d50c72ac8546383</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Air pollution</topic><topic>Atmosphere</topic><topic>Atoms & subatomic particles</topic><topic>Coagulation</topic><topic>Condensing</topic><topic>Dynamics</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Evolution</topic><topic>Evolutionary biology</topic><topic>Nucleation</topic><topic>Particle size distribution</topic><topic>Pollution</topic><topic>Pollution abatement</topic><topic>Research Paper</topic><topic>Urban areas</topic><topic>Urban atmosphere</topic><topic>分布动态</topic><topic>城市大气污染</topic><topic>大小分布</topic><topic>气氛</topic><topic>演变</topic><topic>粒子数分布</topic><topic>粒子数浓度</topic><topic>粒度分布</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>WU ZhiJun, HU Min YUE DingLi Birgit WEHNER Alfred WIEDENSOHLER</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One 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Earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>WU ZhiJun, HU Min YUE DingLi Birgit WEHNER Alfred WIEDENSOHLER</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Evolution of particle number size distribution in an urban atmosphere during episodes of heavy pollution and new particle formation</atitle><jtitle>Science China. Earth sciences</jtitle><stitle>Sci. China Earth Sci</stitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><date>2011-11-01</date><risdate>2011</risdate><volume>54</volume><issue>11</issue><spage>1772</spage><epage>1778</epage><pages>1772-1778</pages><issn>1674-7313</issn><eissn>1869-1897</eissn><abstract>This study discusses the evolution of particle number size distribution during episodes of heavy pollution and new particle formation in the urban atmosphere of Beijing to quantify the effects of dynamic processes (coagulation and condensation) on the particle number size distribution. During a heavy-pollution event, an extremely low number concentration of 3-10 nm particles (on average 46 cm-3) was observed. This is because nucleation-mode particles were easily removed by strong coagulational scavenging of larger particles under this condition. In addition, a large condensation sink (on average 0.13 s-1) restrained nucleation, which is one of the major sources of nucleation-mode particles. Conversely, during a new-particle formation event, the small condensation sink (0.01 s-1) of precursor facilitated nucleation. At the same time, preexisting particles had little ability to scavenge newly formed particles (around 1 nm) and allowed them to grow to a detectable size (larger than 3 nm currently). We suggest that the effects of dynamic processes (coagulation and condensation) on particle size distribution should be stressed under some extreme conditions of the relatively polluted urban atmosphere in addition to traffic and meteorological factors.</abstract><cop>Heidelberg</cop><pub>SP Science China Press</pub><doi>10.1007/s11430-011-4227-9</doi><tpages>7</tpages></addata></record> |
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subjects | Air pollution Atmosphere Atoms & subatomic particles Coagulation Condensing Dynamics Earth and Environmental Science Earth Sciences Evolution Evolutionary biology Nucleation Particle size distribution Pollution Pollution abatement Research Paper Urban areas Urban atmosphere 分布动态 城市大气污染 大小分布 气氛 演变 粒子数分布 粒子数浓度 粒度分布 |
title | Evolution of particle number size distribution in an urban atmosphere during episodes of heavy pollution and new particle formation |
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