首页  |  本刊简介  |  编委会  |  投稿须知  |  订阅与联系  |  微信  |  出版道德声明  |  Ei收录本刊数据  |  封面
北京夏季高温高湿和降水过程对大气颗粒物谱分布的影响
摘要点击 3726  全文点击 1656    
查看HTML全文 查看全文  查看/发表评论  下载PDF阅读器
中文关键词  颗粒物  质量浓度谱分布  数浓度谱分布  高温高湿  降雨
英文关键词  particle  mass size distribution  number size distribution  high temperature, high relative humidity  rainfall
作者单位
胡敏 北京大学环境学院 环境模拟与污染控制国家联合重点实验室北京 100871 
刘尚 北京大学环境学院 环境模拟与污染控制国家联合重点实验室北京 100871 
吴志军 北京大学环境学院 环境模拟与污染控制国家联合重点实验室北京 100871 
张静 北京大学环境学院 环境模拟与污染控制国家联合重点实验室北京 100871 
赵云良 北京大学环境学院 环境模拟与污染控制国家联合重点实验室北京 100871 
Birgit Wehner 德国莱比锡对流层研究所莱比锡 04318 
Alfred Wiedensohler 德国莱比锡对流层研究所莱比锡 04318 
中文摘要
      2004-07-13~2004-08-23使用TDMPS-APS系统在线测量颗粒物的数浓度谱分布,并于07-16~07-18选取了高温闷热夜晚、日间高温高湿和雨后晴朗干洁3种天气条件,使用多级串联撞击式采样器(MOUDI)测量颗粒物的质量浓度谱分布,结果表明:高温高湿天气条件下颗粒物的污染、尤其细粒子污染严重,导致很低的能见度(2.5km);PM1.8和PM10的质量浓度分别为170.68μg/m3和249.35μg/m3,细粒子质量浓度占PM10的68%;粒径为50~100nm颗粒物的数浓度最高,为2×104~3×104个/cm3;降雨过程对粗粒子和细粒子均有去除作用,对细粒子的去除作用尤为明显;降雨后PM10和PM1.8浓度分别比降雨前降低3倍和6倍;降雨过后的晴朗干洁天气有利于新粒子(3~20nm)的生成,生成的新粒子快速长大到50~100nm;随着污染物的累积,以后几天内又变为污染天气。
英文摘要
      On-line measurements of particle number size distribution were conducted during 2004-07-13~2004-08-23 by using TDMPS-APS system in Beijing; in between the size distributions of particle mass and chemical compositions were measured by using MOUDI cascade impactor under three kinds of weather conditions: ① high temperature and high relative humidity night, ② high temperature and high relative humidity day, and ③ clear days. The results indicate that particulate matter, especially fine particle pollution becomes severe under high temperature and high relative humidity conditions, which results in low visibility (2.5km); the average concentrations of PM1.8 and PM10 are 170.68μg/m3 and 249.35μg/m3, respectively, PM1.8 accounts for 68% of PM10; number concentration mainly concentrates in the range of 50~100nm, about 2×104~3×104cm-3; rain process has a great effect on scavenging particles, especially fine particles. After the rain process PM10 is 3 times lower and PM1.8 is 6 times lower than the values before the rain; in the following clear day, new particle formation is observed, the newly formed particles (3~20nm) grow to 50~100nm rapidly. After that, the pollutants start to accumulate and it becomes heavy polluted in few days.

您是第54242057位访客
主办单位:中国科学院生态环境研究中心 单位地址:北京市海淀区双清路18号
电话:010-62941102 邮编:100085 E-mail: hjkx@rcees.ac.cn
本系统由北京勤云科技发展有限公司设计  京ICP备05002858号-2