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北京大气中NO、NO2和O3浓度变化的相关性分析
引用本文:安俊琳,王跃思,李昕,孙扬,申双和,石立庆.北京大气中NO、NO2和O3浓度变化的相关性分析[J].环境科学,2007,28(4):706-711.
作者姓名:安俊琳  王跃思  李昕  孙扬  申双和  石立庆
作者单位:南京信息工程大学应用气象学系,南京210044;中国科学院大气物理研究所,北京100029;中国科学院大气物理研究所,北京100029;中国科学院大气物理研究所,北京100029;南京信息工程大学应用气象学系,南京210044;中国科学院大气物理研究所,北京100029
基金项目:国家自然科学基金项目(40222202)
摘    要:臭氧(O3)是城市污染大气中的首要光化学污染物,其变化规律与氮氧化物(NOx=NO+NO2)关系密切.采用49C臭氧分析仪和42CTL氮氧化物分析仪对北京城区O3和NOx浓度进行了连续观测,时间为2004-08~2005-07.结果显示,O3和OX(O3+NO2)浓度在午后15:00左右出现峰值,NOx呈双峰态日变化,在07:00和23:00左右出现峰值.不同季节污染物的浓度变化存在差异,O3和NOx浓度分别在夏季和冬季达到最大.NOx浓度存在100×10-9(体积分数)的“分界点”,NOx低浓度时以NO2为主,NOx高浓度时NO占大部分.OX区域贡献和局地贡献存在明显的季节变化,前者主要受区域背景O3的影响,在春季最大,后者主要受局地NOx光化学反应的制约,在夏季最强,同时OX组分呈现显著的昼夜差异.

关 键 词:城市大气污染  光化学氧化剂  臭氧  区域贡献  局地贡献
文章编号:0250-3301(2007)04-0706-06
收稿时间:2005/11/22 0:00:00
修稿时间:2005-11-222006-10-24

Analysis of the Relationship between NO, NO2 and O3 Concentrations in Beijing
AN Jun-lin,WANG Yue-si,LI Xin,SUN Yang,SHEN Shuang-he and SHI Li-qing.Analysis of the Relationship between NO, NO2 and O3 Concentrations in Beijing[J].Chinese Journal of Environmental Science,2007,28(4):706-711.
Authors:AN Jun-lin  WANG Yue-si  LI Xin  SUN Yang  SHEN Shuang-he and SHI Li-qing
Institution:Department of Applied Meteorology, Nanjing University of Information Science & Technology, Nanjing 210044, China. junlinan@nuist.edu.cn
Abstract:Ozone (O3) is a primary gaseous contaminant in urban ambient, and its variation correlates well with nitrogen oxides (NOx=NO+NO2). Continuous monitoring in the urban area from August 2004 to July 2005 was carried out in Beijing, using 49C ozone analyzer and 42CTL NO-NO2-NOx gas analyzer. The results show that peak O3 and oxidant (OX=O3+NO2) concentrations in Beijing often appear at about 15:00 in the early afternoon, the diurnal variation of NOx concentrations show a very clear cycle with two peaks, one appears at about 07:00 in the morning and the other is at 23:00 in the evening. However, concentrations variation in four seasons are not same. The highest concentrations of O3 and NOx appear in summer and winter, respectively. The NOx crossover point occurs at about 100×10-9 volume ratio. At lower level, NO2 is the major component of NOx, whereas NO dominates at higher mixing ratio. It is also shown that the level of OX is made up of two contributions, regional contribution and local contribution. The former is affected by regional background O3 level, with the maximum in spring, whereas the latter is effectively correlates with the level of primary pollution, with the maximum in summer. Diurnal variation also appears in the concentrations of the components of oxidants.
Keywords:urban atmospheric pollution  photochemical oxidant  ozone  regional pollution  local pollution
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