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泰山春季臭氧污染特征
引用本文:边 智,李 杰,王喜全,POCHANART Pakpong,王自发.泰山春季臭氧污染特征[J].环境科学研究,2006,19(5):36-39.
作者姓名:边 智  李 杰  王喜全  POCHANART Pakpong  王自发
作者单位:1.山东省泰山气象站,山东,泰安,271000
基金项目:国家自然科学基金 , 中国科学院"百人计划"
摘    要:采用紫外光度法,使用美国热电子公司的TECO model49c型紫外吸收式臭氧分析仪,对2004年5月泰山站的地面臭氧进行监测,以获得更具华北区域代表性的臭氧春季污染特征.结果表明:2004年5月泰山站ψ(O3)的月均值为64μL/m3,变化幅度达到53 μL/m3;其频率分布呈单峰性,主要集中于55~75μL/m3,与济南站的分散型和区域背景站Cape D'Aguilar的双峰型分布有明显的不同;泰山ψ(O3)有明显的日变化特征,变化幅度(19 μL/m3)远大于中国西部的瓦里关站,这可能与泰山处于中国东部,尽管距地面较高,但不可避免地受到区域性的污染有关. 

关 键 词:臭氧小时体积分数    频率分布    日变化
文章编号:1001-6929(2006)05-0036-04
收稿时间:2006-01-02
修稿时间:2006-01-02

The Characters of Variation of Ozone at Taishan in Spring
BIAN Zhi,LI Jie,WANG Xi-quan,POCHANART Pakpong and WANG Zi-fa.The Characters of Variation of Ozone at Taishan in Spring[J].Research of Environmental Sciences,2006,19(5):36-39.
Authors:BIAN Zhi  LI Jie  WANG Xi-quan  POCHANART Pakpong and WANG Zi-fa
Institution:1.Taishan Meteorological Station,The Meteorology Bureau of Taishan,Taian 271000,China2.Nansen_Zhukezhen International Research Center,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China3.Frontier Research System for Global Change,Kanagawa 2360001,Japan
Abstract:In order to obtain regional variation of ozone in North China in spring,the surface ozone was monitored at Mount Tai during May,2004,adopting UV photometry with TECO model49c-type UV absorption ozone analyzer manufactured by US Thermo Electron Corporation.The results show that Monthly ozone concentration is 64 μL/m3,with a variation of 53 μL/m3.The frequency distribution of hourly ozone concentration is one-peak,mainly in 55~75 μL/m3,obviously different from the dispersed pattern in Jinan and the two-peak pattern in Cape D’Aguilar station,the regional background station.The ozone concentration has an obviously diurnal variation,with a variation of 19 μL/m3,which is bigger than Waliguan,a background station in the west of China.This is partly explained by the regional pollution in the east of China. 
Keywords:hourly ozone concentration  frequency distribution  diurnal variation
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