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首页> 外文期刊>Advances in Meteorology >Estimation of Daytime NO3Radical Levels in the UK Urban Atmosphere Using the Steady State Approximation Method
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Estimation of Daytime NO3Radical Levels in the UK Urban Atmosphere Using the Steady State Approximation Method

机译:使用稳态近似法估算英国城市大气中的白天NO3辐射水平

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The steady state approximation has been applied to the UK National Environment Technology Centre (NETCEN) data at three urban sites in the UK (Marylebone Road London, London Eltham, and Harwell) over the period of 1997 to 2012 to estimate the concentrations of daytime NO3. Despite the common assertion that NO3levels are negligible in the day as a consequence of photolysis, there are occasions where NO3reaches a few pptv. A seasonal pattern in NO3concentration was observed with higher levels in the spring with consistent peaks in April and May. A combination of temperature effects (the formation of NO3from the reaction of NO2with O3has a high activation energy barrier), a distinct pattern in O3concentration (peaking in spring), and loss via reaction with NO peaking in winter is responsible for this trend. Although reaction with OH is still the dominant loss process for VOCs during the day, there are VOCs (unsaturated) that will have an appreciable loss due to reaction with NO3in the daytime. Since the addition reaction of NO3with alkenes can lead directly to organic nitrate formation, there are implications for O3formation and secondary organic aerosol formation during daytime and these are discussed.
机译:在1997年至2012年期间,稳态近似值已应用于英国三个城市站点(伦敦马里波恩路,伦敦埃尔特姆和哈维尔)的英国国家环境技术中心(NETCEN)数据,以估算白天NO3的浓度。尽管普遍认为由于光解作用,NO3的水平在一天之内可以忽略不计,但在某些情况下,NO3达到了几个pptv。春季观察到了NO3浓度的季节性变化,其水平较高,4月和5月均达到一致的峰值。温度效应(由NO2与O3反应形成的NO3具有很高的活化能垒),O3浓度(春季峰值)的独特模式以及冬季与NO峰反应引起的损失是这种趋势的综合原因。尽管与OH的反应仍然是白天VOC的主要损失过程,但是由于白天与NO3的反应,仍有一些VOC(不饱和的)损失相当大。由于NO3与烯烃的加成反应可直接导致有机硝酸盐的形成,因此白天会产生O3的形成和二次有机气溶胶的形成,并进行了讨论。

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