Measurements of peroxy radicals in a forested area of Portugal

J. Burkert , T. Behmann , M.D. Andrés Hernández , D. Stöbener , M. Weißenmayer , D. Perner , J.P. Burrows
{"title":"Measurements of peroxy radicals in a forested area of Portugal","authors":"J. Burkert ,&nbsp;T. Behmann ,&nbsp;M.D. Andrés Hernández ,&nbsp;D. Stöbener ,&nbsp;M. Weißenmayer ,&nbsp;D. Perner ,&nbsp;J.P. Burrows","doi":"10.1016/S1465-9972(01)00014-9","DOIUrl":null,"url":null,"abstract":"<div><p>As part of the FIELDVOC'94 study, ambient concentrations of peroxy radicals (RO<sub>2</sub>, R=H, CH<sub>3</sub>, CH<sub>3</sub>CO, etc.) were continuously measured at a forested site in Portugal, using the chemical amplification technique. The amount of RO<sub>2</sub> varied between 0 and 260 pptv with maximum values being obtained under clear sky conditions. The RO<sub>2</sub> mixing ratio correlates with that of isoprene. The rate of production of ozone, O<sub>3</sub>, indicates that the noon-time maximum values lay between 5 and 17 ppbv h<sup>−1</sup>. On several days, the maximum O<sub>3</sub> mixing ratio at this rural site was similar to that found in urban areas, which experience smog episodes (O<sub>3</sub> mixing ratio<!--> <!-->&gt;<!--> <!-->90 ppbv). The RO<sub>2</sub> estimated assuming a photostationary state RO<sub>2</sub>,(PSS) of NO<sub>2</sub>, NO and O<sub>3</sub>, was not found to have a significant statistical correlation with the measured RO<sub>2</sub>. The latter is best explained by the errors associated with the calculation of RO<sub>2</sub>,(PSS) at low NO<sub><em>x</em></sub> (NO<!--> <!-->+<!--> <!-->NO<sub>2</sub>) mixing ratios. The diurnal behavior of O<sub>3</sub> in the boundary layer was estimated using a relatively simple source/sink parameterization. On days having high O<sub>3</sub> mixing ratios, both predicted and observed O<sub>3</sub> behavior agree well. For days having O<sub>3</sub> mixing ratios<!--> <!-->&lt;<!--> <!-->75 ppbv, it was found that the simple parameterization needed to be extended to include entrainment of O<sub>3</sub> after dawn from above the night-time inversion layer.</p></div>","PeriodicalId":100235,"journal":{"name":"Chemosphere - Global Change Science","volume":"3 3","pages":"Pages 327-338"},"PeriodicalIF":0.0000,"publicationDate":"2001-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1465-9972(01)00014-9","citationCount":"27","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemosphere - Global Change Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1465997201000149","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 27

Abstract

As part of the FIELDVOC'94 study, ambient concentrations of peroxy radicals (RO2, R=H, CH3, CH3CO, etc.) were continuously measured at a forested site in Portugal, using the chemical amplification technique. The amount of RO2 varied between 0 and 260 pptv with maximum values being obtained under clear sky conditions. The RO2 mixing ratio correlates with that of isoprene. The rate of production of ozone, O3, indicates that the noon-time maximum values lay between 5 and 17 ppbv h−1. On several days, the maximum O3 mixing ratio at this rural site was similar to that found in urban areas, which experience smog episodes (O3 mixing ratio > 90 ppbv). The RO2 estimated assuming a photostationary state RO2,(PSS) of NO2, NO and O3, was not found to have a significant statistical correlation with the measured RO2. The latter is best explained by the errors associated with the calculation of RO2,(PSS) at low NOx (NO + NO2) mixing ratios. The diurnal behavior of O3 in the boundary layer was estimated using a relatively simple source/sink parameterization. On days having high O3 mixing ratios, both predicted and observed O3 behavior agree well. For days having O3 mixing ratios < 75 ppbv, it was found that the simple parameterization needed to be extended to include entrainment of O3 after dawn from above the night-time inversion layer.

查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
葡萄牙森林地区过氧自由基的测量
作为FIELDVOC'94研究的一部分,使用化学扩增技术在葡萄牙的一个森林站点连续测量了环境过氧化自由基(RO2, R=H, CH3, CH3CO等)的浓度。RO2的量在0至260 pptv之间变化,在晴空条件下达到最大值。RO2的混合比与异戊二烯的混合比相关。臭氧(O3)的生成速率表明,午时最大值在5 ~ 17 ppbv h−1之间。有几天,该农村站点的最大O3混合比与经历雾霾事件的城市地区相似(O3混合比>90 ppbv)。在光稳定状态下估算的RO2, NO2, NO和O3的RO2 (PSS)与测量的RO2没有显著的统计相关性。后者最好的解释是在低NOx (NO + NO2)混合比下计算RO2 (PSS)的误差。使用相对简单的源/汇参数化估算了边界层中O3的日变化。在高O3混合比的日子里,预测和观测到的O3行为吻合得很好。有O3混合比<的天数;75 ppbv,发现需要扩展简单的参数化,以包括黎明后从夜间逆温层上方夹带的O3。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
Methane production and theoretical consumption in UK livestock production: is a realistic balance possible? Carbon sink in cropland soils and the emission of greenhouse gases from paddy soils: a review of work in China Modeling the biogeochemical cycle of dimethylsulfide in the upper ocean: a review On the performance of SF6 permeation tubes used in determining methane emission from grazing livestock An analysis of simulated and observed global mean near-surface air temperature anomalies from 1979 to 1999: trends and attribution of causes
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1