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首页> 外文期刊>Atmospheric Chemistry and Physics Discussions >Missing OH source in a suburban environment near Beijing: observed and modelled OH and HO2 concentrations in summer 2006
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Missing OH source in a suburban environment near Beijing: observed and modelled OH and HO2 concentrations in summer 2006

机译:在北京附近的郊区环境中失踪了哦来源:2006年夏天观察和建模哦和HO2浓度

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摘要

Measurements of ambient OH and HO2 radicals were performed by laser induced fluorescence (LIF) during CAREBeijing2006 (Campaigns of Air Quality Research in Beijing and Surrounding Region 2006) at the suburban site Yufa in the south of Beijing in summer 2006. On most days, local air chemistry was influenced by aged air pollution that was advected by a slow, almost stagnant wind from southern regions. Observed daily concentration maxima were in the range of (4–17) × 106 cm3 for OH and (2–24) × 108 cm3 for HO2 (including an estimated interference of 25% from RO2). During daytime, OH reactivities were generally high (10–30 s?1) and mainly contributed by observed VOCs and their calculated oxidation products. The comparison of modelled and measured HOx concentrations reveals a systematic underprediction of OH as a function of NO. A large discrepancy of a factor 2.6 is found at the lowest NO concentration encountered (0.1 ppb), whereas the discrepancy becomes insignificant above 1 ppb NO. This study extends similar observations from the Pearl-River Delta (PRD) in South China to a more urban environment. The OH discrepancy at Yufa can be resolved, if NO-independent additional OH recycling is assumed in the model. The postulated Leuven Isoprene Mechanism (LIM) has the potential to explain the gap between modelled and measured OH at Beijing taking into account conservative error estimates, but lacks experimental confirmation. This and the hereby unresolved discrepancy at PRD suggest that other VOCs besides isoprene might be involved in the required, additional OH recycling. Fast primary production of ROx radicals up to 7 ppb h1 was determined at Beijing which was dominated by the photolysis of O3, HONO, HCHO, and dicarbonyls. For a special case, 20 August, when the plume of Beijing city was encountered, a missing primary HOx source (about 3 ppb h1) was determined under high NOx conditions similar to other urban areas like Mexico City. CAREBeijing2006 emphasizes the important role of OVOCs as a radical source and sink, and the need for further investigation of the chemical degradation of VOCs in order to better understand radical chemistry in VOC-rich air.
机译:在2006年夏季北京南部的郊区场地yufa的CareBeijing2006(北京和周边地区的空气质量研究活动中的航空质量研究活动期间,通过激光诱导荧光(LiF)进行环境OH和HO2基团的测量。在2006年夏天的郊区yufa。在大多数日子,当地空气化学受到南部地区的缓慢,几乎停滞不前的风化的老年空气污染的影响。观察到的每日浓度最大值为OH和(2-24)×108cm 3的(4-17)×106cm3的HO2的范围(包括估计从RO2的25%的干扰)。在白天期间,OH Reactivities通常高(10-30秒,1),主要由观察到的VOC和它们计算的氧化产品贡献。模型和测量的HOX浓度的比较显示了OH作为否的系统欠压。在遇到的最低浓度(0.1ppb)的最低浓度下发现了因子2.6的大规模差异,而差异在1 ppb中差异不显着。本研究延伸了南方珠江三角洲(珠三角)的类似观察,以更加城市环境。如果在模型中假设无独立的额外oh回收,则可以解决Yufa的OH差异。假设的乳清白异戊二烯机制(LIM)有可能解释在北京的建模和测量oh之间的差距考虑到顾客的保守误差估计,但缺乏实验确认。这个和特此悬而未解决的差异在PRD中表明除了异戊二烯之外的其他VOC可能涉及所需的,额外的OH回收。在北京测定高达7ppb H1的ROX自由基的快速初级生产,其由O3,Hono,Hcho和二羰基的光解为主导。对于一个特殊情况,8月20日,遇到北京市的羽流时,缺少的主要霍尔源(约3个PPB H1)在类似于墨西哥城等其他城市地区的高度NOx条件下确定。 CareBeijing2006强调OVOC作为自由基源和水槽的重要作用,需要进一步调查VOC的化学降解,以便更好地理解富含VOC的空气中的激进化学。
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