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首页> 外文期刊>Atmospheric chemistry and physics >Radical chemistry at night: comparisons between observed and modelled HOsubx/sub, NOsub3/sub and Nsub2/subOsub5/sub during the RONOCO project
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Radical chemistry at night: comparisons between observed and modelled HOsubx/sub, NOsub3/sub and Nsub2/subOsub5/sub during the RONOCO project

机译:夜间的自由基化学:在观测期间和模拟的HO x ,NO 3 和N 2 O 5 之间的比较RONOCO项目

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The RONOCO (ROle of Nighttime chemistry in controlling the Oxidising Capacity of theAtmOsphere) aircraft campaign during July 2010 and January 2011 madeobservations of OH, HO2, NO3, N2O5 and a number ofsupporting measurements at night over the UK, and reflects the firstsimultaneous airborne measurements of these species. We compare the observedconcentrations of these short-lived species with those calculated by a boxmodel constrained by the concentrations of the longer lived species using adetailed chemical scheme. OH concentrations were below the limit ofdetection, consistent with model predictions. The model systematicallyunderpredicts HO2 by ~200% and overpredicts NO3and N2O5 by around 80 and 50%, respectively.Cycling between NO3 and N2O5 is fast and thus we define theNO3x (NO3x=NO3+N2O5) family. Productionof NO3x is overwhelmingly dominated by the reaction of NO2 withO3, whereas its loss is dominated by aerosol uptake of N2O5,with NO3+VOCs (volatile organic compounds) and NO3+RO2 playing smaller roles. The production of HOx and ROx radicals is mainly due to thereaction of NO3 with VOCs. The loss of these radicals occurs through acombination of HO2+RO2 reactions, heterogeneous processes andproduction of HNO3 from OH+NO2, with radical propagationprimarily achieved through reactions of NO3 with peroxy radicals. ThusNO3 at night plays a similar role to both OH and NO during the day inthat it both initiates ROx radical production and acts to propagate thetropospheric oxidation chain. Model sensitivity to the N2O5aerosol uptake coefficient (γN2O5) is discussed and we findthat a value of γN2O5=0.05 improves model simulations forNO3 and N2O5, but that these improvements are at the expenseof model success for HO2. Improvements to model simulations forHO2, NO3 and N2O5 can be realised simultaneously oninclusion of additional unsaturated volatile organic compounds, however thenature of these compounds is extremely uncertain.
机译:在2010年7月至2011年1月的RONOCO(夜间化学作用在控制大气层氧化能力中的作用)飞机运动中进行了OH,HO 2 ,NO 3 ,N 2 O 5 和在英国夜间进行的许多辅助测量,并且反映了这些物种的首次同时空载测量。我们将这些短命物种的浓度与采用详细化学方案的长寿物种的浓度所限制的盒模型计算得出的浓度进行了比较。 OH浓度低于检测极限,与模型预测一致。该模型系统地将HO 2 的预测降低了约200%,将NO 3 和N 2 O 5 的预测高了约80和分别为50%.NO 3 和N 2 O 5 之间的循环速度很快,因此我们定义了NO 3x (NO 3x = NO 3 + N 2 O 5 )系列。 NO 3x 的产生主要由NO 2 与O 3 的反应决定,而其损失主要由N 2的气溶胶吸收决定。 O 5 ,具有NO 3 + VOC(挥发性有机化合物)和NO 3 + RO 2 扮演较小的角色。 HO x 和RO x 自由基的产生主要是由于NO 3 与VOC的反应。这些自由基的损失是通过HO 2 + RO 2 反应,异质过程以及由OH + NO 生成HNO 3 的组合而发生的2 ,自由基的传播主要是通过NO 3 与过氧自由基的反应实现的。因此,夜间的NO 3 与白天的OH和NO相似,因为它们都引发RO x 自由基的产生并起到传播对流层氧化链的作用。模型对N 2 O 5 气溶胶吸收系数(γ N 2 O 5 )进行讨论,我们发现γ N 2 O 5 = sub0.05可以改善NO 3 和N 2 O 5 ,但是这些改进是以HO 2 的模型成功为代价的。包含其他不饱和元素可以同时实现对HO 2 ,NO 3 和N 2 O 5 模型仿真的改进挥发性有机化合物,但是这些化合物的性质非常不确定。

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