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Significant concentrations of nitryl chloride sustained in the morning: investigations of the causes and impacts on ozone production in a polluted region of northern China

机译:早晨维持显着的硝酰氯浓度:对中国北方污染地区臭氧产生的原因和影响进行调查

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摘要

Nitryl chloride (ClNO) is a dominant source of chlorineradical in polluted environment, and can significantly affect the atmosphericoxidative chemistry. However, the abundance of ClNO and its exact roleare not fully understood under different environmental conditions. Duringthe summer of 2014, we deployed a chemical ionization mass spectrometer tomeasure ClNO and dinitrogen pentoxide (NO) at a rural sitein the polluted North China Plain. Elevated mixing ratios of ClNO( 350 pptv) were observed at most of the nights with low levelsof NO ( 200 pptv). The highest ClNO mixing ratioof 2070 pptv (1 min average) was observed in a plume from a megacity(Tianjin), and was characterized with a faster NO heterogeneous loss rateand ClNO production rate compared to average conditions. The abundantClNO concentration kept increasing even after sunrise, and reached apeak 4 h later. Such highly sustained ClNO peaks after sunrise arediscrepant from the previously observed typical diurnal pattern.Meteorological and chemical analysis shows that the sustained ClNOmorning peaks are caused by significant ClNO production in theresidual layer at night followed by downward mixing after breakup of thenocturnal inversion layer in the morning. We estimated that  ∼  1.7–4.0 ppbv of ClNO would exist in the residual layer in order tomaintain the observed morning ClNO peaks at the surface site.Observation-based box model analysis show that photolysis of ClNOproduced chlorine radical with a rate up to 1.12 ppbv h, accountingfor 10–30 % of primary RO production in the morning hours. Theperturbation in total radical production leads to an increase of integrateddaytime net ozone production by 3 % (4.3 ppbv) on average, and with alarger increase of 13 % (11 ppbv) in megacity outflow that wascharacterized with higher ClNO and a relatively lower oxygenated hydrocarbon (OVOC) to non-methane hydrocarbon(NMHC) ratio.
机译:氯化硝基氯(ClNO)是污染环境中氯自由基的主要来源,并且可以显着影响大气中的氧化化学。然而,在不同的环境条件下,ClNO的丰度及其确切作用尚不完全清楚。 2014年夏季,我们在受污染的华北平原农村地区部署了化学电离质谱仪,以测量ClNO和五氧化二氮(NO)。在大多数夜间,低水平的NO(<200 pptv)观察到ClNO(> 350 pptv)的混合比升高。在一个特大城市(天津)的烟羽中观察到最高的ClNO混合比为2070 pptv(平均1 min),与平均条件相比,其NO异质损失率和ClNO生成率更高。即使在日出后,丰富的ClNO浓度仍在增加,并在4 h后达到峰值。日出后这种高度持续的ClNO峰与以前观察到的典型的昼夜模式相差很大。 。我们估计残留层中会存在〜1.7–4.0 ppbv的ClNO,以维持在表面位置观察到的早晨ClNO峰。基于观测的盒模型分析表明,ClNO的光解产生氯自由基的速率高达1.12 ppbv h ,占早上主要反渗透产量的10%至30%。总自由基产生的扰动导致综合臭氧日净产量平均增加3%(4.3(ppbv),而大城市流出量的增加幅度更大,增加了13%(11 ppbv),其特征在于较高的ClNO和相对较低的含氧烃( OVOC)与非甲烷碳氢化合物(NMHC)的比率。

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