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Interpretation of decadal-scale ozone production efficiency in the Seoul Metropolitan Area: Implication for ozone abatement

机译:首尔大都市区的二等级臭氧生产效率解读:臭氧减少的含义

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Understanding the drivers of urban ozone (O-3) formation is challenging and requires uncovering the non-linear relationship between O-3 and its precursors. We used a novel method to differentiate between background O-3 levels and local photochemical O-3 generation using the observation-based O-3 production efficiency (OPE) from decade-long observations including nitrogen dioxide (NO2), nitrogen monoxide (NO), reactive nitrogen compounds (NOy), O-3, and 56 volatile organic compounds (VOCs) covering eight years (2009-2016). In this study, we employed O-x (=O-3+NO2), and defined OPEx as the number of O-x molecules produced from the oxidation of a single NOx molecule, and estimates the local contribution (in %) to total O-3 from the slope of the O-x-NO2(=NOy-NOx) linear regression. We thus identified the local urban O-3 formation regime using the relationship of several factors, including nitrogen oxide (NOx), VOC/NOx, NO2, NO2, and long-range transported O-x, and suggested how O-3 can be reduced in the Seoul Metropolitan Area (SMA).The results show that the regional background dominates the annual level of O-x with a contribution of about 66 +/- 11%, while photochemical production acts as a stronger factor influencing the annual variability of O-x than regional background. Regional background varies by transport evidenced by its good correlation with the west wind fraction, whereas photochemical production depends on the VOC/NOx ratio, which is high in summer and low in winter. The relationship between photochemical production and VOC/NOx indicates that the transition of the O-x formation regime occurs at a VOC/NOx ratio of approximately 4 in the SMA. Urban environments with NOx 20 ppb typically lie in low VOC/NOx zone, where reduced NO2 emissions lead to decreased NO2 but increased OPEx, with no discernible change in photochemical O-x production. Thus, NOx emission reductions in urban environments would have a negligible effect on Ox reduction. In contrast, suburban environments such as usually NOx 10 ppb are located in the higher VOC/NOx zone, where decreased NO2 leads to decreased OPEx with no discernible change in NO2, consequently suppressing photochemical O-x production. Together, these results suggest that any urban O-3 policy in the SMA should consider significant cuts in NOx emissions to allow the O-3 regime to shift. The OPEx method can also be applied to other urban areas for the development of effective O-3 reduction policies.
机译:了解城市臭氧(O-3)形成的司机具有挑战性,需要揭示O-3与其前体之间的非线性关系。我们使用了一种新的方法来利用来自包括氮二氧化氮(NO2),氮一氧化氮(NO)的观测到包括氮气(NO2)(NO)的观察到的o-3水平和局部光化学o-3代的背景O-3水平和局部光化学O-3代。 ,覆盖8年(2009-2016)的反应性氮化合物(Noy),O-3和56个挥发性有机化合物(VOC)。在该研究中,我们使用牛(= O-3 + NO2),并将OPEX定义为由单个NOx分子的氧化产生的氧化氧分子的数量,并估计来自的局部贡献(以%)到总O-3 OX-NO2(= NOY-NOx)线性回归的斜率。因此,我们使用若干因素的关系确定了本地城市O-3形成制度,包括氮氧化物(NOx),VOC / NOx,NO2,NO2和远程运输牛,并提出了O-3如何降低首尔大都市区(SMA)。结果表明,区域背景占据了玉米的年度水平,贡献约为66 +/- 11%,而光化学产量则作为影响牛牛年​​变异性的更强因素,而不是区域背景。区域背景通过与西风分数良好相关性的运输变化,而光化学生产取决于VOC / NOx比率,冬季夏季高,较低。光化学生产和VOC / NOx之间的关系表示O-X形成制度的转变发生在SMA中约4的VOC / NOx比例。 Nox的城市环境> 20 ppb通常位于低VOC / NOx区域,其中降低的NO2排放导致NO2降低,但OPEX增加,光化学O-X生产没有可辨别的变化。因此,城市环境中的NOx排放减少对氧化氧的影响可忽略不计。相反,诸如通常NOx <10 ppb的郊区环境位于更高的VOC / NOx区域中,其中降低的NO2导致OPEX降低,NO2中没有可辨别的变化,因此抑制了光化学O-X的生产。这些结果表明,SMA中的任何城市O-3政策都应考虑NOx排放中的重大削减,以允许O-3制度转变。 OPEX方法也可以应用于其他城市地区,以发展有效的O-3还原政策。

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