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华北平原的臭氧污染蔓延至冬季晚些时候的雾霾季节。

Ozone pollution in the North China Plain spreading into the late-winter haze season.

机构信息

Harvard-NUIST Joint Laboratory for Air Quality and Climate, Nanjing University of Information Science and Technology, 210044 Nanjing, China.

John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138.

出版信息

Proc Natl Acad Sci U S A. 2021 Mar 9;118(10). doi: 10.1073/pnas.2015797118.

DOI:10.1073/pnas.2015797118
PMID:33649215
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7958175/
Abstract

Surface ozone is a severe air pollution problem in the North China Plain, which is home to 300 million people. Ozone concentrations are highest in summer, driven by fast photochemical production of hydrogen oxide radicals (HO) that can overcome the radical titration caused by high emissions of nitrogen oxides (NO) from fuel combustion. Ozone has been very low during winter haze (particulate) pollution episodes. However, the abrupt decrease of NO emissions following the COVID-19 lockdown in January 2020 reveals a switch to fast ozone production during winter haze episodes with maximum daily 8-h average (MDA8) ozone concentrations of 60 to 70 parts per billion. We reproduce this switch with the GEOS-Chem model, where the fast production of ozone is driven by HO radicals from photolysis of formaldehyde, overcoming radical titration from the decreased NO emissions. Formaldehyde is produced by oxidation of reactive volatile organic compounds (VOCs), which have very high emissions in the North China Plain. This remarkable switch to an ozone-producing regime in January-February following the lockdown illustrates a more general tendency from 2013 to 2019 of increasing winter-spring ozone in the North China Plain and increasing association of high ozone with winter haze events, as pollution control efforts have targeted NO emissions (30% decrease) while VOC emissions have remained constant. Decreasing VOC emissions would avoid further spreading of severe ozone pollution events into the winter-spring season.

摘要

地面臭氧是中国华北平原地区严重的空气污染问题,该地区居住着 3 亿人口。由于快速光化学反应产生的氢氧自由基(HO)可克服燃料燃烧产生的大量氮氧化物(NO)引起的自由基滴定作用,因此臭氧浓度在夏季最高。臭氧在冬季雾霾(颗粒物)污染期间非常低。然而,2020 年 1 月 COVID-19 封锁后 NO 排放量的突然下降表明,冬季雾霾期间臭氧的快速生成发生了转变,最大日 8 小时平均(MDA8)臭氧浓度达到 60 至 70 十亿分之一。我们使用 GEOS-Chem 模型再现了这种转变,其中臭氧的快速生成是由甲醛光解产生的 HO 自由基驱动的,克服了因 NO 排放量减少而引起的自由基滴定作用。甲醛是由反应性挥发性有机化合物(VOC)氧化产生的,这些 VOC 在华北平原地区的排放量非常高。这种自封锁以来,1 月至 2 月向臭氧生成机制的显著转变说明了一个更普遍的趋势,即 2013 年至 2019 年,华北平原冬季和春季臭氧增加,与冬季雾霾事件相关的高臭氧浓度增加,因为污染控制措施针对的是 NO 排放(减少 30%),而 VOC 排放保持不变。减少 VOC 排放将避免严重的臭氧污染事件进一步蔓延到冬春季节。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8425/7958175/fb33da325d64/pnas.2015797118fig04.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8425/7958175/4d051df00e43/pnas.2015797118fig01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8425/7958175/e5b865bc3fc1/pnas.2015797118fig02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8425/7958175/b782bc592ee9/pnas.2015797118fig03.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8425/7958175/fb33da325d64/pnas.2015797118fig04.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8425/7958175/4d051df00e43/pnas.2015797118fig01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8425/7958175/e5b865bc3fc1/pnas.2015797118fig02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8425/7958175/b782bc592ee9/pnas.2015797118fig03.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8425/7958175/fb33da325d64/pnas.2015797118fig04.jpg

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