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Atmospheric Hydrogen Peroxide (H2O2) at the Foot and Summit of Mt. Tai: Variations, Sources and Sinks, and Implications for Ozone Formation Chemistry
Journal of Geophysical Research: Atmospheres ( IF 4.4 ) Pub Date : 2021-07-26 , DOI: 10.1029/2020jd033975
Can Ye 1, 2 , Chaoyang Xue 1, 2, 3 , Chenglong Zhang 1, 2, 4 , Zhuobiao Ma 1, 2 , Pengfei Liu 1, 2, 4 , Yuanyuan Zhang 1, 2, 4 , Chengtang Liu 1, 2, 4 , Xiaoxi Zhao 1, 2 , Wenjin Zhang 1, 2 , Xiaowei He 1, 2 , Yifei Song 1, 2 , Junfeng Liu 1, 2, 4 , Weihao Wang 5 , Benhui Sui 6 , Ran Cui 6 , Xue Yang 6 , Rubo Mei 6 , Jianmin Chen 7 , Yujing Mu 1, 2, 4
Affiliation  

Hydrogen peroxide (H2O2) acts as a terminal sink for atmospheric HOx radicals (OH and HO2), playing a key role in tropospheric O3 formation. However, there are few field measurements of atmospheric H2O2 to assess its role in O3 formation, especially for the seriously polluted region of the North China Plain. In this study, H2O2 concentrations were measured at the foot of Mt. Tai from May to July 2018 and the summit of Mt. Tai from May to June 2019, with average values of 0.93 ± 1.01 and 2.05 ± 1.20 ppb, respectively. H2O2 exhibited a pronounced diurnal variation with a noon-peak at the foot of Mt. Tai, which could be well reproduced by a gas-phase box model with H2O2 dry deposition velocity of 3 cm s−1 included, indicating H2O2 was mainly photochemically produced. Modeling analysis showed H2O2 production at the foot was most sensitive to alkenes and aromatics, while the source and sink for H2O2 were dominated by HO2 recombination and dry deposition, respectively. Compared with the summer-measurement in 2007, the remarkable elevation of H2O2 at the summit might be ascribed to volatile organic compounds (VOCs) increase and SO2 decline. Both H2O2-O3 correlation and H2O2/NOz ratio suggested O3 formation at the foot of Mt. Tai was mainly VOC-sensitive in the early morning and shifted to NOx-sensitive thereafter. Therefore, reduction of VOCs emission especially for the reactive species of alkenes and aromatics in the morning as well as NOx emission around noontime will be effective for mitigating the serious O3 (as well as H2O2) pollution in Tai'an city.

中文翻译:

山脚和山顶的大气过氧化氢 (H2O2)。Tai:变化、来源和汇,以及臭氧形成化学的影响

过氧化氢 (H 2 O 2 ) 作为大气中 HO x自由基(OH 和 HO 2)的终端汇,在对流层 O 3 的形成中起关键作用。然而,很少有大气H 2 O 2 的现场测量来评估其在O 3形成中的作用,特别是对于华北平原污染严重的地区。在这项研究中,测量了山脚下的H 2 O 2浓度。2018 年 5 月至 7 月的泰和山的顶峰。Tai 2019 年 5 月至 6 月,平均值分别为 0.93±1.01 和 2.05±1.20 ppb。H 2 O 2表现出明显的昼夜变化,在山脚下有一个中午高峰。Tai 可以很好地被包含H 2 O 2干沉积速度为3 cm s -1的气相箱模型再现,表明H 2 O 2主要是光化学产生的。建模分析表明,脚下产生的H 2 O 2对烯烃和芳烃最敏感,而 H 2 O 2的源和汇分别以 HO 2复合和干沉积为主。与 2007 年夏季实测相比,H 2 O 2显着升高可能归因于挥发性有机化合物 (VOCs) 增加和 SO 2下降。H 2 O 2 -O 3相关性和H 2 O 2 /NO z比均表明在山脚下形成了O 3。Tai 主要在清晨对 VOC 敏感,此后转变为对 NO x敏感。因此,减少挥发性有机化合物排放的特别适用于烯烃和芳族化合物的在上午反应性物质以及NO X周围中午发射将是减轻严重ø有效3(以及以H 2 ö 2) 泰安市污染。
更新日期:2021-08-05
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