Effects of NH3 on secondary aerosol formation from toluene/NOx photo-oxidation in different O3 formation regimes

被引:20
|
作者
Bao, Zhier [1 ]
Xu, Huifeng [1 ]
Li, Kangwei [2 ]
Chen, Linghong [1 ]
Zhang, Xin [1 ]
Wu, Xuecheng [1 ]
Gao, Xiang [1 ]
Azzi, Merched [3 ]
Cen, Kefa [1 ]
机构
[1] Zhejiang Univ, State Key Lab Clean Energy Utilizat, Hangzhou 310027, Peoples R China
[2] Univ Claude Bernard Lyon 1, Univ Lyon, IRCELYON, CNRS, F-69626 Villeurbanne, France
[3] New South Wales Dept Planning Ind & Environm, POB 29, Lidcombe, NSW 1825, Australia
基金
美国国家科学基金会;
关键词
Ammonia; Smog chamber; AMS; Chemical composition; POSITIVE MATRIX FACTORIZATION; ORGANIC AEROSOL; PARTICLE FORMATION; MASS-SPECTROMETER; ALPHA-PINENE; SMOG CHAMBER; COLLECTION EFFICIENCIES; SOURCE APPORTIONMENT; OXIDATION MECHANISM; CHEMICAL MECHANISM;
D O I
10.1016/j.atmosenv.2021.118603
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Ammonia (NH3) is an important base gas in the atmosphere and has received extensive research interest due to its role on secondary aerosol formation. However, the effects of NH3 on the photochemical smog oxidants formation including ozone and secondary aerosol did not attract much attention. In this study, a set of smog chamber experiments was conducted under toluene/NOx photo-oxidation base condition and adding NH3 in the following photochemical regimes referred as hydrocarbon, NOx-limited and transitional regimes. Dedicated instruments including gas analysers, scanning mobility particle sizer (SMPS), aerosol mass spectrometry (HRToF-AMS) were used to measure the gaseous compounds, aerosol mass concentration and chemical composition. It was found that the presence of NH3 did not affect the O3 formation rate. However, the particle number concentration increased dramatically after NH3 was injected in any photochemical regimes. This effect has been mainly attributed to the rapid formation of organic ammonium and ammonium nitrate. The mass spectra of organic aerosols from AMS showed that the most abundant fragments were at m/z 28, 29, 43 and 44, which became higher after the addition of NH3 in the transition and NOx-limited regimes, indicating that NH3 could enhance the formation of the compounds containing carbonyl and carboxylic acid functional groups. Compared to hydrocarbon-limited regime, higher atomic nitrogen-to-carbon (N:C) ratios were observed when NH3 were injected into transition and NOx-limited regimes, and this is mainly due to more organic nitrate formation. Four factors, which were assigned to inorganic nitrate aerosols, carboxylic acid compounds, carbonyl compounds and
引用
收藏
页数:11
相关论文
共 50 条
  • [31] A kinetic mechanism for predicting secondary organic aerosol formation from toluene oxidation in the presence of NOx and natural sunlight
    Hu, Di
    Tolocka, Michael
    Li, Qianfeng
    KamenS, Richard M.
    ATMOSPHERIC ENVIRONMENT, 2007, 41 (31) : 6478 - 6496
  • [32] Secondary organic aerosol formation from photooxidation of C3H6 under the presence of NH3: Effects of seed particles
    Wang, Yuan
    Cui, Shijie
    Fu, Xuewei
    Zhang, Yunjiang
    Wang, Junfeng
    Fu, Pingqing
    Ge, Xinlei
    Li, Haiwei
    Wang, Xinming
    ENVIRONMENTAL RESEARCH, 2022, 211
  • [33] Formation of oxygenated-polycyclic aromatic compounds in aerosol from the photo-oxidation of o-tolualdehyde
    Webb, Paul J.
    Hamilton, Jacqueline F.
    Lewis, Alastair C.
    Wirtz, Klaus
    POLYCYCLIC AROMATIC COMPOUNDS, 2006, 26 (04) : 237 - 252
  • [34] The formation and growth of Fe2O3 nanoparticles from the photo-oxidation of iron pentacarbohyl
    Saunders, Russell W.
    Plane, John M. C.
    JOURNAL OF AEROSOL SCIENCE, 2010, 41 (05) : 475 - 489
  • [35] Chamber studies of secondary organic aerosol formation (SOA) from O3 and NO3 + a-pinene
    Arata, Caleb
    Meade, Rhiana D.
    Fry, Juliane L.
    ABSTRACTS OF PAPERS OF THE AMERICAN CHEMICAL SOCIETY, 2011, 242
  • [36] Secondary organic aerosol and ozone formation from photo-oxidation of unburned diesel fuel in a surrogate atmospheric environment
    Li, Weihua
    Cocker, David R., III
    ATMOSPHERIC ENVIRONMENT, 2018, 184 : 17 - 23
  • [37] Secondary organic aerosol formation from the oxidation of a series of sesquiterpenes: α-cedrene, β-caryophyllene, α-humulene and α-farnesene with O3, OH and NO3 radicals
    Jaoui, Mohammed
    Kleindienst, Tadeusz E.
    Docherty, Kenneth S.
    Lewandowski, Michael
    Offenberg, John H.
    ENVIRONMENTAL CHEMISTRY, 2013, 10 (03) : 178 - 193
  • [38] Effects of Precursor Structure on First-Generation Photo-Oxidation Organic Aerosol Formation
    Sofio, D.
    Long, D.
    Kohls, T.
    Kunz, J.
    Wentzel, M.
    Hanson, D.
    FRONTIERS IN ENVIRONMENTAL SCIENCE, 2022, 10
  • [39] Synergetic formation of secondary inorganic and organic aerosol: effect of SO2 and NH3 on particle formation and growth
    Chu, Biwu
    Zhang, Xiao
    Liu, Yongchun
    He, Hong
    Sun, Yele
    Jiang, Jingkun
    Li, Junhua
    Hao, Jiming
    ATMOSPHERIC CHEMISTRY AND PHYSICS, 2016, 16 (22) : 14219 - 14230
  • [40] Formation of dinitrogen by oxidation of [(bpy)(2)(NH3)RuORu(NH3)(bpy)(2)](4)
    Ishitani, O
    White, PS
    Meyer, TJ
    INORGANIC CHEMISTRY, 1996, 35 (08) : 2167 - &