Sizing and source characterization of particulate organic nitrates based on long time-of-flight aerosol mass spectrometer (Long-ToF-AMS) in Shenzhen
YU Guang-he1, CAO Li-ming1,2, ZHU Qiao2, WANG Chuan1, HUANG Xiao-feng2
1. Peking University-Hong Kong University of Science and Technology Shenzhen Hong Kong Institution, Shenzhen 518055, China; 2. Shenzhen Graduate School, Key Laboratory for Urban Habitat Environmental Science and Technology, Peking University, Shenzhen 518055, China
Abstract:In this study, a long time-of-flight aerosol mass spectrometer (Long- ToF-AMS) was applied to characterize particulate organic nitrates (pON) during March 30th to April 17th in 2021 at Shenzhen. Using cross-validation estimated methods, we calculated pON accounting for 5.08%~11.00% in total OA. The diurnal pattern with nighttime higher mass loading for pON and the best correlation with less-oxidized oxygenated OA (LO-OOA) at night indicated that pON formation might be more associated with nighttime fresh secondary formation. The high-resolution size distribution of pON showed they contained a substantial fraction of smaller size particles, further confirming the contributions from primary aerosols or newly formed secondary aerosols at night. Additionally, the potential precursors for pON formation was further explored based on comparison analysis between mass spectrum of our ambient data and the laboratory generated pON using different precursors. The results implied that volatile organic compounds (VOCs) emitted from biogenic sources and biomass burning were potential precursors for pON formation in Shenzhen.
于广河, 曹礼明, 朱乔, 王川, 黄晓锋. 深圳大气有机硝酸酯粒径分布特征和来源研究[J]. 中国环境科学, 2022, 42(4): 1510-1517.
YU Guang-he, CAO Li-ming, ZHU Qiao, WANG Chuan, HUANG Xiao-feng. Sizing and source characterization of particulate organic nitrates based on long time-of-flight aerosol mass spectrometer (Long-ToF-AMS) in Shenzhen. CHINA ENVIRONMENTAL SCIENCECE, 2022, 42(4): 1510-1517.
Poschl U, Atmospheric aerosols:Composition, transformation, climate and health effects[J]. Angewandte Chemie-International Edition, 2005,44(46):7520-7540.
[2]
Pearce W, Holmberg K, Hellsten I, et al. Climate change on twitter:topics, communities and conversations about the 2013 IPCC Working Group 1Report[J]. Plos One, 2014,9(4).
[3]
Kanakidou M, Seinfeld J H, Pandis S N, et al. Organic aerosol and global climate modelling:a review[J]. Atmospheric Chemistry and Physics, 2005,5:1053-1123.
[4]
Saathoff H, Naumann K H, Möhler O, et al. Temperature dependence of yields of secondary organic aerosols from the ozonolysis of α-pinene and limonene[J]. Atmospheric Chemistry and Physics, 2009,9(5):1551-1577.
[5]
Perring A E, Pusede S E, Cohen R C, An observational perspective on the atmospheric impacts of alkyl and multifunctional nitrates on ozone and secondary organic aerosol[J]. Chemical Reviews, 2013,113(8):5848-5870.
[6]
Ng N L, Brown S S, Archibald A T, et al. Nitrate radicals and biogenic volatile organic compounds:oxidation, mechanisms, and organic aerosol[J]. Atmospheric Chemistry and Physics, 2017,17(3):2103- 2162.
[7]
Obrien S R, Mayewski P A, Meeker L D, et al. Complexity of holocene climate as reconstructed from a Greedland ice core[J]. Science, 1995,270,(5244):1962-1964.
[8]
Rollins A W, Browne E C, Min K E, et al. Evidence for NOx control over nighttime SOA formation[J]. Science, 2012,337(6099):1210- 1212.
[9]
Thieser J, Schuster G, Schuladen J, et al. A two-channel thermal dissociation cavity ring-down spectrometer for the detection of ambient NO2, RO2NO2 and RONO2[J]. Atmospheric Measurement Techniques, 2016,9(2):553-576.
[10]
Lopez-Hilfiker F D, Mohr C, Ehn M, et al. A novel method for online analysis of gas and particle composition:description and evaluation of a Filter Inlet for Gases and AEROsols (FIGAERO)[J]. Atmospheric Measurement Techniques, 2014,7(4):983-1001.
[11]
Farmer D K, Matsunaga A, Docherty K S, et al. Response of an aerosol mass spectrometer to organonitrates and organosulfates and implications for atmospheric chemistry[J]. Proceedings of the National Academy of Sciences of the United States of America, 2010,107(15):6670-5.
[12]
Hao L Q, Kortelainen A, Romakkaniemi S, et al. Atmospheric submicron aerosol composition and particulate organic nitrate formation in a boreal forestland-urban mixed region[J]. Atmospheric Chemistry and Physics, 2014,14(24):13483-13495.
[13]
Xu L, Suresh S, Guo H, et al. Aerosol characterization over the southeastern United States using high-resolution aerosol mass spectrometry:spatial and seasonal variation of aerosol composition and sources with a focus on organic nitrates[J]. Atmospheric Chemistry and Physics, 2015,15(13):7307-7336.
[14]
Xu L, Guo H Y, Boyd C M, et al. Effects of anthropogenic emissions on aerosol formation from isoprene and monoterpenes in the southeastern United States[J]. Proceedings of the National Academy of Sciences of the United States of America, 2015,112(1):37-42.
[15]
Zhu Q, He L-Y, Huang X-F, et al. Atmospheric aerosol compositions and sources at two national background sites in northern and southern China[J]. Atmospheric Chemistry and Physics, 2016,16(15):10283- 10297.
[16]
Yu K, Zhu Q, Du K, et al. Characterization of nighttime formation of particulate organic nitrates based on high-resolution aerosol mass spectrometry in an urban atmosphere in China[J]. Atmospheric Chemistry and Physics, 2019,19(7):5235-5249.
[17]
Middlebrook A M, Bahreini R, Jimenez J L, et al. Evaluation of composition-dependent collection efficiencies for the aerodyne aerosol mass spectrometer using field data[J]. Aerosol Science and Technology, 2012,46(3):258-271.
[18]
Fry J L, Draper D C, Zarzana K J, et al. Observations of gas- and aerosol-phase organic nitrates at BEACHON-RoMBAS 2011[J]. Atmospheric Chemistry and Physics, 2013,13(17):8585-8605.
[19]
Boyd C M, Sanchez J, Xu L, et al. Secondary organic aerosol formation from the β-pinene+NO3system:effect of humidity and peroxy radical fate[J]. Atmospheric Chemistry and Physics, 2015, 15(13):7497-7522.
[20]
Bruns E A, Perraud V, Zelenyuk A, et al. Comparison of FTIR and particle mass spectrometry for the measurement of particulate organic nitrates[J]. Environmental Science & Technology, 2010,44(3):1056- 61.
[21]
Sato K, Takami A, Isozaki T, et al. Mass spectrometric study of secondary organic aerosol formed from the photo-oxidation of aromatic hydrocarbons[J]. Atmospheric Environment, 2010,44(8):1080-1087.
[22]
Joo T, Rivera-Rios J C, Takeuchi M, et al. Secondary organic aerosol formation from reaction of 3-methylfuran with Nitrate Radicals[J]. ACS Earth and Space Chemistry, 2019,3(6):922-934.
[23]
Paatero P, Tapper U, Positive matrix factorization-a nonnegative factor model with optimal utilization of error-estimates of data values[J]. Environmetrics, 1994,5(2):111-126.
[24]
DeCarlo P F, Kimmel J R, Trimborn A, et al. Field-deployable, high-resolution, time-of-flight aerosol mass spectrometer[J]. Analytical Chemistry, 2006,78(24):8281-9.
[25]
Jimenez J L, Jayne J T, Shi Q, et al. Ambient aerosol sampling using the Aerodyne Aerosol Mass Spectrometer[J]. Journal of Geophysical Research-Atmospheres, 2003,108(D7).
[26]
Huang X F, He L Y, Hu M, et al. Highly time-resolved chemical characterization of atmospheric submicron particles during 2008 Beijing Olympic Games using an aerodyne high-resolution aerosol mass spectrometer[J]. Atmospheric Chemistry and Physics, 2010, 10(18):8933-8945.
[27]
Graeffe F. Fragmentation patterns of particulate organic nitrates in an Aerosol Mass Spectrometer[D]. University of Helsinki, 2019.
[28]
Ahern A T, Robinson E S, Tkacik D S, et al. Production of secondary organic aerosol during aging of biomass burning smoke from fresh fuels and its relationship to VOC precursors[J]. Journal of Geophysical Research-Atmospheres, 2019,124(6):3583-3606.
[29]
Zhu Q, Cao L M, Tang M X, et al. Characterization of organic aerosol at a rural site in the North China Plain Region:Sources, volatility and organonitrates[J]. Advances in Atmospheric Sciences, 202138(7):1115-1127