the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Multiple pathways for the formation of secondary organic aerosol in North China Plain in summer
- 1SKLLQG, Center for Excellence in Quaternary Science and Global Change, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
- 2Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266000, China
- 3Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710049, China
- 4University of Chinese Academy of Sciences, Beijing 100049, China
- 5State Key Laboratory of Severe Weather & Key Laboratory of Atmospheric Chemistry of C MA, Chinese Academy of Meteorological Sciences, Beijing 100081, China
- 6Department of Environmental Engineering, School of Energy and Environmental Engineering, Hebei University of Engineering, Handan 056038, China
- 7Hebei Key Laboratory of Air Pollution Cause and Impact, Handan 056038, China
- 8Department of Civil and Environmental Engineering, and Centre for Regional Oceans, Faculty of Science and Technology, University of Macau, Taipa, Macau 999078, China
- 1SKLLQG, Center for Excellence in Quaternary Science and Global Change, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
- 2Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266000, China
- 3Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710049, China
- 4University of Chinese Academy of Sciences, Beijing 100049, China
- 5State Key Laboratory of Severe Weather & Key Laboratory of Atmospheric Chemistry of C MA, Chinese Academy of Meteorological Sciences, Beijing 100081, China
- 6Department of Environmental Engineering, School of Energy and Environmental Engineering, Hebei University of Engineering, Handan 056038, China
- 7Hebei Key Laboratory of Air Pollution Cause and Impact, Handan 056038, China
- 8Department of Civil and Environmental Engineering, and Centre for Regional Oceans, Faculty of Science and Technology, University of Macau, Taipa, Macau 999078, China
Abstract. Secondary organic aerosol (SOA) has been identified as a major contributor to fine particulate matter (PM2.5) in North China Plain (NCP). However, the chemical mechanisms involved are still unclear due to incomplete understanding of its multiple formation processes. Here we report field observations in summer in Handan of NCP, based on high-resolution online measurements. Our results reveal the formation of SOA via photochemistry and two types of aqueous-phase chemistry, the latter of which include nocturnal and daytime processing. The photochemical pathway is the most important under high Ox (=O3 + NO2) conditions (65.1 ± 20.4 ppb). The efficient SOA formation from photochemistry (phochem-SOA) dominated the daytime (65 % to OA) with an average growth rate of 0.8 μg m−3 h−1. During the high relative humidity (RH: 83.7 ± 12.5 %) period, strong nocturnal aqueous-phase SOA formation (aq-SOA) played a significant role in SOA production (45 % to OA) with a nighttime growth rate of 0.6 μg m-3 h-1. Meanwhile, an equally fast growth rate of 0.6 μg m-3 h-1 of phochem-SOA from daytime aqueous-phase photochemistry was also observed, which contributed 39 % to OA, showing that photochemistry in the aqueous phase is also a non-negligible pathway in summer. The primary-related-SOA (SOA attributed to primary particulate organics) and aq-SOA are related to residential coal combustion activities, supported by distinct fragments from polycyclic aromatic hydrocarbons (PAHs). Moreover, the conversion and rapidly oxidation of primary-related-SOA to aq-SOA could be possible in the aqueous phase under high-RH conditions. This work sheds light on the multiple formation pathways of SOA in ambient air of complex pollution, and improves our understanding of ambient SOA formation and aging in summer with high oxidation capacity.
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Yifang Gu et al.
Status: open (until 15 Oct 2022)
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RC1: 'Comment on acp-2022-573', Anonymous Referee #1, 01 Oct 2022
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General comments:
The paper titled “Multiple pathways for the formation of secondary organic aerosol in North China Plain in summer” by Gu et al. reported an summer field observation in Handan City, in which four types of SOA were resolved using the PMF method dealing with the OA mass spectra data from a a soot particle long time-of-flight aerosol mass spectrometer. In addition, the variations and evolution processes of so-called SOA factors were discussed and their formation pathway were then deduced. Although a series of similar studies using AMS data had been reported in NCP previously, this study provided a more detail source appointment results in distinguish SOA as freshly (less-oxidized) and aged (more-oxidized) factors, and further directly associated with the formation pathway (photochemistry and aqueous-phase). With this, a better understanding of ambient SOA formation and aging in complex pollution with high oxidation capacity were gained. The manuscript was well written and presented clearly. Therefore I recommend the publication of Gu et al. work after some issues were clarified and revised.
Specific and technical comments:
- Line 167-170. The new named four SOA factors are interesting, that different from previous studies using same AMS data set resolved by PMF. But the identification of those SOA fators were missed here, or a brief description but not enough appeared in the end of section 3.1. I think the identification of SOA factor is the most important and the foundation of this study, thus a detail description should be provided here. For example, why do the authors directly name the OOA factor as photochemistry and aqueous-phase formed? What the difference between the primary-related SOA and CCOA, both of which showed pronounced peaks of PAH ions?
- Line 260-262. The transformation processes of POA and fresh SOA factor to phochem-SOA is interesting, it deserve more discussions here. Exploring the diurnal pattern of these factors during a special episode would be a choice, such as that conducted in Li et al. 2020. https://doi.org/10.1016/j.atmosenv.2019.117070.
- Line 277-282. The aqueous-phase chemistry may also contributed to the fresh-SOA, but if so it is unclear what the difference of aqueous-phase in fresh-SOA and aq-SOA?
- Line 289-290. It is subjective to conclude that the photochemistry is more efficient in elevating the oxidation degree of OA, as the correlations were analyzed during different periods (P2 and P3), during which other factors like primary emissions and transportation would be different and also effect the O:C ratio of OA.
- Line 308-310. It is unclear where the photochemistry formation of SOA occurred. Please clarify it and revise this sentence.
- Line 351-353. I do not think the transformation of POA to SOA could be deduced based solely on the negative correlation of each other. In fact, as showed in Fig 7, the negative correlation between phochem-SOA and POA would be expected, as the formation period of phochem-SOA usually occurred during the noontime when the boundary layer was much developed, while the POA usually decreased via horizontal and vertical diffusion. It is also supported by the better correlations in P2, which defined as high-Ox period and also has better diffusion conditions. Please clarify it.
Yifang Gu et al.
Yifang Gu et al.
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