4.2 Article

Is reducing new particle formation a plausible solution to mitigate particulate air pollution in Beijing and other Chinese megacities?

Journal

FARADAY DISCUSSIONS
Volume 226, Issue -, Pages 334-347

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/D0FD00078G

Keywords

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Funding

  1. Academy of Finland via the Center of Excellence in Atmospheric Sciences [307331]
  2. European Research Council via ATM-GTP [742206]
  3. European Union [895875]
  4. Academy of Finland [316114, 315203]
  5. Doctoral Programme in Atmospheric Sciences at the University of Helsinki
  6. National Key RAMP
  7. D Program of China [2017YFC0209503, 2017YFC0209505]
  8. National Natural Science Foundation of China [21876094, 91644213, 41730106]
  9. Samsung PM2.5 SRP
  10. Swiss National Science postdoc mobility grant [P2EZP2_181599]
  11. Academy of Finland (AKA) [315203, 315203] Funding Source: Academy of Finland (AKA)
  12. European Research Council (ERC) [742206] Funding Source: European Research Council (ERC)
  13. Marie Curie Actions (MSCA) [895875] Funding Source: Marie Curie Actions (MSCA)
  14. Swiss National Science Foundation (SNF) [P2EZP2_181599] Funding Source: Swiss National Science Foundation (SNF)

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Atmospheric gas-to-particle conversion plays a crucial role in haze formation in Chinese megacities, with over 65% of haze particles resulting from new particle formation. Reducing the subsequent growth rate of newly formed particles can delay haze episodes and improve air quality.
Atmospheric gas-to-particle conversion is a crucial or even dominant contributor to haze formation in Chinese megacities in terms of aerosol number, surface area and mass. Based on our comprehensive observations in Beijing during 15 January 2018-31 March 2019, we are able to show that 80-90% of the aerosol mass (PM2.5) was formed via atmospheric reactions during the haze days and over 65% of the number concentration of haze particles resulted from new particle formation (NPF). Furthermore, the haze formation was faster when the subsequent growth of newly formed particles was enhanced. Our findings suggest that in practice almost all present-day haze episodes originate from NPF, mainly since the direct emission of primary particles in Beijing has considerably decreased during recent years. We also show that reducing the subsequent growth rate of freshly formed particles by a factor of 3-5 would delay the buildup of haze episodes by 1-3 days. Actually, this delay would decrease the length of each haze episode, so that the number of annual haze days could be approximately halved. Such improvement in air quality can be achieved with targeted reduction of gas-phase precursors for NPF, mainly dimethyl amine and ammonia, and further reductions of SO2 emissions. Furthermore, reduction of anthropogenic organic and inorganic precursor emissions would slow down the growth rate of newly-formed particles and consequently reduce the haze formation.

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