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

AI Article Synopsis

  • Atmospheric reactions during haze days contribute to 80-90% of aerosol mass in Beijing, with over 65% of haze particles originating from new particle formation (NPF).
  • Haze formation accelerates when the growth of newly formed particles is enhanced, indicating that nearly all haze episodes stem from NPF due to declines in primary particle emissions in recent years.
  • Reducing the growth rate of fresh particles can delay haze buildup by 1-3 days and potentially halve the annual number of haze days, achievable by targeting specific gas-phase precursors like dimethyl amine, ammonia, and sulfur oxides.

Article Abstract

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 (PM) 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 SO 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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Source
http://dx.doi.org/10.1039/d0fd00078gDOI Listing

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