Haze caused by NO oxidation under restricted residential and industrial activities in a mega city in the south of North China Plain.

The formation of secondary aerosol species, including nitrate and sulfate, induces severe haze in the North China Plain. However, despite substantial reductions in anthropogenic pollutants due to severe restriction of residential and industrial activities in 2020 to stop the spread of COVID-19, haze still formed in Zhengzhou. We compared ionic compositions of PM during the period of the restriction with that immediately before the restriction and in the comparison period in 2019 to investigate the processes that caused the haze. The average concentration of PM was 83.9 μg m in the restriction period, 241.8 μg m before the restriction, and 94.0 μg m in 2019. Nitrate was the largest contributor to the PM in all periods, with an average mass fraction of 24%-30%. The average molar concentration of total nitrogen compounds (NO + nitrate) was 0.89 μmol m in the restriction period, which was much lower than that in the non-restriction periods (1.85-2.74 μmol m). In contrast, the concentration of sulfur compounds (SO + sulfate) was 0.34-0.39 μmol m in all periods. The conversion rate of NO to nitrate (NOR) was 0.35 in the restriction period, significantly higher than that before the restriction (0.26) and in 2019 (0.25). NOR was higher with relative humidity in 40-80% in the restriction period than in the other two periods, whereas the conversion rate of SO to sulfate did not, indicating nitrate formation was more efficient during the restriction. When O occupied more than half of the oxidants (O = O + NO), NOR increased rapidly with the ratio of O to O and was much higher in the daytime than nighttime. Therefore, haze in the restriction period was caused by increased NO-to-nitrate conversion driven by photochemical reactions.