Molecular chlorine (Cl 2 ) and nitryl chloride (ClNO 2 ) concentrations were measured using chemical ionization mass spectrometry at a rural site over the North China Plain during June 2014. High levels of daytime Cl 2 up to ∼450 pptv were observed. The average diurnal Cl 2 mixing ratios showed a maximum around noon at ∼100 pptv. ClNO 2 exhibited a strong diurnal variation with early morning maxima reaching ppbv levels and afternoon minima sustained above 60 pptv. A moderate correlation ( R 2 = 0.31) between Cl 2 and sulfur dioxide was observed, perhaps indicating a role for power plant emissions in the generation of the observed chlorine. We also observed a strong correlation ( R 2 = 0.83) between daytime (10:00–20:00) Cl 2 and ClNO 2, which implies that both of them were formed from a similar mechanism. In addition, Cl 2 production is likely associated with a photochemical mechanism as Cl 2 concentrations varied with ozone (O 3 ) levels. The impact of Cl 2 and ClNO 2 as Cl atom sources is investigated using a photochemical box model. We estimated that the produced Cl atoms oxidized slightly more alkanes than OH radicals and enhanced the daily concentrations of peroxy radicals by 15% and the O 3 production rate by 19%.
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