EGU25-14854, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-14854
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 28 Apr, 16:15–18:00 (CEST), Display time Monday, 28 Apr, 14:00–18:00
 
Hall X5, X5.96
Contributions of Anthropogenic Chlorine Emissions to secondary pollutions in China
Ao Shen, Yiming Liu, and Qi Fan
Ao Shen et al.
  • Sun Yat-sen University, School of Atmospheric Sciences, Zhuhai, China (shenao7@mail.sysu.edu.cn)

Chlorine species play a crucial role as precursors to Cl radicals, which can significantly impact the atmospheric oxidation capacity and influence the levels of trace gases related to climate and air quality. We developed The Anthropogenic Chlorine Emission Inventory for China (ACEIC), which was the first chlorine emission inventory for China based on local data, and explored the impact of chlorine species emissions on secondary pollutants in 2019 in China using the CMAQ model. Considering chlorine emissions, the concentration of chlorine radicals (Cl·) in China increased by about 1000 molecules/cm3 on average, with a maximum increase of more than 6000 molecules/cm3 in major cities. Cl2 and HOCl emissions were the most important contributors to the increase of Cl·, with both Cl2 and HOCl emissions originating mainly from the residential sector. Regarding monthly variation, the increase in Cl· was most significant in summer due to intensified human activities. Regarding daily variation, the increase in Cl· peaked around 9 am and decreased to zero at night. Process analyses showed that the main reactions affecting the change in Cl· were the photolysis reactions of Cl2 and HOCl and the consumption reactions of Cl· and VOCs. As an important precursor of Cl·, the concentration of Nitryl chloride (ClNO2) in China increased by about 50 ppt on average, with a maximum increase of more than 150 ppt in major cities. HCl and fine particulate Cl- emissions were the most important contributors to the increase of ClNO2. The increase in ClNO2 was most significant in winter, peaked around 6 am and decreased to zero at daytime. Process analysis identified the upper boundary layer as the critical region for ClNO2 formation. Chlorine emissions caused some increase in O3 concentration. Maximum Daily 8-hour Average O3 (MDA8 O3) concentration increased by about 1 ppb, with O3 increasing much higher in winter than in summer. In the daily variation, the ozone increase was most significant at 12 am, with a maximum increase of more than 1.5 ppb. These findings highlight the significant contribution of chlorine emissions to secondary pollutants and can aid in the formulation of emission control strategies to mitigate secondary pollution in China.

How to cite: Shen, A., Liu, Y., and Fan, Q.: Contributions of Anthropogenic Chlorine Emissions to secondary pollutions in China, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-14854, https://doi.org/10.5194/egusphere-egu25-14854, 2025.