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Pollution characteristics of atmospheric formaldehyde (HCHO) and its environmental effects in autumn in a coastal city |
LIN Yi-ling1,2, HONG You-wei2,3,4,5, JI Xiao-ting2,3,4, XU Ke3,4,5, SHAO Zhi-qian2,3,4, YU Rui-lian1, CHEN Jin-sheng2,3,4 |
1. College of Chemical Engineering, Huaqiao University, Xiamen 361021, China; 2. Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China; 3. Key Lab of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China; 4. Fujian Key Laboratory of Atmospheric Ozone Pollution Prevention, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China; 5. School of Life Sciences, Hebei University, Baoding 071000, China |
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Abstract The temporal variations and key influencing factors of atmospheric formaldehyde (HCHO) in autumn in the southeastern coastal city of Xiamen were investigated using online observation data of gaseous pollutants (HCHO, O3, peroxyacetyl nitrate (PAN), CO, NOx, isoprene) and the meteorological parameters (temperature, humidity, wind speed, wind direction) at an atmospheric environment supersite. The major sources of HCHO were identified quantitatively using the multilinear regression analysis method, and the contribution of HCHO to the formation of hydroxyl radical (·OH) was also estimated. It showed that the diurnal variation of HCHO displayed an obvious single-peak pattern, with the peak value appearing at around 13:00; and the concentrations of HCHO varied from 0.55×10-9 to 7.96×10-9 with an average concentration of (3.15±1.40)×10-9. Significant positive correlations between O3, PAN, and HCHO were observed. Temperature, humidity, and UV were the main meteorological factors affecting HCHO levels. Intense solar radiation, high temperature, low humidity, low wind speed, and southwest wind conditions favor the secondary formation of HCHO in Xiamen. The photolysis rate of HCHO (PHCHO) ranged from 0.01×10-9/h to 3.02×10-9/h, with a mean value PHCHO of 0.61×10-9/h. The rate of HCHO photolysis to produce stable molecules of H2 and CO was 1.1~1.6 times that of H· and HCO· free radicals. The primary sources of atmospheric HCHO in the autumn of Xiamen included secondary formations (39.2%), direct emissions (26.6%), and regional background (34.2%). During the daytime in autumn, the average ·OH formation rates from the photolysis of HONO, O3, and HCHO were 1.86×10-9/h, 1.11×10-9/h, and 0.70×10-9/h, respectively. And the production rate of OH caused by HCHO photolysis (P(OH_HCHO)) accounted for 10%~21% of the total ·OH formation rate.
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Received: 15 June 2022
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