Identification of ozone sensitivity for NO2 and secondary HCHO based on MAX-DOAS measurements in northeast China

被引:31
作者
Xue, Jiexiao [1 ]
Zhao, Ting [1 ]
Luo, Yifu [1 ]
Miao, Congke [1 ]
Su, Pinjie [1 ]
Liu, Feng [1 ]
Zhang, Guohui [1 ]
Qin, Sida [2 ]
Song, Youtao [1 ]
Bu, Naishun [1 ,3 ]
Xing, Chengzhi [4 ]
机构
[1] Liaoning Univ, Sch Environm Sci, Shenyang 110036, Peoples R China
[2] Liaoning Sci & Technol Ctr Ecol & Environm Protec, Shenyang 110161, Peoples R China
[3] Harbin Univ, Key Lab Wetland Ecol & Environm Res Cold Reg Heil, Harbin 150086, Peoples R China
[4] Chinese Acad Sci, Anhui Inst Opt & Fine Mech, Hefei Inst Phys Sci, Key Lab Environm Opt & Technol, Hefei 230031, Peoples R China
基金
美国国家科学基金会;
关键词
MAX-DOAS; Formaldehyde; Secondary source; HCHO/NO2; Ozone production sensitivity; ABSORPTION CROSS-SECTIONS; AEROSOL OPTICAL-PROPERTIES; VOLATILE ORGANIC-COMPOUNDS; AMBIENT FORMALDEHYDE; TROPOSPHERIC NO2; CARBONYL-COMPOUNDS; RIVER DELTA; VERTICAL DISTRIBUTIONS; STATISTICAL-ANALYSIS; MEXICO-CITY;
D O I
10.1016/j.envint.2021.107048
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this study, tropospheric formaldehyde (HCHO) vertical column densities (VCDs) were measured using multiaxis differential optical absorption spectroscopy (MAX-DOAS) from January to November 2019 in Shenyang, Northeast China. The maximum HCHO VCD value appeared in the summer (1.74 x 10(16) molec/cm(2)), due to increased photo-oxidation of volatile organic compounds (VOCs). HCHO concentrations increased from 08:00 and peaked near 13:00, which was mainly attributed to the increased release of isoprene from plants and enhanced photolysis at noon. The HCHO VCDs observed by MAX-DOAS and OMI have a good correlation coefficient (R) of 0.78, and the contributions from primary and secondary HCHO sources were distinguished by the multi-linear regression model. The anthropogenic emissions showed unobvious seasonal variations, and the primary HCHO was relatively stable in Shenyang. Secondary HCHO contributed 82.62%, 83.90%, 78.90%, and 41.53% to the total measured ambient HCHO during the winter, spring, summer, and autumn, respectively. We also found a good correlation (R = 0.78) between enhanced vegetation index (EVI) and HCHO VCDs, indicating that the oxidation of biogenic volatile organic compounds (BVOCs) was the main source of HCHO. The ratio of secondary HCHO to nitrogen dioxide (NO2) was used as the tracer to analyze O-3-NOx-VOC sensitivities. We found that the VOC-limited, VOC-NOx-limited, and NOx-limited regimes made up 93.67%, 6.23%, 0.11% of the overall measurements, respectively. In addition, summertime ozone (O-3) sensitivity changed from VOC-limited in the morning to VOC-NOx-limited in the afternoon. Therefore, this study offers information on HCHO sources and corresponding O-3 production sensitivities to support strategic management decisions.
引用
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页数:10
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