Source apportionment and ozone formation mechanism of VOCs considering photochemical loss in Guangzhou, China.

Megacity Ozone pollution Photochemical age Volatile organic compounds (VOCs)

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
10 Dec 2023
Historique:
received: 10 04 2023
revised: 07 08 2023
accepted: 08 08 2023
pubmed: 12 8 2023
medline: 12 8 2023
entrez: 11 8 2023
Statut: ppublish

Résumé

Understanding the sources and impact of volatile organic compounds (VOCs) on ozone formation is challenging when the traditional method does not account for their photochemical loss. In this study, online monitoring of 56 VOCs was carried out in summer and autumn during high ozone pollution episodes. The photochemical age method was used to evaluate the atmospheric chemical loss of VOCs and to analyze the effects on characteristics, sources, and ozone formation of VOC components. The initial concentrations during daytime were 5.12 ppbv and 4.49 ppbv higher than the observed concentrations in the summer and autumn, respectively. The positive matrix factorization (PMF) model identified 5 major emission sources. However, the omission of the chemical loss of VOCs led to underestimating the contributions of sources associated with highly reactive VOC components, such as those produced by biogenic emissions and solvent usage. Conversely it resulted in overestimating the contributions from VOC components with lower chemical activity such as liquefied petroleum gas (LPG) usage, vehicle emissions, and gasoline evaporation. Furthermore, the estimation of ozone formation may be underestimated when the atmospheric photochemical loss is not taken into account. The ozone formation potential (OFP) method and propylene-equivalent concentration method both underestimated ozone formation by 53.24 ppbv and 47.25 ppbc, respectively, in the summer, and by 40.34 ppbv and 26.37 ppbc, respectively, in the autumn. The determination of the ozone formation regime based on VOC chemical loss was more acceptable. In the summer, the ozone formation regime changed from the VOC-limited regime to the VOC-NOx transition regime, while in the autumn, the ozone formation regime changed from the strong VOC-limited regime to the weak VOC-limited regime. To obtain more thorough and precise conclusions, further monitoring and analysis studies will be conducted in the near future on a wider variety of VOC species such as oxygenated VOCs (OVOCs).

Identifiants

pubmed: 37567293
pii: S0048-9697(23)04816-7
doi: 10.1016/j.scitotenv.2023.166191
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

166191

Informations de copyright

Copyright © 2023 Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Y Zou (Y)

School of Environment and Energy, South China University of Technology, Guangzhou 510006, China; Institute of Tropical and Marine Meteorology, China Meteorological Administration (CMA), Guangzhou 510640, China.

X L Yan (XL)

State Key Laboratory of Severe Weather & Institute of Tibetan Plateau Meteorology, Chinese Academy of Meteorological Sciences, Beijing, China.

R M Flores (RM)

Marmara University, Department of Environmental Engineering, Istanbul, Turkey.

L Y Zhang (LY)

Institute of Tropical and Marine Meteorology, China Meteorological Administration (CMA), Guangzhou 510640, China.

S P Yang (SP)

Institute of Tropical and Marine Meteorology, China Meteorological Administration (CMA), Guangzhou 510640, China.

L Y Fan (LY)

School of Environment and Energy, South China University of Technology, Guangzhou 510006, China.

T Deng (T)

Institute of Tropical and Marine Meteorology, China Meteorological Administration (CMA), Guangzhou 510640, China.

X J Deng (XJ)

Institute of Tropical and Marine Meteorology, China Meteorological Administration (CMA), Guangzhou 510640, China.

D Q Ye (DQ)

School of Environment and Energy, South China University of Technology, Guangzhou 510006, China. Electronic address: cedqye@scut.edu.cn.

Classifications MeSH