Preprints
https://doi.org/10.5194/egusphere-2025-131
https://doi.org/10.5194/egusphere-2025-131
05 Mar 2025
 | 05 Mar 2025
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Carbonyl compounds from typical combustion sources: emission characteristics, influencing factors, and their contribution to ozone formation

Yanjie Lu, Xinxin Feng, Yanli Feng, Minjun Jiang, Yu Peng, Tian Chen, and Yingjun Chen

Abstract. Combustion sources are the important primary emission sources of carbonyl compounds (CCs), yet the emission factors (EFs) and influencing factors for CCs in different sources remain unclear. The emission characteristics, influencing factors, and ozone formation potentials (OFPs) of CCs from four combustion sources, including biomass burning (BB), residential coal combustion (RCC), on-road sources, and agricultural machinery (AM), were investigated by field measurements. Results indicate that the EFCCs from four combustion sources exhibit significant differences. Specifically, the EFs from BB (1968.2±661.2 mg/kg) are significantly higher than other sources, being an order of magnitude greater than the on-road sources (117.8±78.3~576.3±47.4 mg/kg). Fuel types is key factors affecting the CCs components. BB primarily emit formaldehyde and acetaldehyde (F+A), accounting for 80 % of CCs, whereas RCC exhibits a higher proportion of aromatic aldehydes and acetone (26.0 %). The addition of ethanol in on-road sources and biodiesel in AM effectively promotes the formation of acetaldehyde (67.9 %) and unsaturated aldehydes (20.4 %), respectively. The formation of CCs in solid and liquid fuel sources is more sensitive to combustion temperature and emission standards, respectively. Higher combustion temperature and stricter emission standards can reduce CCs emissions by 94.6 % in solid fuels and by 61.3 % in liquid fuel, respectively. High-temperature promotes small molecules like F+A tend to cyclize, supplying ample precursors for the formation of acetone and aromatic aldehydes. More attention should be paid to the OFPs of CCs from BB and AM to allevite the oxidizing capacity of regional atmospheres.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Share
Yanjie Lu, Xinxin Feng, Yanli Feng, Minjun Jiang, Yu Peng, Tian Chen, and Yingjun Chen

Status: open (until 16 Apr 2025)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-131', Anonymous Referee #1, 14 Mar 2025 reply
    • AC1: 'Reply on RC1', Yingjun Chen, 17 Mar 2025 reply
  • RC2: 'Comment on egusphere-2025-131', Anonymous Referee #2, 17 Mar 2025 reply
Yanjie Lu, Xinxin Feng, Yanli Feng, Minjun Jiang, Yu Peng, Tian Chen, and Yingjun Chen
Yanjie Lu, Xinxin Feng, Yanli Feng, Minjun Jiang, Yu Peng, Tian Chen, and Yingjun Chen

Viewed

Total article views: 132 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
106 20 6 132 8 2 2
  • HTML: 106
  • PDF: 20
  • XML: 6
  • Total: 132
  • Supplement: 8
  • BibTeX: 2
  • EndNote: 2
Views and downloads (calculated since 05 Mar 2025)
Cumulative views and downloads (calculated since 05 Mar 2025)

Viewed (geographical distribution)

Total article views: 139 (including HTML, PDF, and XML) Thereof 139 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 18 Mar 2025
Download
Short summary
The EFs of CCs from biomass burning (BB) is an order of magnitude higher than that from on-road sources. Fuel type determines the emission characteristics and composition of CCs. The formation of CCs from solid and liquid fuel sources is respectively controlled by combustion temperature and emission standards. In addition, biomass burning and agricultural machinery sources significantly contribute to the oxidizing capacity of regional atmospheres.
Share