4.6 Article

The variability of volatile organic compounds during a persistent fog-haze episode

期刊

FRONTIERS IN ENVIRONMENTAL SCIENCE
卷 10, 期 -, 页码 -

出版社

FRONTIERS MEDIA SA
DOI: 10.3389/fenvs.2022.1069905

关键词

volatile organic compounds (VOCs); fog-haze transformation; extremely dense fog; wet scavenge; microphysical processes

资金

  1. National Natural Science Foundation of China
  2. Guangxi Key Research and Development Program
  3. [41675136]
  4. [41875170]
  5. [42075177]
  6. [41675132]
  7. [42075186]

向作者/读者索取更多资源

This study conducted comprehensive chemical and microphysical observations on a persistent fog-haze process in the northern suburbs of Nanjing in 2013. It compared and analyzed the characteristics and variations of volatile organic compounds (VOCs) under different weather conditions and discussed the factors influencing VOCs during extremely dense fog. The results showed that the concentration of VOCs differed significantly under different weather conditions, mainly due to the boundary layer characteristics and photochemical reaction rate. The enhanced collision and deposition of fog droplets also played a role in removing VOCs from the atmosphere.
A persistent fog-haze process associated with high pollution occurred in the northern suburbs of Nanjing from November to December 2013. Based on the comprehensive chemical and microphysical observations during the intense observation period, the composition characteristics, and variation rules of volatile organic compounds (VOCs) in the atmosphere under four weather conditions (slight haze, haze, fog, and dense fog) were compared and analyzed, the influencing factors for VOCs during extremely dense fog were discussed in more detail. The average concentrations of VOCs displayed as alkanes > aromatics > alkenes > alkynes, and their concentrations were ranked as dense fog > fog > haze > slight haze, the main factor contributing to the difference in concentrations of VOCs under different weather conditions is the boundary layer characteristics and photochemical reaction rate. Microphysical parameters such as liquid water content (LWC) were negatively correlated with VOCs concentration in dense fog (LWC > 0.008 g m(-3)). Also, the concentration of VOCs showed an oscillating decrease in extremely dense fog (LWC > 0.12 g m(-3)), and the total VOCs removal rate was close to 30%, which may be attributed to an indirect/direct removal effect, in which the enhanced collision and deposition of fog droplets promote the redistribution of VOCs gas-aqueous/particle partitioning, and remove them from the atmosphere by fog water.

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