Investigating atmospheric nitrate sources and formation pathways between heating and non-heating seasons in urban North China

  • Xiao Yan
  • , Beibei Hu*
  • , Yilan Li
  • , Guitao Shi*
  • *Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

12 Scopus citations

Abstract

In urban North China, nitrate ( NO 3 − ) is a primary contributor to haze formation. So far, the production processes and source apportionments of atmospheric NO 3 − during the heating season (i.e. the wintertime) have not yet been well understood. This study determined δ15N- NO 3 − , δ18O- NO 3 − , and Δ17O- NO 3 − of aerosol samples to compare the potential sources and formation pathways of atmospheric NO 3 − during heating (November to March) and non-heating (April to May) seasons. Combining stable isotope composition with the MixSIAR model based on Δ17O- NO 3 − showed that NO3 + DMS/HC (dimethyl sulfate/hydrocarbon) pathway was the dominant process of atmospheric nitrate formation during the heating season (mean = 52.88 ± 16.11%). During the non-heating season, the contributions of NO3 + DMS/HC (mean = 37.89 ± 13.57%) and N2O5 + H2O (mean = 35.24 ± 3.75%) pathways were comparable. We found that Δ17O- NO 3 − was negatively correlated with wind speed and positively correlated with relative humidity during the heating season, possibly associated with the sources and production of atmospheric NO 3 − . In specific, in a dust storm event, the very low Δ17O- NO 3 − is likely associated with particles from land surface. Under the premise of considering 15N fractionation, the constraint-based on δ15N- NO 3 − illustrated that coal combustion was the major source of NO x emission during the heating season, and the relative contribution of coal combustion decreased rapidly from the heating season (mean = 42.56 ± 15.50%) to the non-heating season (mean = 21.86 ± 4.91%). Conversely, the proportion of NOx emitted by soil microbes rose significantly from the heating (mean = 9.67 ± 5.99%) to non-heating season (mean = 24.02 ± 11.65%). This study revealed differences in the sources and formation processes of atmospheric NO 3 − during the heating and non-heating seasons, which are of significance to atmospheric nitrogen oxide/nitrate pollution mitigation.

Original languageEnglish
Article number034006
JournalEnvironmental Research Letters
Volume18
Issue number3
DOIs
StatePublished - 1 Mar 2023

Keywords

  • MixSIAR
  • heating season
  • nitrate formation
  • stable isotope

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