TY - JOUR
T1 - Investigating atmospheric nitrate sources and formation pathways between heating and non-heating seasons in urban North China
AU - Yan, Xiao
AU - Hu, Beibei
AU - Li, Yilan
AU - Shi, Guitao
N1 - Publisher Copyright:
© 2023 The Author(s). Published by IOP Publishing Ltd.
PY - 2023/3/1
Y1 - 2023/3/1
N2 - 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.
AB - 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.
KW - MixSIAR
KW - heating season
KW - nitrate formation
KW - stable isotope
UR - https://www.scopus.com/pages/publications/85148723912
U2 - 10.1088/1748-9326/acb805
DO - 10.1088/1748-9326/acb805
M3 - 文章
AN - SCOPUS:85148723912
SN - 1748-9326
VL - 18
JO - Environmental Research Letters
JF - Environmental Research Letters
IS - 3
M1 - 034006
ER -