TY - JOUR
T1 - Important contribution of N2O5 hydrolysis to the daytime nitrate in Xi'an, China during haze periods
T2 - Isotopic analysis and WRF-Chem model simulation
AU - Wu, Can
AU - Liu, Lang
AU - Wang, Gehui
AU - Zhang, Si
AU - Li, Guohui
AU - Lv, Shaojun
AU - Li, Jianjun
AU - Wang, Fanglin
AU - Meng, Jingjing
AU - Zeng, Ying
N1 - Publisher Copyright:
© 2021 Elsevier Ltd
PY - 2021/11/1
Y1 - 2021/11/1
N2 - Nitrate, as one of the major components of tropospheric aerosols, plays a crucial role in winter haze formation. While, the formation mechanism of the high production of nitrate in Chinese megacities is still not fully understood. To quantify the contributions of major formation pathways to nitrate, airborne particles in Xi'an, inland China during the winter of 2017 were measured and analyzed for the water-soluble ions and stable nitrogen/oxygen isotope compositions of nitrate in PM2.5, followed by a WRF-Chem model simulation. The oxygen isotopic results indicated that N2O5 hydrolysis was an important formation pathway for the daytime nitrate in the haze episodes. The model simulation further revealed that N2O5 hydrolysis contribution increased from 8.2% to 20.5% of the total nitrate over 14:00–16:00 p.m., clearly showing that N2O5 formation followed by a heterogeneous hydrolysis to nitrate can effectively proceed in daytime under the abundantly co-existing O3, NO2 and NH3 conditions.
AB - Nitrate, as one of the major components of tropospheric aerosols, plays a crucial role in winter haze formation. While, the formation mechanism of the high production of nitrate in Chinese megacities is still not fully understood. To quantify the contributions of major formation pathways to nitrate, airborne particles in Xi'an, inland China during the winter of 2017 were measured and analyzed for the water-soluble ions and stable nitrogen/oxygen isotope compositions of nitrate in PM2.5, followed by a WRF-Chem model simulation. The oxygen isotopic results indicated that N2O5 hydrolysis was an important formation pathway for the daytime nitrate in the haze episodes. The model simulation further revealed that N2O5 hydrolysis contribution increased from 8.2% to 20.5% of the total nitrate over 14:00–16:00 p.m., clearly showing that N2O5 formation followed by a heterogeneous hydrolysis to nitrate can effectively proceed in daytime under the abundantly co-existing O3, NO2 and NH3 conditions.
KW - Aerosol liquid water content (ALWC)
KW - Ammonia
KW - NO andO
KW - Nitrate
KW - PM
UR - https://www.scopus.com/pages/publications/85109425615
U2 - 10.1016/j.envpol.2021.117712
DO - 10.1016/j.envpol.2021.117712
M3 - 文章
C2 - 34246996
AN - SCOPUS:85109425615
SN - 0269-7491
VL - 288
JO - Environmental Pollution
JF - Environmental Pollution
M1 - 117712
ER -