天气研究与预报模式
硝酸盐
大气科学
白天
薄雾
水解
化学
环境化学
有机化学
地质学
作者
Can Wu,Lang Liu,Gehui Wang,Si Zhang,Guohui Li,Shaojun Lv,Jianjun Li,Fanglin Wang,Jingjing Meng,Ying Zeng
标识
DOI:10.1016/j.envpol.2021.117712
摘要
Abstract 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.
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