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Two years of online measurement of fine particulate nitrate in the western Yangtze River Delta: influences of thermodynamics and Nsub2/subOsub5/sub hydrolysis

机译:长江三角洲近两年在线细颗粒硝酸盐在线测量:热力学和N 2 O 5 水解的影响

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Particulate nitrate contributes a large fraction of secondary aerosols. Despite understanding of its important role in regional air quality and global climate, long-term continuous measurements are rather limited in China. In this study, we conducted online measurement of PM sub2.5/sub (particulate matter with diameters less than 2.5 μm ) nitrate for 2 years from March?2014 to February?2016 using the Monitor for AeRosols and Gases in ambient Air (MARGA) in the western Yangtze River Delta (YRD), eastern China, and investigate the main factors that influenced its temporal variations and formation pathways. Compared to other sites in China, an overall high concentration of particulate nitrate was observed, with a mean value of 15.8 μg?msup?3/sup (0.5 to 92.6 μg?msup?3/sup ). Nitrate on average accounted for 32?% of the total mass of water-soluble ions and the proportion increased with PM loading, indicating that nitrate is a major driver of haze pollution episodes in this region. Sufficient ammonia drove most nitrate into the particle phase in the form of ammonium nitrate. A typical seasonal cycle of nitrate was observed, with the concentrations in winter on average 2 times higher than those in summer mainly due to different meteorological conditions. In summer, the diurnal variation of particulate nitrate was determined by thermodynamic equilibrium, resulting in a much lower concentration during daytime despite a considerable photochemical production. Air masses from the polluted YRD and biomass burning region contributed to the high nitrate concentration during summer. In winter, particulate nitrate did not reveal an evident diurnal variation. Regional transport from northern China played an important role in enhancing nitrate concentration. A total of 18 nitrate episodes were selected to understand the processes that drive the formation of high concentration of nitrate. Rapid nitrate formation was observed during the pre-episode (the day before nitrate episode day) nights, and dominated the increase of total water-soluble ions. Calculated nitrate from Nsub2/subOsub5/sub hydrolysis was highly correlated to and accounted for 80?% of the observed nitrate, suggesting that Nsub2/subOsub5/sub hydrolysis was a major contributor to the nitrate episodes. Our results suggested that rapid formation of nitrate could be a main cause for extreme aerosol pollution events in the YRD during winter, and illustrated the urgent need to control NOsubx/sub emission.
机译:硝酸盐颗粒占第二气溶胶的很大一部分。尽管了解其在区域空气质量和全球气候中的重要作用,但在中国,长期连续测量相当有限。在这项研究中,我们使用环境空气中的气溶胶和气体监测仪从2014年3月至2016年2月进行了为期2年的在线测量PM 2.5 (直径小于2.5μm的微粒)硝酸盐中国东部长江三角洲(YRD)的海星(MARGA),并研究了影响其时间变化和形成途径的主要因素。与中国其他地区相比,总体上硝酸盐颗粒浓度很高,平均值为15.8μg?m ?3 (0.5至92.6μg?m ?3 )。硝酸盐平均占水溶性离子总量的32%,并且该比例随PM含量的增加而增加,表明硝酸盐是该地区雾霾污染发作的主要驱动力。足够的氨将大多数硝酸盐以硝酸铵的形式驱使进入颗粒相。观察到典型的硝酸盐季节循环,冬季的平均浓度比夏季平均高2倍,这主要是由于不同的气象条件。在夏季,通过热力学平衡确定了硝酸盐颗粒的日变化,尽管产生了大量光化学产物,但白天的浓度却低得多。夏季,来自受污染的长三角和生物质燃烧区的空气团促成了高硝酸盐浓度。在冬季,硝酸盐颗粒没有显示出明显的昼夜变化。来自中国北方的区域运输在提高硝酸盐浓度方面发挥了重要作用。总共选择了18次硝酸盐发作以了解驱动高浓度硝酸盐形成的过程。在前期(硝酸盐发生前一天)的夜晚观察到硝酸盐的快速形成,并主导了总水溶性离子的增加。由N 2 O 5 水解计算得出的硝酸盐与所观察到的硝酸盐高度相关,占80%,表明N 2 O < sub> 5 水解是造成硝酸盐发作的主要因素。我们的研究结果表明硝酸盐的快速形成可能是冬季长三角地区极端气溶胶污染事件的主要原因,并说明了控制NO x 排放的迫切需要。

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