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长三角城郊冬夏PM2.5中铵盐的形成过程及来源解析
摘要点击 2553  全文点击 785  投稿时间:2022-12-29  修订日期:2023-03-01
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中文关键词  PM2.5  气溶胶铵盐  稳定同位素技术  δ15N-NH4+  源解析
英文关键词  PM2.5  aerosol ammonium  sable isotope technology  δ15N-NH4+  source apportionment
作者单位E-mail
项妍琨 南京信息工程大学应用气象学院, 南京 210044
南京信息工程大学大气环境中心, 教育部气候与环境变化国际合作联合实验室, 南京 210044 
xyk6688@126.com 
曹芳 南京信息工程大学应用气象学院, 南京 210044
南京信息工程大学大气环境中心, 教育部气候与环境变化国际合作联合实验室, 南京 210044 
caofangle@163.com 
张雯淇 南京信息工程大学应用气象学院, 南京 210044
南京信息工程大学大气环境中心, 教育部气候与环境变化国际合作联合实验室, 南京 210044
浙江省宁波市气象台, 宁波 315012 
 
范美益 南京信息工程大学应用气象学院, 南京 210044
南京信息工程大学大气环境中心, 教育部气候与环境变化国际合作联合实验室, 南京 210044 
 
章炎麟 南京信息工程大学应用气象学院, 南京 210044
南京信息工程大学大气环境中心, 教育部气候与环境变化国际合作联合实验室, 南京 210044 
 
中文摘要
      气溶胶铵盐(p-NH4+)作为大气气溶胶细颗粒物(PM2.5)中主要的二次无机气溶胶(SIAs)污染物,在灰霾形成过程中起重要作用.然而对于大气中NHx(p-NH4+和NH3)各潜在来源的贡献仍存在争议.分别于2015年冬季和夏季在苏州东山半岛采集了3 h高频大气气溶胶PM2.5样品,测定总氮(TN)和p-NH4+的质量浓度及其δ15N同位素比值,并结合贝叶斯模型(SIAR)模拟,定量解析了PM2.5中铵盐的生成过程和来源.结果表明,在冬夏两季SO42-、NO3-和NH4+均为主要的水溶性离子,占比总和超过70%.PM2.5、TN和p-NH4+质量浓度变化趋势一致,且冬季均是夏季的2~3倍.δ15N-NH4+值在冬季和夏季均与浓度呈正比,然而冬季整体(-1.7‰±4.3‰)却比夏季整体(7.8‰±5.9‰)更低,这表明每个季节内δ15N-NH4+值的变化是由于不同潜在来源的贡献率不同造成的,而冬夏两季δ15N-NH4+值的差异则主要是由于铵-氨气粒分配时的氮同位素分馏导致的.SIAR溯源结果显示,非农业来源是东山地区p-NH4+主导来源,冬季贡献率为59%,夏季贡献率为69%,相较于农业来源挥发形成的NH3,化石燃料燃烧生成的NH3更易于在大气中生成气溶胶铵盐.
英文摘要
      As the main pollutants of secondary inorganic aerosols(SIAs) in fine particulate matter(PM2.5), aerosol ammonium(p-NH4+) plays a significant role in the formation of haze. However, the contribution ratio of each potential source of atmospheric NHx(p-NH4+ and NH3) still remains controversial. In this study, 3 h high-frequency PM2.5 samples were collected in Dongshan, Suzhou during winter and summer in 2015, respectively. Meanwhile, we determined concentrations and δ15N isotope ratios of total nitrogen(TN) and p-NH4+ and quantitatively analyzed formation processes and sources of p-NH4+ based on the Bayesian mixing model(SIAR). SO42-, NO3-, and NH4+ were the main water-soluble ions(WSIs) both in winter and summer, accounting for more than 70% in general. The concentration change trends of PM2.5, TN, and p-NH4+ were consistent, and the concentrations in winter were 2-3 times those in summer. The δ15N-NH4+ value was in direct proportion to the p-NH4+ concentration both in winter and summer. However, δ15N-NH4+ values in winter(-1.7‰±4.3‰) were lower than those in summer(7.8‰±5.9‰). This indicated that the differences in δ15N-NH4+ were caused by different contribution rates of each potential source within each season, whereas it was mainly led by nitrogen isotope fractionation during ammonium-ammonia gas particle distribution in different seasons. The SIAR model calculated that non-agricultural sources were the dominant source of p-NH4+ in Dongshan, with the contribution rate of 59% in winter and 69% in summer, which indicated that NH3 emitted by fossil fuel combustion more easily formed particle aerosol ammonium than that volatilized from agricultural sources.

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