摘要
使用MARGA离子在线分析仪ADI2080对2017年12月27日~2018年1月5日南京市PM_(2.5)化学组分进行连续采样分析,结合气象要素和大气环境监测数据,探讨了霾污染过程中水溶性离子的时间分布特征及其来源特征.结果表明:霾日中南京水溶性离子浓度为121.41μg/m~3,是洁净日的3.2倍.霾污染过程中水溶性离子平均浓度大小顺序为NO_3~-> SO_4~(2-)> NH_4~+> Cl~-> K~+> Ca~(2+)> Mg~(2+),SNA离子占总水溶性离子浓度的91.97%.霾日中水溶性离子日变化均为三峰型,洁净日中Cl~-、SO_4~(2-)和NH_4~+的日变化为单峰型,Ca~(2+)为双峰型,K~+、Mg~(2+)为三峰型.随着空气污染状况的加重,总水溶性离子在PM_(2.5)中的占比不断减少,空气质量为优时占比95.93%,严重污染时为63.25%.霾日中随着污染加重,NH_4~+占总离子的比例稳定在23%左右,SO_4~(2-)占比缓慢减小,NO_3~-占比不断增大.NOR、SOR的日变化在霾日呈双峰型分布,洁净日则较为平稳.观测期间的水溶性离子主要来源有二次转化、煤烟尘、扬尘以及生物质燃烧.
The composition of PM_(2.5) was monitored online continuously by using MARGA 1 S Analyzer ADI 2080 in Nanjing from December 27, 2017 to January 5, 2018. Combined with meteorological elements and atmospheric environmental monitoring data, the time distribution and source characteristics of water-soluble ions in haze pollution process was investigated. The mass concentration of water-soluble ions in Nanjing during the haze pollution was 121.41μg/m~3, 3.2 times of the level in clean days. The order of the average mass concentration of water-soluble ions in the haze pollution process was NO_3~-> SO_4~(2-)> NH_4~+ > Cl~-> K~+ > Ca~(2+) > Mg~(2+).SO_4~(2-), NO_3~- and NH_4~+ accounted for 91.97% of the total water-soluble ions concentration. The diurnal variations of water-soluble ions in haze days were all trimodal, while in clean days, Cl~-, SO_4~(2-)and NH_4~- were unimodal, Ca~(2+) was bimodal, K~+ and Mg~(2+) were trimodal. With the aggravation of the air pollution, the proportion of total water-soluble ions in PM_(2.5) was decreasing. When the air quality was excellent, the proportion was 95.93%, while it was 63.25% when serious pollution occurred. With the increase of pollution in haze days, the proportion of NH_4~+ to total water-soluble ions was stable at around 23%, the proportion of SO_4~(2-)decreased slowly, and the proportion of NO_3~-increased continuously. The diurnal variations of NOR and SOR were bimodal in haze days, while in clear days, they were relatively stable. During the observation period, water-soluble ions were derived mainly from secondary conversion, coal ash, dust, and biomass combustion.
引文
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