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西安市PM2.5中水溶性离子的季节变化特征
摘要点击 2109  全文点击 673  投稿时间:2019-10-15  修订日期:2020-01-10
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中文关键词  PM2.5  水溶性阴阳离子  二次转化率  存在形式  污染特征
英文关键词  PM2.5  water soluble anion and cation  secondary conversion rate  existing form  pollution characteristics
作者单位E-mail
黄含含 陕西科技大学环境科学与工程学院, 西安 710021 huanghanhan1996@163.com 
王羽琴 陕西科技大学环境科学与工程学院, 西安 710021 wangyuqin@sust.edu.cn 
李升苹 陕西科技大学环境科学与工程学院, 西安 710021  
陈庆彩 陕西科技大学环境科学与工程学院, 西安 710021  
中文摘要
      为探究西安市大气PM2.5中水溶性离子的污染特征及来源,本研究采集2017~2018年的PM2.5样品,利用离子色谱仪测定9种水溶性离子(SO42-、NO3-、Cl-、F-、Na+、Mg2+、NH4+、K+和Ca2+)的浓度水平,并对NH4+的存在形式分析、氮氧化率(NOR)、硫氧化率(SOR)以及[NO3-]/[SO42-]等进行探究.结果表明,西安市PM2.5中水溶性离子主要来自扬尘、燃煤、生物质燃烧和二次生成.Ca2+、SO42-、NH4+和NO3-是西安市大气PM2.5中主要的水溶性离子.相关性分析结果表明,西安市春季NH4+不能完全中和SO42-,未中和的SO42-主要与K+和Ca2+结合;夏季NH4+主要以NH4HSO4和(NH42SO4的形式存在于大气中;秋季的NH4+主要以NH4HSO4和NH4NO3的形式存在;冬季大气中NH4+多以(NH42SO4和NH4NO3的形式存在.硫氧化率和氮氧化率的年均值分别为0.35和0.16,说明研究期间SO42-、NO3-的二次生成率较大.[NO3-]/[SO42-]比值说明西安市春夏季主要受固定源影响,秋冬季主要受移动源影响.
英文摘要
      To explore the seasonal variations and sources of water-soluble ions, PM2.5 samples were collected from 2017 to 2018. Water-soluble ions including SO42-, NO3-, Cl-, F-, Na+, Mg2+, NH4+, K+, and Ca2+ were determined via ion chromatography. Furthermore, the existing form of NH4+, nitrogen oxidation rate (NOR), sulfur oxidation rate (SOR), and [NO3-]/[SO42-] ratio were explored. The results showed that dust, coal combustion, biomass burning, and secondary aerosols were the dominant contributors to water-soluble ions. Ca2+, SO42-, NH4+, and NO3- were the main water-soluble ions in PM2.5 in Xi'an. Correlation analysis results showed that NH4+ could not completely neutralize SO42- in spring; unneutralized SO42- could be mainly combined with K+ and Ca2+. NH4+ mainly existed in the form of ① NH4HSO4 and (NH4)2SO4 in summer; ② NH4HSO4 and NH4NO3 in autumn; and ③ (NH4)2SO4 and NH4NO3 in winter. The yearly mean values of SOR and NOR were 0.35 and 0.16, respectively, indicating a high secondary aerosol transformation rate during the study period. The [NO3-]/[SO42-] ratio showed Xi'an was mainly affected by stationary sources in spring and summer, while the contribution of mobile sources in autumn and winter was greater than stationary sources.

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