中国地质学会岩矿测试技术专业委员会、国家地质实验测试中心主办

广州市大气颗粒物PM2.5显微形貌特征和来源解析

周莉, 石贵勇, 付宇, 关瑶, 陈来国. 广州市大气颗粒物PM2.5显微形貌特征和来源解析[J]. 岩矿测试, 2016, 35(3): 302-309. doi: 10.15898/j.cnki.11-2131/td.2016.03.014
引用本文: 周莉, 石贵勇, 付宇, 关瑶, 陈来国. 广州市大气颗粒物PM2.5显微形貌特征和来源解析[J]. 岩矿测试, 2016, 35(3): 302-309. doi: 10.15898/j.cnki.11-2131/td.2016.03.014
Li ZHOU, Gui-yong SHI, Yu FU, Yao Guan, Lai-guo CHEN. Preliminary Study on the Microscopic Morphology and Chemical Composition, and Its Source of PM2.5 in Guangzhou[J]. Rock and Mineral Analysis, 2016, 35(3): 302-309. doi: 10.15898/j.cnki.11-2131/td.2016.03.014
Citation: Li ZHOU, Gui-yong SHI, Yu FU, Yao Guan, Lai-guo CHEN. Preliminary Study on the Microscopic Morphology and Chemical Composition, and Its Source of PM2.5 in Guangzhou[J]. Rock and Mineral Analysis, 2016, 35(3): 302-309. doi: 10.15898/j.cnki.11-2131/td.2016.03.014

广州市大气颗粒物PM2.5显微形貌特征和来源解析

  • 基金项目:
    国家自然科学基金资助项目(41373012);广州市科信局应用基础专项节能环保项目(2013J4100115)
详细信息
    通讯作者: 石贵勇,博士,讲师,从事矿床地球化学方面的研究工作。E-mail:eessgy@mail.sysu.edu.cn
  • 中图分类号: O657.63

Preliminary Study on the Microscopic Morphology and Chemical Composition, and Its Source of PM2.5 in Guangzhou

More Information
  • PM2.5是近年来影响我国城市大气环境的首要污染物,其成因机制复杂。本文采用扫描电镜和ICP-MS研究了广州市大气颗粒物PM2.5的显微形貌及其化学组成特征,并应用富集因子法进行源解析。结果表明,PM2.5的颗粒形态以无定形态为主;主要物质表现为含Fe、Mg、Al、K、Na的硅酸盐组合,具有道路扬尘、建筑施工排放等一次粒子特征;单个无定形颗粒物能谱表现出硫酸盐+硝酸盐的组合特征,为汽车尾气所排放的前体污染气体NOx和SO2进入大气环境中,在特定的物理化学条件下通过成核作用发生相态改变所形成的二次粒子。PM2.5中高度富集Cd、Se、Zn、Cu、Pb、As等重金属,异常富集的Br主要为当地普遍使用的阻燃剂十溴联苯醚和拆解电子垃圾所致,稀土元素的浓度在0.022~0.582 ng/m3之间,具有重稀土元素富集的特征。这些特征反映出广州市PM2.5颗粒物的组成既有一次粒子,也有二次粒子,物质来源具有多重性。
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  • 图 1  扫描电镜下PM2.5二次电子形貌图

    Figure 1. 

    图 2  PM2.5能谱化学组成图

    Figure 2. 

    图 3  广州大气PM2.5中稀土元素的富集特征

    Figure 3. 

    表 1  广州市PM2.5 4件样品中44个微量元素浓度(ng/m3)

    Table 1.  The trace elements concentrations of four samples PM2.5 in Guangzhou

    元素含量最小值含量最大值含量平均值富集因子(EF)元素含量最小值含量最大值含量平均值富集因子(EF)
    Ti13.216.415.21Ba4.574.974.72-
    V1.974.813.17.24W0.4990.5910.541-
    Cr2.935.024.4315.5Hg0.0110.0340.025126
    Mn10.316.212.511.8Tl0.2380.3570.285-
    Co0.1530.3510.2335.52Pb74.993.783.3424
    Ni1.703.472.3831.5Bi4.386.404.99-
    Cu23.959.233.5533Y1.973.522.85-
    Zn196241211660Zr1.654.172.64-
    Ga1.001.211.10-La0.2800.3420.314-
    Ge0.1330.4180.235-Ce0.5190.7400.582-
    As17.635.625.4470Pr0.0420.0770.051-
    Se2.473.642.97914Nd0.1550.5460.278-
    Br120347202-Sm0.0340.3230.130-
    Rb2.252.742.43-Eu0.0070.1040.041-
    Sr0.7630.9710.859-Gd0.0590.7470.297-
    Mo1.232.301.63-Tb0.0120.1670.065-
    Cd2.693.953.209250Dy0.0671.1800.466-
    In0.0970.1290.110-Ho0.0140.2250.089-
    Sn1.302.782.07-Er0.0380.6640.271-
    Sb18.524.520.5-Tm0.0030.0850.034-
    Te0.2260.6810.381-Yb0.0330.5080.198-
    Cs0.3640.5080.413-Lu0.0040.0570.022-
    注:富集因子计算中,土壤背景值单位除Ti为%,其余为mg/kg;土壤背景值中Ti取自文献[21],其余元素取自文献[22]。富集因子栏中“-”表示无对应元素土壤背景值。
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出版历程
收稿日期:  2016-01-10
修回日期:  2016-05-15
录用日期:  2016-05-20

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