天津大氣氣溶膠化學組分的粒徑分布和垂直分布
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中國氣象局北京區域氣象中心科技創新基金項目(BRMCCX200604)、北京城市氣象基金資助項目(UMF200607)、天津市氣象局科技培育攻關項目(KJPY0703)共同資助


Size Distribution and Vertical Variation of Atmospheric Aerosol in Tianjin
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    摘要:

    2006年8月在天津氣象鐵塔的10、120、220 m 3個不同高度,利用Andersen分級采樣器同步進行大氣氣溶膠采樣,樣品用離子色譜和電感耦合等離子體質譜儀進行分析。結果表明, K元素主要集中在細粒子,Mg、Ca、Al、Fe元素主要集中在粗粒子,Na元素則具有雙峰結構;總離子濃度隨著高度的升高有增加的趨勢,SO2-4、NO-3、NH+4、Ca2+是最主要的水溶性無機離子;二次源是水溶性離子重要的貢獻源, NO-3、SO2-4、NH+4隨著高度升高,濃度有向小粒徑集中的趨勢;各層氣溶膠陰陽離子平衡值小于1,表明氣溶膠偏堿性,與天津地處北方,土壤偏堿性,且非采暖期地面揚塵是主要的氣溶膠來源有關;各層NO-3/SO2-4平均值為0.48,表明非采暖期固定排放源(燃煤)仍然是天津大氣細粒子中水溶性離子的主要來源。

    Abstract:

    The sampling was conducted simultaneously in August 2006 at the levels of 10,120,220 m of the 255 m meteorological tower in Tianjin with the Andersen cascade sampler. The atmospheric aerosol samples are analyzed by IC (Ion Chromatograph) and ICP/MS (Inductively Coupled Plasma Mass Spectrometer). The results indicate that there are three types of size distribution: (1) K particles are mainly in the fine particle section with the peak at 0.43 to 2.1 μm. (2) Mg, Ca, Al, Fe are mainly in the coarse particle section with the peak at 2.1 to 9.0 μm. (3) Na particle distribution exhibits a doublepeak structure with the peaks at 0.65 to 2.1 μm and 3.3 to 5.8 μm. SO2-4, NO-3,NH+4 and Ca2+ are mainly watersoluble ions,which occupy 17.6%,45.7%,18.1% and 13.7% in the total ions,respectively.The total concentration of ion, as well as NO-,3 SO2-4 and NH+4, increases with height. The ion balance values between total cations and total anions at various levels are less than one, which indicates that the aerosol is slightly alkaline, can attributed to the soil properties of Tianjin. The mean concentration ratio of NO-3 to SO2-4 is 0.48,indicating that coal burning,which represents the stationary sources, compared to the mobile sources of vehicle emission,is the main pollution sources of watersoluble ions in Tianjin.

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姚青,孫玫玲,張長春,穆懷斌.天津大氣氣溶膠化學組分的粒徑分布和垂直分布[J].氣象科技,2008,36(6):692~696

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  • 收稿日期:2008-01-05
  • 定稿日期:2008-08-28
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