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    請使用永久網址來引用或連結此文件: https://ir.cnu.edu.tw/handle/310902800/2391


    標題: 大氣次微米微粒衍生性二元酸之生成及粒徑分布變異探討(II)
    Formation and size distributions of secondary dicarboxylic acids in atmospheric submicro aerosols (II)
    作者: 蔡瀛逸
    貢獻者: 環境工程與科學系
    關鍵字: 大氣氣膠
    二元有機酸
    軌跡模式
    atmospheric aerosol
    dicarboxylic acids
    trajectory model
    日期: 2005
    上傳時間: 2008-07-31 14:37:45 (UTC+8)
    出版者: 台南縣:嘉南藥理科技大學環境工程與科學系
    摘要: 本研究探討台南郊區之大氣氣膠無機鹽
    類及二元有機酸之組成特性變異,結果顯示台
    南郊區夏季及秋季氣膠無機鹽類濃度均以
    SO4
    2-、NO3
    -及NH4
    +光化產物為最大量,而秋
    季高污染時期氣膠NO3
    ->SO4
    2-,與在夏季與秋
    季非高污染時期為SO4
    2->NO3
    -不同,且氣膠
    NO3
    - 濃度表現在農廢燃燒時期與高污染時
    期,佔PM2.5 質量比例分別為19.6%及18.0%。
    在高污染時期氣膠二元有機酸日夜間濃度高
    低與夏季相同,依序為oxalic acid>succinic
    acid>maleic acid,然而高污染時期二元有機酸
    之濃度較夏季時期高出約2-3 倍。農廢燃燒時
    期,由主成份分析發現NH4
    +、NO3
    -、SO4
    2-、
    oxalic acid、K+和Cl-的高相關負荷,顯示二元
    有機酸之來源貢獻與光化產物相似,皆為二次
    污染;而此時期K+和Cl-之濃度佔PM2.5 質量比
    例分別為1.6%及3.3%,與秋季非高污染時期
    及秋季高染時期相比,其濃度比例明顯上升,
    且oxalic acid 與K+及Cl-的相關係數亦較其他
    空氣品質時期更高,顯示農廢燃燒時期除了
    K+與Cl-的明顯貢獻外,氣膠中亦存在來自生
    物源燃燒產生oxalic acid 的貢獻。在台南郊區
    之氣膠無機鹽類與二元有機酸組成之濃度粒
    徑分布,由夏季的單峰或雙峰,轉變成秋季的
    三峰及更多波峰的形態,高污染時的二元有機
    酸最大濃度波峰集中於0.19-0.32 µm 的
    condensation mode,顯示高污染時期氣膠有更
    明顯的二元有機酸膠凝及光化產物生成貢
    獻。此外,氣膠succinic acid (C4)及malonic acid
    (C3)之最大濃度波峰與oxalic acid (C2)不同,秋
    季非高污染時期及高污染時期之oxalic acid 最
    大濃度波峰往更小粒徑位移,顯示秋季氣膠
    oxalic acid 是經由C4和C3二元有機酸光化反應
    後之最後產物。此外,以空氣品質高斯軌跡傳
    遞係數模式(Gaussian trajectory transfercoefficient
    model, GTx)探討氣膠污染貢獻來源
    發現以面源為最大,污染來源佔35%,其次為
    點源的貢獻量佔23%,而上風邊界濃度、高空
    沉降以及線源模式則分別佔了17%、14%及
    11%,此結果對其台南空品區之管制策略可提
    供參考。
    In this research, variations of characteristic
    compositions of the atmospheric inorganic salts
    and low-molecular-weight dicarboxylic acids
    (low-Mw DCAs) for Tainan suburban regions
    were studied. During summer and autumn, SO4
    2-,
    NO3
    - and NH4
    + are the major inorganic species
    with higher NO3
    - than SO4
    2- during the autumn
    episodic period that is different from the higher
    SO4
    2- than NO3
    - during summer and the autumn
    non-serious pollution period. The NO3
    - sol mass
    constitutes 19.6% of PM2.5 mass during the
    agricultural waste burning period and 18.0%
    during the autumn episodic period. During the
    autumn episodic period, variations of the daytime
    and nighttime low-Mw DCAs concentrations are
    similar to those observed during summer with
    oxalic acid being the most abundant followed by
    succinic acid and maleic acid. However,
    concentrations of low-Mw DCAs during the
    autumn episodic period are 2 to 3 time the
    concentrations during summer. Results of
    principal component analyses reveal that during
    the agricultural waste burning period, the high
    correlation loadings between NH4
    +, NO3
    -, SO4
    2-,
    oxalic acid, K+ and Cl-, indicating that the sources
    for low-Mw DCAs are similar to those for
    photochemical products; both are considered as
    the secondary pollution. During the agricultural
    waste burning period, the concentration ratios of
    K+ and Cl- to PM2.5 mass are 1.6% and 3.3%,
    respectively, which are similar to those during
    the autumn non-serious pollution period and the
    autumn episodic period; concentrations of K+ and
    Cl- obviously increase during the agricultural
    2
    waste burning period. Oxalic acid during these
    periods is more correlated with K+ and Cl- than
    during other air quality periods demonstrating
    that in addition to K+ and Cl-, a large quantity of
    oxalic acid sol is also generated by burning
    agricultural wastes. For Tainan suburban region,
    the particle size distributions for both aerosol
    inorganic salts and low-Mw DCAs change from
    single peak or double peaks in summer to triple
    or multiple peaks in autumn. During the high
    pollution period, the maximum concentration
    peaks for low-Mw DCAs dominant in the
    condensation mode of 0.19-0.32 µm. This reveals
    that particle coagulation and photochemical
    products contribute to the observed aerosols
    during the high pollution period. Additionally,
    the aerosol succinic (C4) and malonic acids (C3)
    have different maximum concentration peaks
    from oxalic acid (C2). During the autumn
    non-serious pollution period and high pollution
    period, the maximum concentration peak for
    oxalic acid shifts toward the smaller range
    indicating that the autumn sol oxalic acid is an
    end photochemical product from C4 and C3
    low-Mw DCAs. Using the developed aerosol
    transformation mechanisms of the Gaussian
    trajectory transfer-coefficient model (GTx), the
    source apportionment reveals the most dominant
    contribution comes form area sources (35%) and
    follows by point sources (23%), upwind
    boundary sources (17%), top boundary sources
    (14%) and line sources (11%). These results
    could provide a view to applying proper and
    effective strategies for improving air quality in
    Tainan air basin.
    關聯: 計畫編號:NSC94-2211-E-041-010
    顯示於類別:[環境工程與科學系(所)] 科技部計畫

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