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Terpenylic Acid and Related Compounds from the Oxidation of α-Pinene: Implications for New Particle Formation and Growth above Forests

机译:萜烯酸和α-P烯氧化的相关化合物:对森林上方新颗粒形成和生长的影响

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摘要

Novel secondary organic aerosol (SOA) products from the monoterpene α-pinene with unique dimer-forming properties have been identified as lactone-containing terpenoic acids, i.e., terpenylic and 2-hydroxyterpenylic acid, and diaterpenylic acid acetate. The structural characterizations were based on the synthesis of reference compounds and detailed interpretation of mass spectral data. Terpenylic acid and diaterpenylic acid acetate are early oxidation products generated upon both photooxidation and ozonolysis, while 2-hydroxyterpenylic acid is an abundant SOA tracer in ambient fine aerosol that can be explained by further oxidation of terpenylic acid. Quantum chemical calculations support that noncovalent dimer formation involving double hydrogen bonding interactions between carboxyl groups of the monomers is energetically favorable.rnThe molecular properties allow us to explain initial particle formation in laboratory chamber experiments and are suggested to play a role in new particle formation and growth above forests, a natural phenomenon that has fascinated scientists for more than a century.
机译:具有独特的二聚体形成特性的单萜α-pine烯的新颖的第二有机气溶胶(SOA)产物已被鉴定为含内酯的萜烯酸,即萜烯酸和2-羟基萜烯酸,以及二萜烯基乙酸酯。结构表征是基于参考化合物的合成和质谱数据的详细解释。萜烯酸和乙酸二戊二烯基乙酸酯是在光氧化和臭氧分解中均产生的早期氧化产物,而2-羟基萜烯酸是环境精细气溶胶中大量的SOA示踪剂,这可以通过萜烯酸的进一步氧化来解释。量子化学计算证明,涉及单体羧基之间双氢键相互作用的非共价二聚体形成在能量上是有利的。分子性质使我们能够解释实验室室内实验中的初始颗粒形成,并建议其在新的颗粒形成和生长中发挥作用森林上方的自然现象吸引了一个多世纪的科学家。

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  • 来源
    《Environmental Science & Technology》 |2009年第18期|6976-6982|共7页
  • 作者单位

    Departments of Pharmaceutical Sciences and Chemistry, University of Antwerp, BE-2610 Antwerp, Belgium;

    Leibniz-Institut fuer Troposphdrenforschung (IfT), D-04318 Leipzig, Germany;

    Departments of Pharmaceutical Sciences and Chemistry, University of Antwerp, BE-2610 Antwerp, Belgium;

    Departments of Chemistry, California Institute of Technology (Caltech), Pasadena, California 91125;

    Departments of Chemistry, University of Antwerp, BE-2610 Antwerp, Belgium;

    Departments of Chemistry, University of Antwerp, BE-2610 Antwerp, Belgium;

    Leibniz-Institut fuer Troposphaerenforschung (IfT), D-04318 Leipzig, Germany;

    Leibniz-Institut fuer Troposphaerenforschung (IfT), D-04318 Leipzig, Germany Eidgenoessische Technische Hochschule Zuerich, Institute for Atmospheric and Climate Science, Universitaetstrasse 16, CH-8092 Zuerich, Switzerland;

    Departments of Pharmaceutical Sciences, University of Antwerp, BE-2610 Antwerp, Belgium;

    Departments of Pharmaceutical Sciences, University of Antwerp, BE-2610 Antwerp, Belgium;

    Departments of Pharmaceutical Sciences, University of Antwerp, BE-2610 Antwerp, Belgium;

    Departments of Chemistry, California Institute of Technology (Caltech), Pasadena, California 91125;

    Departments of Chemical Engineering, California Institute of Technology (Caltech), Pasadena, California 91125;

    Leibniz-Institut fuer Troposphaerenforschung (IfT), D-04318 Leipzig, Germany;

    Departments of Chemical Engineering, California Institute of Technology (Caltech), Pasadena, California 91125 Departments of Environmental Science and Engineering, California Institute of Technology (Caltech), Pasadena, California 91125;

    Department of Analytical Chemistry, Institute for Nuclear Sciences, Ghent University, BE-9000 Gent, Belgium;

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