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On the fate of oxygenated organic molecules in atmospheric aerosol particles

机译:在大气气溶胶颗粒中含氧有机分子的命运

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Highly oxygenated organic molecules (HOMs) are formed from the oxidation of biogenic and anthropogenic gases and affect Earth’s climate and air quality by their key role in particle formation and growth. While the formation of these molecules in the gas phase has been extensively studied, the complexity of organic aerosol (OA) and lack of suitable measurement techniques have hindered the investigation of their fate post-condensation, although further reactions have been proposed. We report here novel real-time measurements of these species in the particle phase, achieved using our recently developed extractive electrospray ionization time-of-flight mass spectrometer (EESI-TOF). Our results reveal that condensed-phase reactions rapidly alter OA composition and the contribution of HOMs to the particle mass. In consequence, the atmospheric fate of HOMs cannot be described solely in terms of volatility, but particle-phase reactions must be considered to describe HOM effects on the overall particle life cycle and global carbon budget.
机译:高含氧有机分子(HOMS)由生物和人为气体的氧化形成,并通过其在颗粒形成和生长中的关键作用来影响地球的气候和空气质量。虽然已经广泛地研究了气相中这些分子的形成,但有机气溶胶(OA)的复杂性和缺乏合适的测量技术已经阻碍了它们的命运后凝结后的调查,尽管已经提出了进一步的反应。我们在这里报告了这些物种在粒子阶段的新型实时测量,使用我们最近开发的萃取电喷雾电离飞行时间质谱仪(EESI-TOF)实现。我们的结果表明,浓缩相反应迅速改变OA组成和矿物对颗粒物质的贡献。因此,霍姆的大气命运不能仅仅在挥发性方面描述,但必须考虑粒子相反应来描述对整体粒子生命周期和全球碳预算的HOM效应。

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