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首页> 外文期刊>Atmospheric chemistry and physics >Liquid–liquid phase separation and morphologies in organic particles consisting of iα/i-pinene and iβ/i-caryophyllene ozonolysis products and mixtures with commercially available organic compounds
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Liquid–liquid phase separation and morphologies in organic particles consisting of iα/i-pinene and iβ/i-caryophyllene ozonolysis products and mixtures with commercially available organic compounds

机译:由有机颗粒中的液 - 液相分离和形态,其包括α - 烯烃和β-β-β - 与市售有机化合物的羧基臭氧产物和混合物

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Liquid–liquid phase separation (LLPS) in organic aerosol particles can impact several properties of atmospheric particulate matter, such as cloud condensation nuclei (CCN) properties, optical properties, and gas-to-particle partitioning. Yet, our understanding of LLPS in organic aerosols is far from complete. Here, we report on the LLPS of one-component and two-component organic particles consisting of α-pinene- and β-caryophyllene-derived ozonolysis products and commercially available organic compounds of relevance to atmospheric organic particles. In the experiments involving single-component organic particles, LLPS was observed in 8 out of 11 particle types studied. LLPS almost always occurred when the oxygen-to-carbon elemental ratio (O:C) was ≤0.44 but did not occur when O:C was 0.44. The phase separation occurred by spinodal decomposition as well as the nucleation and growth mechanism, and when LLPS occurred, two liquid phases coexisted up to ~100 % relative humidity (RH). In the experiments involving two-component organic particles, LLPS was observed in 23 out of 25 particles types studied. LLPS almost always occurred when the average was O:C ≤0.67 but never occurred when the average O:C was 0.67. The phase separation occurred by spinodal decomposition as well as the nucleation and growth mechanism. When LLPS occurred, two liquid phases coexisted up to ~100 % RH. These results provide further evidence that LLPS is likely a frequent occurrence in organic aerosol particles in the troposphere, even in the absence of inorganic salts.
机译:有机气溶胶颗粒中的液液相分离(LLP)可以影响大气颗粒物质的几种性质,例如云缩合核(CCN)性质,光学性质和气体到颗粒分配。然而,我们对有机气溶胶中的LLP的理解远非完整。在此,我们报告了由α-叉烯 - 和β-羧基醚衍生的臭氧产物和与大气有机颗粒相关的市售有机化合物组成的单组分和双组分有机颗粒的LLP。在涉及单组分有机颗粒的实验中,在研究的11种颗粒类型中观察到LLP。当氧 - 碳素元素比(O:C)≤0.44时,LLP几乎总是发生,但是当O:C> 0.44时没有发生。通过旋光性分解以及成核和生长机制发生相分离,并且当LLP发生时,两个液相共存高达〜100%相对湿度(RH)。在涉及双组分有机颗粒的实验中,在研究的25种颗粒类型中观察到LLP。当平均值为O:C≤0.67时,LLP几乎总是发生,但是当平均O:C> 0.67时,从未发生过。通过旋光性分解以及成核和生长机制发生相分离。当LLP发生时,两个液相共存至〜100%RH。这些结果提供了进一步的证据,即使在没有无机盐的情况下,LLP可能频繁发生在对流层中的有机气溶胶颗粒。

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