气相二氧化硫是否能从水性气溶胶的空气-水界面上去除大气萃取的有机物薄膜?

IF 2.8 Q3 ENVIRONMENTAL SCIENCES
Edward J. Stuckey, Rebecca J. L. Welbourn, Stephanie H. Jones, Alexander J. Armstrong, Matthew Wilkinson, James I. L. Morison and Martin D. King
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引用次数: 0

摘要

气相二氧化硫与不饱和碳碳双键反应,在气溶胶表面形成有机硫酸盐。以往的研究侧重于反应产物,而不是有机薄膜在大气中的归宿。中子反射仪被用来研究气相二氧化硫在空气-水界面与从大气颗粒物和纯代理化学品中提取的有机物的相互作用,以确定有机薄膜与二氧化硫的反应是否会去除薄膜,以及是否会形成产物薄膜。在城市和林地环境中收集的大气气溶胶所形成的薄膜通常只有大约 0.6 纳米厚,而木烟样品则形成了一层厚(40 纳米)的薄膜。对这层较厚的木烟薄膜进行拟合后发现,在界面处有一个三层结构,这与空气-水界面旁富含表面活性剂的一层、富含多芳烃(PAH)的中层以及顶部脂肪族较多的区域是一致的。大气提取物在空气-水界面的多层结构可能是一个令人兴奋的结果,需要进一步研究。经证实,气相二氧化硫会与空气-水界面上含有碳碳双键的纯不溶性表面活性剂分子(油酸)发生反应,而不会与类似的饱和表面活性剂(硬脂酸)发生反应。在二氧化硫与从城市和林地环境中提取的大气材料相互作用的过程中,没有观察到任何反应,也没有材料从界面上脱落;不过,从木质烟雾中提取的材料制成的薄膜似乎被二氧化硫改变了,但材料没有明显损失。此外,中子屏蔽室中的气相臭氧混合比历来是与有机物发生反应的一些问题,但研究发现,该混合比约为 15 ppb,没有证据表明中子束路径中产生了额外的臭氧。由于从大气中萃取的真实薄膜中没有大量物质被去除,因此认为二氧化硫对去除空气-水界面上的有机薄膜并不重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Does gas-phase sulfur dioxide remove films of atmosphere-extracted organic material from the aqueous aerosol air–water interface?†

Does gas-phase sulfur dioxide remove films of atmosphere-extracted organic material from the aqueous aerosol air–water interface?†

The reaction of gas-phase SO2 with unsaturated carbon–carbon double bonds forms organosulfates at the surface of the aerosol. Previous studies have focused on the reaction products and not the fate of organic films in the atmosphere. Neutron reflectometry was used to study the interaction of gas-phase SO2 at the air–water interface with organic material extracted from atmospheric particulate matter and pure proxy chemicals to determine whether the reaction of organic films with SO2 removes the film and if a product film is formed. Films formed from atmospheric aerosol collected in urban and woodland environments typically produced a layer of approximately 0.6 nm thickness, whereas a thick (>40 nm) film was formed by the woodsmoke sample. Fitting of this thicker woodsmoke film suggested a three-layered structure at the interface that has been interpreted to be consistent with a surfactant-rich layer next to the air–water interface, a mid-layer rich in polyaromatic hydrocarbons (PAH), and topped with a more aliphatic region. The multilayer structure of atmospheric extracted material at the air–water interface is potentially an exciting result that requires further study. Gas-phase SO2 was confirmed to react with pure insoluble surfactant molecules at the air–water interface that contained carbon–carbon double bonds (oleic acid) and did not react with a similar saturated surfactant (stearic acid). No reaction was observed during the interaction of SO2 and atmospheric material extracted from urban and woodland environments, and no material appeared to be removed from the interface; however, films made from woodsmoke-extracted material did appear to be altered by SO2 but there was no significant loss of material. In addition, the gas-phase ozone mixing ratios in the neutron blockhouse, which have historically been of some concern for reactions with organics, were found to be of the order 15 ppb, with no evidence of additional production in the neutron beam-path. Owing to a lack of substantial removal of material from real atmospheric extracted films, SO2 is not considered atmospherically significant for the removal of organic films from the air–water interface.

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