多相硫化学有利于颗粒在寒冷和黑暗的城市环境中生长。

IF 3.3 3区 化学 Q2 CHEMISTRY, PHYSICAL
Jingqiu Mao, Kunal Bali, James R Campbell, Ellis S Robinson, Peter F DeCarlo, Amna Ijaz, Brice Temime-Roussel, Barbara D'Anna, Damien Ketcherside, Robert J Yokelson, Lu Hu, Meeta Cesler-Maloney, William R Simpson, Fangzhou Guo, James H Flynn, Jason M St Clair, Athanasios Nenes, Rodney J Weber
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引用次数: 0

摘要

根据24小时过滤测量,在费尔班克斯冬季,硫酸盐平均占环境PM2.5质量的20%。在ALPACA 2022野外活动(2022年1月15日至2月28日)期间,我们在三个城市站点部署了两台气溶胶质谱仪(AMS)和一台气溶胶化学形态监测仪(ACSM),并结合扫描迁移度粒径仪(SMPS),研究了亚小时尺度下气溶胶成分和粒径分布的演变。在环境温度在-25至-35°C之间的严重污染事件中,所有三个仪器(两个AMS和一个ACSM)都记录到硫酸盐质量急剧增加,在几小时内从5到40 μg m-3不等。这一增加贡献了观测到的环境PM2.5质量浓度上升的一半,并且与数量分布从直径小于100纳米的颗粒(Dp < 100纳米)向直径大于100纳米的颗粒(Dp > 100纳米)的实质性转变相吻合,而数量浓度几乎没有增加。相应的体积浓度的增加和分布向更大粒径的转变表明,硫酸盐和有机气溶胶是在原有气溶胶上二次形成的。将AMS-硫酸盐(所有硫种)与通过在线颗粒进液采样离子色谱(PILS-IC)测量的无机硫酸盐进行比较,我们发现大约80%的硫酸盐增加是由于有机硫,这与有机硫化合物AMS的质谱特征一致。硫酸盐的快速形成似乎与环境醛浓度(甲醛和乙醛)的峰值和环境PM2.5中S(IV)的增加相一致。这可能是多相化学的结果,在多相化学中,羟甲磺酸盐(HMS)和其他醛- s (IV)加合物是通过醛和溶解的气溶胶中的SO2之间的反应形成的。我们估计,包括HMS在内的所有S(IV)物种对气溶胶硫的贡献平均为30%,其中大部分发生在硫酸盐快速增加事件中。我们的工作强调了控制醛在减轻费尔班克斯严重空气污染事件中的关键作用,并可能适用于其他城市地区。它还强调了多相化学在驱动颗粒从艾特肯模式生长到积累模式的重要性,这是气溶胶与云相互作用的关键步骤。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multiphase sulfur chemistry facilitates particle growth in a cold and dark urban environment.

Sulfate comprises an average of 20% of the ambient PM2.5 mass during the winter months in Fairbanks, based on 24-hour filter measurements. During the ALPACA 2022 field campaign (Jan 15th-Feb 28th of 2022), we deployed two aerosol mass spectrometers (AMS) and one aerosol chemical speciation monitor (ACSM) at three urban sites, combined with Scanning Mobility Particle Sizers (SMPS), to examine the evolution of aerosol composition and size distribution at a sub-hourly time scale. During an intense pollution episode with ambient temperature between -25 and -35 °C, all three instruments (two AMS and one ACSM) recorded a sharp increase in sulfate mass, ranging from 5 to 40 μg m-3 within a few hours. This increase contributed up to half of the observed rise in ambient PM2.5 mass concentration and coincided with a substantial shift in the number distribution from particle sizes less than 100 nm diameter (Dp < 100 nm) to larger particles (Dp > 100 nm) with little increase in number concentration. The corresponding increase in the volume concentration and distribution shift to larger particle size suggests the secondary formation of sulfate and organic aerosol onto pre-existing aerosols. Comparing AMS-sulfate (all sulfur species) to inorganic sulfate measured by online particle-into-liquid sampler-ion chromatography (PILS-IC), we find roughly 80% of sulfate increase was due to organic sulfur, consistent with the observation of mass spectral signatures in the AMS of organosulfur compounds. The rapid formation of sulfate appears to coincide with spikes in ambient aldehyde concentrations (formaldehyde and acetaldehyde) and an increase in S(IV) in ambient PM2.5. This likely results from multiphase chemistry, where hydroxymethanesulfonate (HMS) and other aldehyde-S(IV) adducts are formed through reactions between aldehydes and SO2 in deliquesced aerosols. We estimate that all S(IV) species, including HMS, contribute an average of 30% to aerosol sulfur, with a dominant fraction occurring during rapid sulfate increase events. Our work highlights the crucial role of controlling aldehydes to mitigate severe air pollution events in Fairbanks and may apply to other urban areas. It also emphasizes the significance of multiphase chemistry in driving particle growth from Aitken mode to accumulation mode, a key step for aerosol-cloud interactions.

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来源期刊
Faraday Discussions
Faraday Discussions 化学-物理化学
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期刊介绍: Discussion summary and research papers from discussion meetings that focus on rapidly developing areas of physical chemistry and its interfaces
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