墨西哥城大气气溶胶硫的分布和种类:低氮途径产生的硫酸盐、有机硫酸盐和异戊二烯二次有机气溶胶

Madeline E. Cooke, Cara M. Waters, Joel Y. Asare, Jessica A. Mirrielees, Andrew L. Holen, Molly P. Frauenheim, Zhenfa Zhang, Avram Gold, Kerri A. Pratt, Jason D. Surratt, Luis A. Ladino and Andrew P. Ault*, 
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引用次数: 0

摘要

空气质量差是墨西哥城长期面临的挑战,要解决这一问题,就必须了解 PM2.5(直径小于 2.5 μm 的颗粒物)的化学成分。硫酸盐和二次有机气溶胶(SOA)是墨西哥城 PM2.5 的两大来源,但它们的来源、在单个颗粒中的分布以及形成有机硫酸盐的能力还存在不确定性。在此,我们使用电子色散 X 射线光谱法表明,在墨西哥城的两个地点,按数量计算,分别只有 41±1% 和 25± 1% 的颗粒(空气动力学直径,0.32-0.56 μm)含有硫。振动光谱(光学-光热红外光谱 + 拉曼微光谱)显示,这些含硫颗粒由无机硫酸盐(SO42-)和有机硫酸盐(ROSO3-)组成。此外,我们还利用液相色谱-高分辨率质谱法意外地测量到了来自低一氧化氮反应途径的大量异戊二烯衍生 SOA,特别是有机硫酸盐(甲基四醇硫酸盐 = 平均 50 纳克/立方米,最大 150 纳克/立方米)和多元醇(甲基四醇 = 平均 70 纳克/立方米,最大 190 纳克/立方米)。不同地点之间二氧化硫和氮氧化物浓度的差异很可能导致了硫酸盐、有机硫酸盐和 SOA 形成的空间差异。这些发现加深了人们对墨西哥城硫分布和 SOA 来源的了解,为改善空气质量提供了参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Atmospheric Aerosol Sulfur Distribution and Speciation in Mexico City: Sulfate, Organosulfates, and Isoprene-Derived Secondary Organic Aerosol from Low NO Pathways

Atmospheric Aerosol Sulfur Distribution and Speciation in Mexico City: Sulfate, Organosulfates, and Isoprene-Derived Secondary Organic Aerosol from Low NO Pathways

Poor air quality is a persistent challenge in Mexico City, and addressing this issue requires an understanding of the chemical composition of PM2.5 (particulate matter less than 2.5 μm in diameter). Sulfate and secondary organic aerosol (SOA) are two of the largest contributors to PM2.5 in Mexico City, but uncertainties exist regarding their sources, distribution across individual particles, and ability to form organosulfates. Herein, we show using electron dispersive x-ray spectroscopy that only 41 ± 1% and 25 ± 1% of particles (aerodynamic diameter, 0.32–0.56 μm) by number at two sites in Mexico City, respectively, contain sulfur. Vibrational spectroscopy (Optical-Photothermal Infrared + Raman Microspectroscopy) shows that these sulfur-containing particles consist of inorganic sulfate (SO42–) and organosulfates (ROSO3). In addition, we unexpectedly measured abundant isoprene-derived SOA from low nitric oxide reaction pathways, specifically organosulfates (methyltetrol sulfates = avg. 50 ng/m3, max. 150 ng/m3) and polyols (methyltetrols = avg. 70 ng/m3, max. 190 ng/m3) using liquid chromatography with high-resolution mass spectrometry. Differences in SO2 and NOx concentrations between sites likely contribute to these spatial differences in sulfate, organosulfate, and SOA formation. These findings improve understanding of sulfur distribution and sources of SOA in Mexico City, which can inform efforts to improve air quality.

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