Xiao Yao, Costa Emily J, He Xu, Rogers Mitchell J, Mirrielees Jessica A, Hass-Mitchell Tori N, Joo Taekyu, Nault Benjamin A, Gentner Drew R, O'Brien Rachel E, Ault Andrew P
Department of Chemistry, University of Michigan, Ann Arbor, Michigan, USA.
Department of Civil and Environmental Engineering, University of Michigan, Ann Arbor, Michigan, USA.
Aerosol Sci Technol. 2025 Sep 12. doi: 10.1080/02786826.2025.2555886.
Elevated concentrations of fine particulate matter (PM, particles < 2.5 m) lead to negative health outcomes in urban areas, such as New York City (NYC). The sources of particles contributing to PM in NYC are variable and complex due to the range of primary anthropogenic and biogenic emissions, as well as secondary aerosol formation (i.e., aging) from gaseous precursors. To improve understanding of the contributors to PM, single particle microspectroscopy uses chemical fingerprints to identify sources and the extent of aging, but few studies have integrated multiple microspectroscopy methods to understand PM in NYC. Herein, we focus on a recently-developed form of microspectroscopy that can measure atmospherically-sized particles (>~0.8 m), optical photothermal infrared (O-PTIR). We compare O-PTIR to existing microspectroscopy methods [Raman, fluorescence, and energy dispersive X-ray (EDX)] to study sources and aging of the complex NYC aerosol based on functional group and elemental information, which we also relate to bulk mass spectrometry methods. Single particle data shows submicron aerosol composition dominated by carbonaceous particles that fluoresce mixed with ammonium and sulfate, with a range of oxidized organic functional groups observed. At larger sizes, more primary sources (salts, dust, and biological) were observed, with nitrate being the dominant secondary anion. Collectively, the results from OPTIR and other instruments across case-study days reveal variations in sources and aging, with greater variability at larger diameters. Demonstrating the potential of O-PTIR when combined with the other methods to provide data that is important for improving air quality in urban megacities.
细颗粒物(PM,粒径小于2.5微米的颗粒物)浓度升高会在纽约市等城市地区导致负面健康后果。由于主要人为排放和生物排放范围广泛,以及气态前体形成二次气溶胶(即老化),纽约市造成PM的颗粒物来源多变且复杂。为了更好地了解造成PM的因素,单颗粒光谱学利用化学指纹来识别来源和老化程度,但很少有研究整合多种光谱学方法来了解纽约市的PM。在此,我们聚焦于一种最近开发的可测量大气尺寸颗粒(大于约0.8微米)的光谱学形式,即光学光热红外(O-PTIR)。我们将O-PTIR与现有的光谱学方法[拉曼光谱、荧光光谱和能量色散X射线(EDX)]进行比较,以基于官能团和元素信息研究复杂的纽约市气溶胶的来源和老化情况,我们还将这些信息与整体质谱方法相关联。单颗粒数据显示,亚微米气溶胶成分以与铵和硫酸盐混合的发荧光的含碳颗粒为主,观察到一系列氧化有机官能团。在较大粒径下,观察到更多的一次源(盐类、灰尘和生物源),硝酸盐是主要的二次阴离子。总体而言,在案例研究日期间,O-PTIR和其他仪器的结果揭示了来源和老化的变化,直径越大变异性越大。这证明了O-PTIR与其他方法结合时的潜力,可为改善特大城市空气质量提供重要数据。