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Direct Determination of Aerosol pH: Size-Resolved Measurements of Submicrometer and Supermicrometer Aqueous Particles

机译:气溶胶PH的直接测定:潜置尺寸尺寸分辨测量和超级计含水粒子

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摘要

Measuring the acidity of atmospheric aerosols is critical, as many key multiphase chemical reactions involving aerosols are highly pH-dependent. These reactions impact processes, such as secondary organic aerosol (SOA) formation, that impact climate and health. However, determining the pH of atmospheric particles, which have minute volumes (10(-23)-10(-18) L), is an analytical challenge due to the nonconservative nature of the hydronium ion, particularly as most chemical aerosol measurements are made offline or under vacuum, where water can be lost and acid-base equilibria shifted. Because of these challenges, there have been no direct methods to probe atmospheric aerosol acidity, and pH has typically been determined by proxy/indirect methods, such as ion balance, or thermodynamic models. Herein, we present a novel and facile method for direct measurement of size-resolved aerosol acidity from pH 0 to 4.5 using quantitative colorimetric image processing of cellular phone images of (NH4)(2)SO4-H2SO4 aqueous aerosol particles impacted onto pH-indicator paper. A trend of increasing aerosol acidity with decreasing particle size was observed that is consistent with spectroscopic measurements of individual particle pH. These results indicate the potential for direct measurements of size-resolved atmospheric aerosol acidity, which is needed to improve fundamental understanding of pH-dependent atmospheric processes, such as SOA formation.
机译:测量大气气溶胶的酸度至关重要,因为涉及气溶胶的许多关键多相化学反应是高度pH依赖性的。这些反应影响过程,如次要有机气溶胶(SOA)形成,影响气候和健康。然而,确定具有微小体积(10(-23)-10(-18)L)的大气颗粒的pH是由于散氢离子的非不合理性质,特别是随着大多数化学气溶胶测量来进行分析攻击离线或在真空下,水可以丢失,酸碱平衡偏移。由于这些挑战,没有直接方法探测大气气溶胶酸度,并且通常通过代理/间接方法,例如离子平衡或热力学模型来确定pH。在此,我们使用(NH4)(2)SO4-H2SO4水溶液水溶液水溶液水溶液的定量比色图像处理直接测量从pH 0至4.5直接测量从pH 0到4.5的尺寸分辨的气溶胶酸度。纸。观察到随着单个颗粒pH的光谱测量,观察到增加粒度降低的气溶胶酸度的趋势。这些结果表明了尺寸分辨大气气溶胶酸度直接测量的可能性,这是改善对pH依赖性大气过程的基本理解,例如SOA形成。

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