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Journal ArticleDOI

Colorimetric Particle Acidity Analysis of Secondary Organic Aerosol Coating on Submicron Acidic Aerosols

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TLDR
In this paper, the particle acidity of secondary organic aerosol (SOA) created from ozonolysis of α-pinene in the presence of acidic inorganic seed aerosols was investigated using an indoor Teflon film chamber.
Abstract
The particle acidity of secondary organic aerosol (SOA) created from ozonolysis of α-pinene in the presence of acidic inorganic seed aerosols was investigated using an indoor Teflon film chamber. Colorimetry integrated with a reflectance UV-Visible spectrometer was used for the first time to dynamically measure the aerosol acidity over time. An external calibration curve was produced based on the correlation between the proton mass (ng) collected on the filter, which was impregnated with metanil yellow, and the absorbance of the reflectance UV-Visible spectra for the protonated and the unprotonated metanil yellow on the filter. Using this calibration curve, the particle acidity of the submicron acidic sulfate aerosol coated with SOA was measured from the reflectance UV-Visible spectra of filter samples. The colorimetric analysis requires a short sampling time (less than 2 m) for SOA studies using the laboratory Teflon film chamber and eliminates extraction of the filter sample with water. Results show tha...

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Citations
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Journal ArticleDOI

A critical evaluation of proxy methods used to estimate the acidity of atmospheric particles

TL;DR: In this article, the authors evaluated four of the most common aerosol acidity proxies: ion balance method, molar ratio method, thermodynamic equilibrium models, and phase partitioning of ammonia.
Journal ArticleDOI

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

TL;DR: A novel and facile method for direct measurement of size-resolved aerosol acidity from pH 0 to 4.5 is presented using quantitative colorimetric image processing of cellular phone images of (NH4)2SO4-H2 SO4 aqueous aerosol particles impacted onto pH-indicator paper.
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Direct Measurement of pH in Individual Particles via Raman Microspectroscopy and Variation in Acidity with Relative Humidity

TL;DR: Raman microspectroscopy was used to determine the pH of individual particles based on sulfate and bisulfate concentrations determined from νs(SO4(2-)) and νS(HSO4(-)), the acid dissociation constant, and activity coefficients from extended Debye-Hückel calculations, indicating the potential for direct spectroscopic determination of pH in individual particles.
References
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Journal ArticleDOI

Organic aerosol and global climate modelling: a review

TL;DR: In this article, the authors reviewed existing knowledge with regard to organic aerosol (OA) of importance for global climate modelling and defined critical gaps needed to reduce the involved uncertainties, and synthesized the information to provide a continuous analysis of the flow from the emitted material to the atmosphere up to the point of the climate impact of the produced organic aerosols.
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ISORROPIA: A New Thermodynamic Equilibrium Model for Multiphase Multicomponent Inorganic Aerosols

TL;DR: In this article, a computationally efficient and rigorous thermodynamic model that predicts the physical state and composition of inorganic atmospheric aerosol is presented, where the main features of the model is the implementation of mutual deliquescence of multicomponent salt particles.
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Heterogeneous Atmospheric Aerosol Production by Acid-Catalyzed Particle-Phase Reactions

TL;DR: If acid-catalyzed heterogeneous reactions of SOA products are included in current models, the predicted SOA formation will be much greater and could have a much larger impact on climate forcing effects than the authors now predict.
Journal ArticleDOI

Identification of polymers as major components of atmospheric organic aerosols.

TL;DR: Results from photooxidation of aromatic compounds in a reaction chamber show that a substantial fraction of the organic aerosol mass is composed of polymers, which results in a lower volatility of this secondaryorganic aerosol and a higher aerosol yield than a model using vapor pressures of individual organic species would predict.
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