Abstract

Abstract. The hygroscopic phase transitions of ammonium sulfate mixed with isoprene-derived secondary organic material were investigated in aerosol experiments. The organic material was produced by isoprene photo-oxidation at 40% and 60% relative humidity. The low volatility fraction of the photo-oxidation products condensed onto ammonium sulfate particles. The particle-phase organic material had oxygen-to-carbon ratios of 0.67 to 0.74 (±0.2) for mass concentrations of 20 to 30 μg m−3. The deliquescence, efflorescence, and phase miscibility of the mixed particles were investigated using a dual arm tandem differential mobility analyzer. The isoprene photo-oxidation products induced deviations in behavior relative to pure ammonium sulfate. Compared to an efflorescence relative humidity (ERH) of 30 to 35% for pure ammonium sulfate, efflorescence was eliminated for aqueous particles having organic volume fractions ϵ of 0.6 and greater. Compared to a deliquescence relative humidity (DRH) of 80% for pure ammonium sulfate, the DRH steadily decreased with increasing ϵ, approaching a DRH of 40% for ϵ of 0.9. Parameterizations of the DRH(ϵ) and ERH(ϵ) curves were as follows: DRH(ϵ)= ∑i ci,d ϵi valid for 0 ≤ ϵ ≤0.86 and ERH(ϵ)= ∑ i ci,e ϵi valid for 0 ≤ ϵ ≤ 0.55 for the coefficients c0,d= 80.67, c0,e = 28.35, c1,d = −11.45, c1,e = −13.66, c2,d = 0, c2,e = 0, c3,d = 57.99, c3,e = -83.80, c4,d = −106.80, and c4,e = 0. The molecular description that is thermodynamically implied by these strongly sloped DRH(ϵ) and ERH(ϵ) curves is that the organic isoprene photo-oxidation products, the inorganic ammonium sulfate, and water form a miscible liquid phase even at low relative humidity. This phase miscibility is in contrast to the liquid-liquid separation that occurs for some other types of secondary organic material. These differences in liquid-liquid separation are consistent with a prediction recently presented in the literature that the bifurcation between liquid-liquid phase separation versus mixing depends on the oxygen-to-carbon ratio of the organic material. The conclusions are that the influence of secondary organic material on the hygroscopic properties of ammonium sulfate varies with organic composition and that the degree of oxygenation of the organic material, which is a measurable characteristic of complex organic materials, is an important variable influencing the hygroscopic properties of mixed organic-inorganic particles.

Highlights

  • The water content of atmospheric particles can influence heterogeneous chemistry, cloud activation, and radiative forcing, among other phenomena (Seinfeld and Pandis, 2006)

  • The results of this study show that secondary organic material produced by isoprene photo-oxidation strongly influences the hygroscopic phase transitions of ammonium sulfate

  • Compared to a deliquescence relative humidity of 80 % and an efflorescence relative humidity of 30–35 % for pure ammonium sulfate, efflorescence was eliminated for mixed aqueous particles of high organic volume fractions of approximately 0.6, and the deliquescence relative humidity decreased to 40 % for volume fractions approaching 0.9

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Summary

Introduction

The water content of atmospheric particles can influence heterogeneous chemistry, cloud activation, and radiative forcing, among other phenomena (Seinfeld and Pandis, 2006). The effects of secondary organic material on the phase transitions of the inorganic components of particles such as ammonium sulfate have been characterized in only a few studies These studies show that SOM produced by α-pinene, limonene, and β-caryophyllene ozonolysis exerts a minor influence on the deliquescence relative humidity (DRH) and the efflorescence relative humidity (ERH) of the ammonium sulfate component of the mixed particles (Saathoff et al, 2003; Takahama et al, 2007; Bertram et al, 2011; Smith et al, 2011). Bertram et al (2011) likewise presented an initial data set for the effects of SOM produced by isoprene photo-oxidation on the phase transitions of ammonium sulfate, showing a decrease in DRH for organic volume fractions from 0 to 0.8 and a decrease in ERH for organic volume fractions from 0 to 0.6. The influence of different conditions of SOM production, including in the presence of aqueous compared to solid sulfate particles at relative humidities of 40 and 60 %, is explored

Particle generation
Particle hygroscopic analysis
Transmission ratio experiments
Number-diameter distribution experiments
Other number-diameter distribution experiments
Particle population and sub-populations
Transmission ratios
Number-diameter distributions
Comparison to other studies
Conclusions and implications
DMAmono outflow
Water content
Hygroscopic growth
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