Abstract

Abstract. Viscosity in particles consisting of secondary organic material (SOM) has recently become an area of research focus, since information on viscosity is needed to predict the environmental impacts of SOM particles. Recently Renbaum-Wolff et al. (2013a) developed a poke-flow technique that was combined with simulations of fluid flow to constrain the viscosities of SOM samples of 1–5 mg mass, roughly the maximum that may be collected from environmental chambers or flow tubes on a reasonable timescale. The current manuscript expands on the initial validation experiments carried out by Renbaum-Wolff et al. First, the poke-flow technique combined with simulations of fluid flow was used to determine the viscosity of sucrose–water particles over a relatively wide range of relative humidities (RHs). The lower and upper limits of viscosity at 59% RH were 1.0 × 101 and 1.6 × 104 Pa s, whilst at 37% RH the corresponding values were 7.2 × 104 and 4.7 × 106 Pa s, respectively. The results are in good agreement with recent measurements by Quintas et al. (2006) and Power et al. (2013). Second, the approach was used to determine the viscosity of two polybutene standards. The simulated lower and upper limits of viscosity for standard #1 was 2.0 × 102 and 1.2 × 104 Pa s, whilst for standard #2 the corresponding values were 3.1 × 102 and 2.4 × 104 Pa s. These values are in good agreement with values reported by the manufacturer. The results for both the sucrose–water particles and the polybutene standards show that the poke-flow technique combined with simulations of fluid flow is capable of providing both lower and upper limits of viscosity that are consistent with literature or measured values when the viscosity of the particles are in the range of ≈ 5 × 102 to ≈ 3 × 106 Pa s.

Highlights

  • Particles consisting of secondary organic material (SOM) are abundant in the atmosphere and, depending upon location, typically account for 20–80 % of the mass of atmospheric aerosol particles (Kanakidou et al, 2005; Jimenez et al, 2009)

  • In the paper by Renbaum-Wolff et al (2013a), only a preliminary validation of the poke-flow technique combined with simulations of fluid flow was carried out for viscosities < 108 Pa s due to the lack of suitable standards for validation at the time of publication

  • The approach is used to determine the viscosity of sucrose–water particles over a wider range of relative humidities (RHs) than previously done by Renbaum-Wolff et al (2013a). These results are compared to recent results published by Power et al (2013), who reported viscosities of sucrose–water particles ranging from 10−3 to 109 Pa s, and Quintas et al (2006), who measured a viscosity of 103 Pa s at 54 % RH using a rotational controlled stress rheometer

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Summary

Introduction

Particles consisting of secondary organic material (SOM) are abundant in the atmosphere and, depending upon location, typically account for 20–80 % of the mass of atmospheric aerosol particles (Kanakidou et al, 2005; Jimenez et al, 2009). These SOM particles can affect the Earth’s climate directly by scattering and/or absorbing solar radiation and indirectly by acting as ice and liquid cloud droplet nuclei (Solomon et al, 2007; Murray et al, 2010; Wang et al, 2012). Riipinen et al (2011) showed that the size distribution and number concentrations of ultrafine aerosol particles, which are important for the aerosol direct and indirect effect on climate, depend on diffusion within particles. Shiraiwa and Seinfeld (2012) showed that predictions of the total mass

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