ACPD Atmospheric Chemistry and Physics Discussions ACPD 1680-7375 Copernicus GmbH Göttingen, Germany 10.5194/acpd-9-955-2009 Towards closing the gap between hygroscopic growth and activation for secondary organic aerosol: Part 1 – Evidence from measurements Wex H. 1 Petters M. D. 2 Carrico C. M. 2 Hallbauer E. 1 Massling A. 1 3 McMeeking G. R. 2 4 Poulain L. 1 Wu Z. 1 Kreidenweis S. M. 2 Stratmann F. 1 Institute for Tropospheric Research, Leipzig, Germany Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA now at: National Environmental Research Institute, Aarhus University, Roskilde, Denmark now at: Centre for Atmospheric Science, University of Manchester, Manchester, UK 13 01 2009 9 1 955 989 This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. This article is available from http://www.atmos-chem-phys-discuss.net/9/955/2009/acpd-9-955-2009.html The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/955/2009/acpd-9-955-2009.pdf

Secondary Organic Aerosols (SOA) studied in laboratory experiments generally was found to show only slight hygroscopic growth, but a much better activity as a CCN (Cloud Condensation Nucleus) than indicated by the hygroscopic growth. This discrepancy was examined at LACIS (Leipzig Aerosol Cloud Interaction Simulator), using a portable generator that produced SOA particles from the ozonolysis of α-pinene, and adding butanol or butanol and water vapor during some of the experiments. The light scattering signal of dry SOA-particles was measured by the LACIS optical particle spectrometer and was used to derive a refractive index for SOA of 1.45. LACIS also measured the hygroscopic growth of SOA particles up to 99.6% relative humidity (RH), and a CCN counter was used to measure the particle activation. SOA-particles were CCN active with critical diameters of e.g. 100 and 55 nm at supersaturations of 0.4 and 1.1%, respectively. But only slight hygroscopic growth with hygroscopic growth factors &le;1.05 was observed at RH<98% RH. The hygroscopic growth increased slightly with the OH concentration present during the SOA-generation. At RH>98%, the hygroscopic growth increased stronger than would be expected if a constant hygroscopicity parameter for the particle/droplet solution was assumed. An increase of the hygroscopicity parameter by a factor of 4–6 was observed in the RH-range from below 90 to 99.6%, and this increase continued for increasingly diluted particle solutions for activating particles. This explains an observation already made in the past: that the relation between critical supersaturation and dry diameter for activation is steeper than what would be expected for a constant value of the hygroscopicity. The increase in the hygroscopicity parameter could be explained by either an increase in the number of ions/molecules in solution (e.g. due to the presence of slightly soluble particles with deliquescence RHs above 98%), or a change in the non-ideal behaviour (see companion paper Petters et al., 2008). Combining measurements of hygroscopic growth and activation, it was found that the surface tension that has to be assumed to interpret the measurements consistently is greater than 55 mN/m, possibly close to that of pure water, depending on the different SOA-types produced, and therefore only in part accounts for the discrepancy between hygroscopic growth and CCN activity observed for SOA particles in the past.

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