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Experimental evidence for excess entropy discontinuities in glass-forming solutions.Measurements of thermodynamic and optical properties of selected aqueous organic and organic-inorganic mixtures of atmospheric relevance.Surface tension prevails over solute effect in organic-influenced cloud droplet activation.Size distribution dynamics reveal particle-phase chemistry in organic aerosol formationMicrophysical explanation of the RH-dependent water affinity of biogenic organic aerosol and its importance for climate.On the mixing and evaporation of secondary organic aerosol components.Gas-particle partitioning of atmospheric aerosols: interplay of physical state, non-ideal mixing and morphology.Role of nucleation mechanism on the size dependent morphology of organic aerosol.Coupling of organic and inorganic aerosol systems and the effect on gas–particle partitioning in the southeastern US.Influence of particle-phase state on the hygroscopic behavior of mixed organic–inorganic aerosolsDiscontinuities in hygroscopic growth below and above water saturation for laboratory surrogates of oligomers in organic atmospheric aerosolsImproved AIOMFAC model parameterisation of the temperature dependence of activity coefficients for aqueous organic mixturesComposition and hygroscopicity of the Los Angeles Aerosol: CalNexExperimental determination of the temperature dependence of water activities for a selection of aqueous organic solutionsResponse to “Comment on ‘Experimental evidence for excess entropy discontinuities in glass-forming solutions”’ [J. Chem. Phys. 139, 047101 (2013)]Vapor pressures of substituted polycarboxylic acids are much lower than previously reportedCorrigendum to "A thermodynamic model of mixed organic–inorganic aerosols to predict activity coefficients" published in Atmos. Chem. Phys., 8, 4559–4593, 2008Liquid-liquid phase separation and morphology of internally mixed dicarboxylic acids/ammonium sulfate/water particlesLiquid-liquid phase separation in aerosol particles: Dependence on O:C, organic functionalities, and compositional complexityNew and extended parameterization of the thermodynamic model AIOMFAC: calculation of activity coefficients for organic-inorganic mixtures containing carboxyl, hydroxyl, carbonyl, ether, ester, alkenyl, alkyl, and aromatic functional groupsComputation of liquid-liquid equilibria and phase stabilities: implications for RH-dependent gas/particle partitioning of organic-inorganic aerosolsEfflorescence of Ammonium Sulfate and Coated Ammonium Sulfate Particles: Evidence for Surface NucleationA thermodynamic model of mixed organic-inorganic aerosols to predict activity coefficientsSummertime Primary and Secondary Contributions to Southern Ocean Cloud Condensation NucleiAirborne characterization of subsaturated aerosol hygroscopicity and dry refractive index from the surface to 6.5 km during the SEAC4RS campaignHygroscopicity of organic surrogate compounds from biomass burning and their effect on the efflorescence of ammonium sulfate in mixed aerosol particlesCompositional evolution of particle-phase reaction products and water in the heterogeneous OH oxidation of model aqueous organic aerosolsHygroscopicity of organic compounds from biomass burning and their influence on the water uptake of mixed organic ammonium sulfate aerosolsA practical method for the calculation of liquid–liquid equilibria in multicomponent organic–water–electrolyte systems using physicochemical constraintsModeling the gas-particle partitioning of secondary organic aerosol: the importance of liquid-liquid phase separationThe vapor pressures and activities of dicarboxylic acids reconsidered: the impact of the physical state of the aerosolOptical deformation of single aerosol particlesAuthor Correction: Summertime Primary and Secondary Contributions to Southern Ocean Cloud Condensation NucleiMultiphase reactivity of polycyclic aromatic hydrocarbons is driven by phase separation and diffusion limitations
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P50
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P106
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