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dc.contributor.authorDaskalakis, Evangelos-
dc.contributor.authorSalameh, Anastasia-
dc.identifier.citationAGU 2016 Fall Meeting, 2016, San Francisco, USA, 12-16 Decemberen_US
dc.description.abstractThe impact of aerosol properties on cloud dynamics and the radiative balance of the atmosphere relies on the parametrizations of cloud droplet formation. Such parametrization is based on equilibrium thermodynamics proposed by Köhler in 1936. There is considerable debate in the literature on the importance of factors like the surface tension depression or the water activity decrease for the correct parametrization. To gain fundamental insight into New Particle Formation (NPF), or Cloud Condensation Nuclei (CCN) activation one has to study microscopic properties of aqueous droplets, involving surface and bulk dynamics. The surface tension of droplets can be associated with the effects from Organic Matter (OM), whereas the static dielectric constant of water reflects the structure and dynamics of ions within solutions and can present a measure of water activity. In this study we employ Molecular Dynamics Simulations on aquatic droplets that contain surface active OM (acetaldehyde, methylglyoxal) and salts. We give insight into the dynamics of aquatic droplets with radials of 3.6nm at a level of detail that is not accessible experimentally (J. Phys. Chem. C 2016, 120:11508). We propose that as the surface tension of an aquatic droplet is decreased in the presence of surface-active OM, the water activity is affected as well. This is due to the fact that the water dipoles are oriented based on the salt morphology within the droplet. We suggest that the surface tension depression can be accompanied by the water activity change. This can be associated with the possible effects of surface-active species in terms of salt morphology transitions within an aerosol at the NPF and early particle growth time scales. Based on this study, surface-active OM seems important in controlling (a) the salt morphology transitions within a nucleus during NPF and particle growth and (b) a correlation between surface activity and water activity of ionic aquatic droplets. The latter correlation could be a fundamental property to consider when assessing NPF and the Köhler theory.en_US
dc.subjectAerosols and particlesen_US
dc.subjectAtmospheric composition and structuredeen_US
dc.subjectClouds and cloud feedbacksen_US
dc.subjectBiogeochemical cyclesen_US
dc.titleCorrelation Between Surface Tension and the Bulk Dynamics in Salty Atmospheric Aquatic Dropletsen_US
dc.typeConference Papersen_US
dc.collaborationCyprus University of Technologyen_US
dc.subject.categoryChemical Sciencesen_US
dc.subject.fieldNatural Sciencesen_US
dc.publicationPeer Revieweden_US
item.fulltextNo Fulltext-
item.grantfulltextnone- of Environmental Science and Technology- of Geotechnical Sciences and Environmental Management- of Geotechnical Sciences and Environmental Management-
Appears in Collections:Δημοσιεύσεις σε συνέδρια/Conference papers
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