0000000001026579

AUTHOR

Jürg Thudium

showing 2 related works from this author

Water uptake and equilibrium sizes of aerosol particles at high relative humidities: Their dependence on the composition of the water-soluble material

1978

Equilibrium water uptake and the sizes of atmospheric aerosol particles have for the first time been determined for high relative humidities, i.e., for humidities above 95 percent, as a function of the particles chemical composition. For that purpose a new treatment of the osmotic coefficient has been developed and experimentally confirmed. It is shown that the equilibrium water uptake and the equilibrium sizes of atmospheric aerosol particles at large relative humidities are significantly dependent on their chemical composition.

ChemistryAnalytical chemistryfood and beveragesAtmospheric scienceshumanitiesAerosolGeophysicsWater solubleGeochemistry and PetrologyWater uptakeCloud condensation nucleiComposition (visual arts)Osmotic coefficientChemical compositionPhysics::Atmospheric and Oceanic PhysicsPure and Applied Geophysics PAGEOPH
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Mean bulk densities of samples of dry atmospheric aerosol particles: A summary of measured data

1977

Mean bulk densities of various samples of dry atmospheric aerosol particles sampled at different sites and during different seasons and weather situations range between 1.8 and more than 3 gm cm3.

GeophysicsGeochemistry and PetrologyRange (biology)ClimatologyEnvironmental sciencerespiratory systemAtmospheric sciencesAerosolPure and Applied Geophysics PAGEOPH
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