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dc.contributor.authorAlofs, D. J.
dc.contributor.authorTrueblood, M. B.
dc.contributor.authorWhite, D. R.
dc.contributor.authorBehr, V. L.
dc.date.accessioned2017-06-09T17:40:09Z
dc.date.available2017-06-09T17:40:09Z
dc.date.copyright1979/09/01
dc.date.issued1979
dc.identifier.issn0021-8952
dc.identifier.otherams-9760.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233284
dc.description.abstractNucleation experiments with monodisperse NaCl aerosols showed good agreement with the Köhler theory relating the critical super-saturation Sc to the dry size. Aerosols produced by condensing NaCl showed the same Sc as those produced by evaporating aqueous NaCl solution droplets. This indicates that if there is an energy barrier in going from a dry NaCl particle to a solution droplet, this energy barrier is small. The fact that the evaporation aerosol particles are cubical crystals and the condensation aerosols are amorphous spheres is shown to make no difference in the nucleation threshold. The investigation also gives insights into the performance of the equipment used, especially the commercial electrostatic aerosol classifier and the vertical flow thermal diffusion chamber developed in this laboratory. When operating this chamber in the isothermal mode, a 36% upper limit was found on the uncertainty in Sc due to index of refraction sensitivity in sizing the water drops. Within this range of uncertainty, the isothermal mode data agreed with the Köhler theory.
dc.publisherAmerican Meteorological Society
dc.titleNucleation Experiments with Monodisperse NaCl Aerosols
dc.typeJournal Paper
dc.journal.volume18
dc.journal.issue9
dc.journal.titleJournal of Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1979)018<1106:NEWMNA>2.0.CO;2
dc.journal.fristpage1106
dc.journal.lastpage1117
dc.treeJournal of Applied Meteorology:;1979:;volume( 018 ):;issue: 009
dc.contenttypeFulltext


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