Charge induced stability of water droplets in subsaturated environment

Atmospheric liquid and solid water particles are stabilized if they are coated with either negative or positive electric charge. The surface charge causes an increase of the partial pressure of water vapour close to the surface of each particle, effectively allowing the part...

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Main Authors: J. K. Nielsen, C. Maus, D. Rzesanke, T. Leisner
Format: Article
Language:English
Published: Copernicus Publications 2011-03-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/11/2031/2011/acp-11-2031-2011.pdf
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spelling doaj-4526ef9dc7b5496b878902310b77fed22020-11-24T22:36:10ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242011-03-011152031203710.5194/acp-11-2031-2011Charge induced stability of water droplets in subsaturated environmentJ. K. Nielsen0C. Maus1D. Rzesanke2T. Leisner3Danish Meterological Institute, Lyngbyvej 100, 2100 Kbh Ø, DenmarkTechnical University Ilmenau (TUI), Institute for Physics, Postfach 100565, 98684 Ilmenau, GermanyKarlsruhe Institute of Technology (KIT), Institute for Meteorology and Climate Research, Hermann-von-Helmholtz-Platz 1, 76344 Eggenstein-Leopoldshafen, GermanyKarlsruhe Institute of Technology (KIT), Institute for Meteorology and Climate Research, Hermann-von-Helmholtz-Platz 1, 76344 Eggenstein-Leopoldshafen, GermanyAtmospheric liquid and solid water particles are stabilized if they are coated with either negative or positive electric charge. The surface charge causes an increase of the partial pressure of water vapour close to the surface of each particle, effectively allowing the particles to remain in their condensed phase even if the environmental relative humidity drops below unity. The theory, briefly presented in this paper, predicts a zero parameter relation between surface charge density and water vapour pressure. This relation was tested in a series of Electrodynamic Balance experiments. The measurements were performed by stabilizing charged droplets of pure water near an ice-surface. We observed a divergence in radius as the temperature approached the freezing point from below. We find that the measurements confirm the theory within the experimental uncertainty. In some cases this generally overlooked effect may have impact on cloud processes and on results produced by Electrodynamic Balance experiments.http://www.atmos-chem-phys.net/11/2031/2011/acp-11-2031-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. K. Nielsen
C. Maus
D. Rzesanke
T. Leisner
spellingShingle J. K. Nielsen
C. Maus
D. Rzesanke
T. Leisner
Charge induced stability of water droplets in subsaturated environment
Atmospheric Chemistry and Physics
author_facet J. K. Nielsen
C. Maus
D. Rzesanke
T. Leisner
author_sort J. K. Nielsen
title Charge induced stability of water droplets in subsaturated environment
title_short Charge induced stability of water droplets in subsaturated environment
title_full Charge induced stability of water droplets in subsaturated environment
title_fullStr Charge induced stability of water droplets in subsaturated environment
title_full_unstemmed Charge induced stability of water droplets in subsaturated environment
title_sort charge induced stability of water droplets in subsaturated environment
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2011-03-01
description Atmospheric liquid and solid water particles are stabilized if they are coated with either negative or positive electric charge. The surface charge causes an increase of the partial pressure of water vapour close to the surface of each particle, effectively allowing the particles to remain in their condensed phase even if the environmental relative humidity drops below unity. The theory, briefly presented in this paper, predicts a zero parameter relation between surface charge density and water vapour pressure. This relation was tested in a series of Electrodynamic Balance experiments. The measurements were performed by stabilizing charged droplets of pure water near an ice-surface. We observed a divergence in radius as the temperature approached the freezing point from below. We find that the measurements confirm the theory within the experimental uncertainty. In some cases this generally overlooked effect may have impact on cloud processes and on results produced by Electrodynamic Balance experiments.
url http://www.atmos-chem-phys.net/11/2031/2011/acp-11-2031-2011.pdf
work_keys_str_mv AT jknielsen chargeinducedstabilityofwaterdropletsinsubsaturatedenvironment
AT cmaus chargeinducedstabilityofwaterdropletsinsubsaturatedenvironment
AT drzesanke chargeinducedstabilityofwaterdropletsinsubsaturatedenvironment
AT tleisner chargeinducedstabilityofwaterdropletsinsubsaturatedenvironment
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