Waterfalls as sources of small charged aerosol particles

In this study, we measured the mobility distributions of cluster and intermediate ions with an ion spectrometer near a waterfall. We observed that the concentration of negative 1.5–10 nm ions was one-hundred fold higher than a reference point 100 m away from the waterfall. Also, the concen...

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Main Authors: L. Laakso, A. Hirsikko, T. Grönholm, M. Kulmala, A. Luts, T.-E. Parts
Format: Article
Language:English
Published: Copernicus Publications 2007-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/7/2271/2007/acp-7-2271-2007.pdf
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author L. Laakso
A. Hirsikko
T. Grönholm
M. Kulmala
A. Luts
T.-E. Parts
author_facet L. Laakso
A. Hirsikko
T. Grönholm
M. Kulmala
A. Luts
T.-E. Parts
author_sort L. Laakso
collection DOAJ
description In this study, we measured the mobility distributions of cluster and intermediate ions with an ion spectrometer near a waterfall. We observed that the concentration of negative 1.5–10 nm ions was one-hundred fold higher than a reference point 100 m away from the waterfall. Also, the concentration of positive intermediate ions was found to be higher than that at the reference point by a factor of ten. This difference was observed only at the smallest sizes; above 10 nm the difference was insignificant.
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spelling doaj.art-4344e6868645403a933c662d309c98902022-12-22T00:45:54ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242007-01-017922712275Waterfalls as sources of small charged aerosol particlesL. LaaksoA. HirsikkoT. GrönholmM. KulmalaA. LutsT.-E. PartsIn this study, we measured the mobility distributions of cluster and intermediate ions with an ion spectrometer near a waterfall. We observed that the concentration of negative 1.5–10 nm ions was one-hundred fold higher than a reference point 100 m away from the waterfall. Also, the concentration of positive intermediate ions was found to be higher than that at the reference point by a factor of ten. This difference was observed only at the smallest sizes; above 10 nm the difference was insignificant.http://www.atmos-chem-phys.net/7/2271/2007/acp-7-2271-2007.pdf
spellingShingle L. Laakso
A. Hirsikko
T. Grönholm
M. Kulmala
A. Luts
T.-E. Parts
Waterfalls as sources of small charged aerosol particles
Atmospheric Chemistry and Physics
title Waterfalls as sources of small charged aerosol particles
title_full Waterfalls as sources of small charged aerosol particles
title_fullStr Waterfalls as sources of small charged aerosol particles
title_full_unstemmed Waterfalls as sources of small charged aerosol particles
title_short Waterfalls as sources of small charged aerosol particles
title_sort waterfalls as sources of small charged aerosol particles
url http://www.atmos-chem-phys.net/7/2271/2007/acp-7-2271-2007.pdf
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AT tgronholm waterfallsassourcesofsmallchargedaerosolparticles
AT mkulmala waterfallsassourcesofsmallchargedaerosolparticles
AT aluts waterfallsassourcesofsmallchargedaerosolparticles
AT teparts waterfallsassourcesofsmallchargedaerosolparticles