Nanoparticle formation by ozonolysis of inducible plant volatiles

We present the first laboratory experiments of aerosol formation from oxidation of volatile organic species emitted by living plants, a process which for half a century has been known to take place in the atmosphere. We have treated white cabbage plants with methyl jasmonate in order to induce the p...

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Main Authors: J. Joutsensaari, M. Loivamäki, T. Vuorinen, P. Miettinen, A.-M. Nerg, J. K. Holopainen, A. Laaksonen
Format: Article
Language:English
Published: Copernicus Publications 2005-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/5/1489/2005/acp-5-1489-2005.pdf
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spelling doaj-a716313e0ef2471ca71e4150897292a72020-11-24T22:16:32ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242005-01-015614891495Nanoparticle formation by ozonolysis of inducible plant volatilesJ. JoutsensaariM. LoivamäkiM. LoivamäkiT. VuorinenP. MiettinenA.-M. NergJ. K. HolopainenA. LaaksonenWe present the first laboratory experiments of aerosol formation from oxidation of volatile organic species emitted by living plants, a process which for half a century has been known to take place in the atmosphere. We have treated white cabbage plants with methyl jasmonate in order to induce the production of monoterpenes and certain less-volatile sesqui- and homoterpenes. Ozone was introduced into the growth chamber in which the plants were placed, and the subsequent aerosol formation and growth of aerosols were monitored by measuring the particle size distributions continuously during the experiments. Our observations show similar particle formation rates as in the atmosphere but much higher growth rates. The results indicate that the concentrations of nonvolatile oxidation products of plant released precursors needed to induce the nucleation are roughly an order-of-magnitude higher than their concentrations during atmospheric nucleation events. Our results therefore suggest that if oxidized organics are involved in atmospheric nucleation events, their role is to participate in the growth of pre-existing molecular clusters rather than to form such clusters through homogeneous or ion-induced nucleation.http://www.atmos-chem-phys.net/5/1489/2005/acp-5-1489-2005.pdf
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language English
format Article
sources DOAJ
author J. Joutsensaari
M. Loivamäki
M. Loivamäki
T. Vuorinen
P. Miettinen
A.-M. Nerg
J. K. Holopainen
A. Laaksonen
spellingShingle J. Joutsensaari
M. Loivamäki
M. Loivamäki
T. Vuorinen
P. Miettinen
A.-M. Nerg
J. K. Holopainen
A. Laaksonen
Nanoparticle formation by ozonolysis of inducible plant volatiles
Atmospheric Chemistry and Physics
author_facet J. Joutsensaari
M. Loivamäki
M. Loivamäki
T. Vuorinen
P. Miettinen
A.-M. Nerg
J. K. Holopainen
A. Laaksonen
author_sort J. Joutsensaari
title Nanoparticle formation by ozonolysis of inducible plant volatiles
title_short Nanoparticle formation by ozonolysis of inducible plant volatiles
title_full Nanoparticle formation by ozonolysis of inducible plant volatiles
title_fullStr Nanoparticle formation by ozonolysis of inducible plant volatiles
title_full_unstemmed Nanoparticle formation by ozonolysis of inducible plant volatiles
title_sort nanoparticle formation by ozonolysis of inducible plant volatiles
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2005-01-01
description We present the first laboratory experiments of aerosol formation from oxidation of volatile organic species emitted by living plants, a process which for half a century has been known to take place in the atmosphere. We have treated white cabbage plants with methyl jasmonate in order to induce the production of monoterpenes and certain less-volatile sesqui- and homoterpenes. Ozone was introduced into the growth chamber in which the plants were placed, and the subsequent aerosol formation and growth of aerosols were monitored by measuring the particle size distributions continuously during the experiments. Our observations show similar particle formation rates as in the atmosphere but much higher growth rates. The results indicate that the concentrations of nonvolatile oxidation products of plant released precursors needed to induce the nucleation are roughly an order-of-magnitude higher than their concentrations during atmospheric nucleation events. Our results therefore suggest that if oxidized organics are involved in atmospheric nucleation events, their role is to participate in the growth of pre-existing molecular clusters rather than to form such clusters through homogeneous or ion-induced nucleation.
url http://www.atmos-chem-phys.net/5/1489/2005/acp-5-1489-2005.pdf
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