An improved criterion for new particle formation in diverse atmospheric environments

A dimensionless theory for new particle formation (NPF) was developed, using an aerosol population balance model incorporating recent developments in nucleation rates and measured particle growth rates. Based on this theoretical analysis, it was shown that a dimensionless parameter <i>...

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Main Authors: C. Kuang, I. Riipinen, S.-L. Sihto, M. Kulmala, A. V. McCormick, P. H. McMurry
Format: Article
Language:English
Published: Copernicus Publications 2010-09-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/10/8469/2010/acp-10-8469-2010.pdf
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author C. Kuang
I. Riipinen
S.-L. Sihto
M. Kulmala
A. V. McCormick
P. H. McMurry
author_facet C. Kuang
I. Riipinen
S.-L. Sihto
M. Kulmala
A. V. McCormick
P. H. McMurry
author_sort C. Kuang
collection DOAJ
description A dimensionless theory for new particle formation (NPF) was developed, using an aerosol population balance model incorporating recent developments in nucleation rates and measured particle growth rates. Based on this theoretical analysis, it was shown that a dimensionless parameter <i>L</i><sub>Γ</sub>, characterizing the ratio of the particle scavenging loss rate to the particle growth rate, exclusively determined whether or not NPF would occur on a particular day. This parameter determines the probability that a nucleated particle will grow to a detectable size before being lost by coagulation with the pre-existing aerosol. Cluster-cluster coagulation was shown to contribute negligibly to this survival probability under conditions pertinent to the atmosphere. Data acquired during intensive measurement campaigns in Tecamac (MILAGRO), Atlanta (ANARChE), Boulder, and Hyytiälä (QUEST II, QUEST IV, and EUCAARI) were used to test the validity of <i>L</i><sub>Γ</sub> as an NPF criterion. Measurements included aerosol size distributions down to 3 nm and gas-phase sulfuric acid concentrations. The model was applied to seventy-seven NPF events and nineteen non-events (characterized by growth of pre-existing aerosol without NPF) measured in diverse environments with broad ranges in sulfuric acid concentrations, ultrafine number concentrations, aerosol surface areas, and particle growth rates (nearly two orders of magnitude). Across this diverse data set, a nominal value of <i>L</i><sub>Γ</sub>=0.7 was found to determine the boundary for the occurrence of NPF, with NPF occurring when <i>L</i><sub>Γ</sub><0.7 and being suppressed when <i>L</i><sub>Γ</sub>>0.7. Moreover, nearly 45% of measured <i>L</i><sub>Γ</sub> values associated with NPF fell in the relatively narrow range of 0.1<<i>L</i><sub>Γ</sub><0.3.
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spelling doaj.art-4c3bfcbf0a2148a8a9065371f7fefa942022-12-21T18:00:13ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242010-09-0110178469848010.5194/acp-10-8469-2010An improved criterion for new particle formation in diverse atmospheric environmentsC. KuangI. RiipinenS.-L. SihtoM. KulmalaA. V. McCormickP. H. McMurryA dimensionless theory for new particle formation (NPF) was developed, using an aerosol population balance model incorporating recent developments in nucleation rates and measured particle growth rates. Based on this theoretical analysis, it was shown that a dimensionless parameter <i>L</i><sub>Γ</sub>, characterizing the ratio of the particle scavenging loss rate to the particle growth rate, exclusively determined whether or not NPF would occur on a particular day. This parameter determines the probability that a nucleated particle will grow to a detectable size before being lost by coagulation with the pre-existing aerosol. Cluster-cluster coagulation was shown to contribute negligibly to this survival probability under conditions pertinent to the atmosphere. Data acquired during intensive measurement campaigns in Tecamac (MILAGRO), Atlanta (ANARChE), Boulder, and Hyytiälä (QUEST II, QUEST IV, and EUCAARI) were used to test the validity of <i>L</i><sub>Γ</sub> as an NPF criterion. Measurements included aerosol size distributions down to 3 nm and gas-phase sulfuric acid concentrations. The model was applied to seventy-seven NPF events and nineteen non-events (characterized by growth of pre-existing aerosol without NPF) measured in diverse environments with broad ranges in sulfuric acid concentrations, ultrafine number concentrations, aerosol surface areas, and particle growth rates (nearly two orders of magnitude). Across this diverse data set, a nominal value of <i>L</i><sub>Γ</sub>=0.7 was found to determine the boundary for the occurrence of NPF, with NPF occurring when <i>L</i><sub>Γ</sub><0.7 and being suppressed when <i>L</i><sub>Γ</sub>>0.7. Moreover, nearly 45% of measured <i>L</i><sub>Γ</sub> values associated with NPF fell in the relatively narrow range of 0.1<<i>L</i><sub>Γ</sub><0.3.http://www.atmos-chem-phys.net/10/8469/2010/acp-10-8469-2010.pdf
spellingShingle C. Kuang
I. Riipinen
S.-L. Sihto
M. Kulmala
A. V. McCormick
P. H. McMurry
An improved criterion for new particle formation in diverse atmospheric environments
Atmospheric Chemistry and Physics
title An improved criterion for new particle formation in diverse atmospheric environments
title_full An improved criterion for new particle formation in diverse atmospheric environments
title_fullStr An improved criterion for new particle formation in diverse atmospheric environments
title_full_unstemmed An improved criterion for new particle formation in diverse atmospheric environments
title_short An improved criterion for new particle formation in diverse atmospheric environments
title_sort improved criterion for new particle formation in diverse atmospheric environments
url http://www.atmos-chem-phys.net/10/8469/2010/acp-10-8469-2010.pdf
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