A Review of Aerosol Nanoparticle Formation from Ions

Ion-induced nucleation (IIN) mechanism has been widely accepted as an efficient source of new particle formation in the middle and upper troposphere. However, there have been debates on its contribution to the nucleation events observed in the boundary layer. To reveal the current understanding of I...

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Main Authors: Qing Li, Jingkun Jiang, Jiming Hao
Format: Article
Language:English
Published: Hosokawa Powder Technology Foundation 2014-10-01
Series:KONA Powder and Particle Journal
Subjects:
Online Access:https://www.jstage.jst.go.jp/article/kona/32/0/32_2015013/_html/-char/en
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spelling doaj-208f45df400249b79c30012363e845bb2021-02-03T00:50:30ZengHosokawa Powder Technology FoundationKONA Powder and Particle Journal0288-45342187-55372014-10-01320577410.14356/kona.2015013konaA Review of Aerosol Nanoparticle Formation from IonsQing Li0Jingkun Jiang1Jiming Hao2State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, ChinaState Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, ChinaState Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, ChinaIon-induced nucleation (IIN) mechanism has been widely accepted as an efficient source of new particle formation in the middle and upper troposphere. However, there have been debates on its contribution to the nucleation events observed in the boundary layer. To reveal the current understanding of IINs, we here summarise investigations on microphysical mechanisms of aerosol formation from ions, i.e., ion induced homogeneous nucleation (HN). The basic formation steps of ion-induced HN include primary ion production, charged cluster formation from ions, and stable nanoparticle formation from clusters. Two essential controlling processes (ion generation and formation of condensable species) are emphasized in the viewpoint of plasma performance for three case studies, i.e., galactic cosmic ray travelling in the troposphere, lightning discharges, and charging processes by aerosol chargers. The first two cases result in IINs due to the simultaneous generation of ions and condensable species (such as H2SO4 and oxidized organic vapours) from oxidizing trace atmospheric molecules. The third case leads to ion-induced clustering or nucleation in aerosol chargers. Due to a relatively short residence time in chargers (normally less than 1 minute), big charged clusters often exist in the outgoing aerosol flows.https://www.jstage.jst.go.jp/article/kona/32/0/32_2015013/_html/-char/enion-induced nucleationcharged clustersplasmaslightningcosmic rayschargers
collection DOAJ
language English
format Article
sources DOAJ
author Qing Li
Jingkun Jiang
Jiming Hao
spellingShingle Qing Li
Jingkun Jiang
Jiming Hao
A Review of Aerosol Nanoparticle Formation from Ions
KONA Powder and Particle Journal
ion-induced nucleation
charged clusters
plasmas
lightning
cosmic rays
chargers
author_facet Qing Li
Jingkun Jiang
Jiming Hao
author_sort Qing Li
title A Review of Aerosol Nanoparticle Formation from Ions
title_short A Review of Aerosol Nanoparticle Formation from Ions
title_full A Review of Aerosol Nanoparticle Formation from Ions
title_fullStr A Review of Aerosol Nanoparticle Formation from Ions
title_full_unstemmed A Review of Aerosol Nanoparticle Formation from Ions
title_sort review of aerosol nanoparticle formation from ions
publisher Hosokawa Powder Technology Foundation
series KONA Powder and Particle Journal
issn 0288-4534
2187-5537
publishDate 2014-10-01
description Ion-induced nucleation (IIN) mechanism has been widely accepted as an efficient source of new particle formation in the middle and upper troposphere. However, there have been debates on its contribution to the nucleation events observed in the boundary layer. To reveal the current understanding of IINs, we here summarise investigations on microphysical mechanisms of aerosol formation from ions, i.e., ion induced homogeneous nucleation (HN). The basic formation steps of ion-induced HN include primary ion production, charged cluster formation from ions, and stable nanoparticle formation from clusters. Two essential controlling processes (ion generation and formation of condensable species) are emphasized in the viewpoint of plasma performance for three case studies, i.e., galactic cosmic ray travelling in the troposphere, lightning discharges, and charging processes by aerosol chargers. The first two cases result in IINs due to the simultaneous generation of ions and condensable species (such as H2SO4 and oxidized organic vapours) from oxidizing trace atmospheric molecules. The third case leads to ion-induced clustering or nucleation in aerosol chargers. Due to a relatively short residence time in chargers (normally less than 1 minute), big charged clusters often exist in the outgoing aerosol flows.
topic ion-induced nucleation
charged clusters
plasmas
lightning
cosmic rays
chargers
url https://www.jstage.jst.go.jp/article/kona/32/0/32_2015013/_html/-char/en
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