Electrostatic charging of wind-blown dust and implications on dust transport

It is well known that electric fields occur in wind-blown dust, due to the triboelectric charging of particles as they collide. Triboelectric charging, or contact electrification, is a poorly understood and complex phenomenon. It is especially important in granular systems, as the high surface-to-vo...

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Main Authors: Toth Joseph R., Rajupet Siddharth, Squire Henry, Volbers Blaire, Zhou Jùn, Li Xie, Sankaran R. Mohan, Lacks Daniel J.
Format: Article
Language:English
Published: EDP Sciences 2019-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/25/e3sconf_caduc2019_02011.pdf
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spelling doaj-1c91877909f24e8fa1c0dc12c4e9b8af2021-04-02T15:20:52ZengEDP SciencesE3S Web of Conferences2267-12422019-01-01990201110.1051/e3sconf/20199902011e3sconf_caduc2019_02011Electrostatic charging of wind-blown dust and implications on dust transportToth Joseph R.Rajupet SiddharthSquire HenryVolbers BlaireZhou JùnLi XieSankaran R. MohanLacks Daniel J.It is well known that electric fields occur in wind-blown dust, due to the triboelectric charging of particles as they collide. Triboelectric charging, or contact electrification, is a poorly understood and complex phenomenon. It is especially important in granular systems, as the high surface-to-volume ratio can lead to the build-up of large amounts of charge. A particularly surprising effect, which is important in dust systems, is that charge transfer occurs in systems of a single composition, such that there is a particle-size dependent polarity of the particles. Here, we use a combined experimental and theoretical approach to elucidate the electrostatic charging that occurs during dust storms, and the effects of this electrostatic charging on dust transport. We create laboratory-scale wind-blown dust systems, and study the electrostatic charging. We find that larger particles tend to charge positive and to stay at or near the sand bed, while smaller particles tend to charge negative and get lofted to higher elevations. This self-segregating of charged particles would lead to electric fields within a dust storm. Our results show that electric fields then increase the dust transport by more easily lofting charged particles.https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/25/e3sconf_caduc2019_02011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Toth Joseph R.
Rajupet Siddharth
Squire Henry
Volbers Blaire
Zhou Jùn
Li Xie
Sankaran R. Mohan
Lacks Daniel J.
spellingShingle Toth Joseph R.
Rajupet Siddharth
Squire Henry
Volbers Blaire
Zhou Jùn
Li Xie
Sankaran R. Mohan
Lacks Daniel J.
Electrostatic charging of wind-blown dust and implications on dust transport
E3S Web of Conferences
author_facet Toth Joseph R.
Rajupet Siddharth
Squire Henry
Volbers Blaire
Zhou Jùn
Li Xie
Sankaran R. Mohan
Lacks Daniel J.
author_sort Toth Joseph R.
title Electrostatic charging of wind-blown dust and implications on dust transport
title_short Electrostatic charging of wind-blown dust and implications on dust transport
title_full Electrostatic charging of wind-blown dust and implications on dust transport
title_fullStr Electrostatic charging of wind-blown dust and implications on dust transport
title_full_unstemmed Electrostatic charging of wind-blown dust and implications on dust transport
title_sort electrostatic charging of wind-blown dust and implications on dust transport
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2019-01-01
description It is well known that electric fields occur in wind-blown dust, due to the triboelectric charging of particles as they collide. Triboelectric charging, or contact electrification, is a poorly understood and complex phenomenon. It is especially important in granular systems, as the high surface-to-volume ratio can lead to the build-up of large amounts of charge. A particularly surprising effect, which is important in dust systems, is that charge transfer occurs in systems of a single composition, such that there is a particle-size dependent polarity of the particles. Here, we use a combined experimental and theoretical approach to elucidate the electrostatic charging that occurs during dust storms, and the effects of this electrostatic charging on dust transport. We create laboratory-scale wind-blown dust systems, and study the electrostatic charging. We find that larger particles tend to charge positive and to stay at or near the sand bed, while smaller particles tend to charge negative and get lofted to higher elevations. This self-segregating of charged particles would lead to electric fields within a dust storm. Our results show that electric fields then increase the dust transport by more easily lofting charged particles.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/25/e3sconf_caduc2019_02011.pdf
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AT squirehenry electrostaticchargingofwindblowndustandimplicationsondusttransport
AT volbersblaire electrostaticchargingofwindblowndustandimplicationsondusttransport
AT zhoujun electrostaticchargingofwindblowndustandimplicationsondusttransport
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