Translation-deformation coupling effects on the Rayleigh instability of an electrodynamically levitated charged droplet

The breakup pathway of the Rayleigh fission process observed experimentally using high-speed imaging of a charged drop levitated in an AC quadrupole trap is shown to undergo asymmetric breakup by ejecting a jet in the upward direction ((i.e., opposite to the direction of gravity)). To explain this t...

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Main Authors: Gawande, Neha, Mayya, Y. S., Thaokar, Rochish
Format: Article in Journal/Newspaper
Language:unknown
Published: arXiv 2021
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.2106.02092
https://arxiv.org/abs/2106.02092
id ftdatacite:10.48550/arxiv.2106.02092
record_format openpolar
spelling ftdatacite:10.48550/arxiv.2106.02092 2023-05-15T17:39:56+02:00 Translation-deformation coupling effects on the Rayleigh instability of an electrodynamically levitated charged droplet Gawande, Neha Mayya, Y. S. Thaokar, Rochish 2021 https://dx.doi.org/10.48550/arxiv.2106.02092 https://arxiv.org/abs/2106.02092 unknown arXiv Creative Commons Attribution Non Commercial Share Alike 4.0 International https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode cc-by-nc-sa-4.0 CC-BY-NC-SA Fluid Dynamics physics.flu-dyn FOS Physical sciences Article CreativeWork article Preprint 2021 ftdatacite https://doi.org/10.48550/arxiv.2106.02092 2022-03-10T14:48:18Z The breakup pathway of the Rayleigh fission process observed experimentally using high-speed imaging of a charged drop levitated in an AC quadrupole trap is shown to undergo asymmetric breakup by ejecting a jet in the upward direction ((i.e., opposite to the direction of gravity)). To explain this typical experimental observation, we carry out numerical calculations based on the boundary element method considering inertial droplets levitated electrodynamically using quadrupole electric fields. The simulations show that the gravity-induced downward shift in the equilibrium position of the drop in the trap causes significant, large-amplitude shape oscillations superimposed over the center-of-mass oscillations of the drop. An important observation here is that the shape oscillations due to the applied quadrupole fields, result in sufficient deformations that act as triggers for the onset of the instability below the Rayleigh limit, thereby admitting a sub-critical instability. The center-of-mass oscillations of the droplet within the trap, which follow the applied frequency, are out of phase with the applied AC signal. Thus the combined effect of shape deformations and dynamic position of the drop leads to an asymmetric breakup such that the Rayleigh fission occurs upwards via the ejection of a jet at the north-pole of the deformed drop. : 9 figures, 7 pages Article in Journal/Newspaper North Pole DataCite Metadata Store (German National Library of Science and Technology) North Pole
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Fluid Dynamics physics.flu-dyn
FOS Physical sciences
spellingShingle Fluid Dynamics physics.flu-dyn
FOS Physical sciences
Gawande, Neha
Mayya, Y. S.
Thaokar, Rochish
Translation-deformation coupling effects on the Rayleigh instability of an electrodynamically levitated charged droplet
topic_facet Fluid Dynamics physics.flu-dyn
FOS Physical sciences
description The breakup pathway of the Rayleigh fission process observed experimentally using high-speed imaging of a charged drop levitated in an AC quadrupole trap is shown to undergo asymmetric breakup by ejecting a jet in the upward direction ((i.e., opposite to the direction of gravity)). To explain this typical experimental observation, we carry out numerical calculations based on the boundary element method considering inertial droplets levitated electrodynamically using quadrupole electric fields. The simulations show that the gravity-induced downward shift in the equilibrium position of the drop in the trap causes significant, large-amplitude shape oscillations superimposed over the center-of-mass oscillations of the drop. An important observation here is that the shape oscillations due to the applied quadrupole fields, result in sufficient deformations that act as triggers for the onset of the instability below the Rayleigh limit, thereby admitting a sub-critical instability. The center-of-mass oscillations of the droplet within the trap, which follow the applied frequency, are out of phase with the applied AC signal. Thus the combined effect of shape deformations and dynamic position of the drop leads to an asymmetric breakup such that the Rayleigh fission occurs upwards via the ejection of a jet at the north-pole of the deformed drop. : 9 figures, 7 pages
format Article in Journal/Newspaper
author Gawande, Neha
Mayya, Y. S.
Thaokar, Rochish
author_facet Gawande, Neha
Mayya, Y. S.
Thaokar, Rochish
author_sort Gawande, Neha
title Translation-deformation coupling effects on the Rayleigh instability of an electrodynamically levitated charged droplet
title_short Translation-deformation coupling effects on the Rayleigh instability of an electrodynamically levitated charged droplet
title_full Translation-deformation coupling effects on the Rayleigh instability of an electrodynamically levitated charged droplet
title_fullStr Translation-deformation coupling effects on the Rayleigh instability of an electrodynamically levitated charged droplet
title_full_unstemmed Translation-deformation coupling effects on the Rayleigh instability of an electrodynamically levitated charged droplet
title_sort translation-deformation coupling effects on the rayleigh instability of an electrodynamically levitated charged droplet
publisher arXiv
publishDate 2021
url https://dx.doi.org/10.48550/arxiv.2106.02092
https://arxiv.org/abs/2106.02092
geographic North Pole
geographic_facet North Pole
genre North Pole
genre_facet North Pole
op_rights Creative Commons Attribution Non Commercial Share Alike 4.0 International
https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode
cc-by-nc-sa-4.0
op_rightsnorm CC-BY-NC-SA
op_doi https://doi.org/10.48550/arxiv.2106.02092
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