Three-dimensional interaction between uniform current and a submerged horizontal cylinder in an ice-covered channel

The problem of interaction of a uniform current with a submerged horizontal circular cylinder in an ice-covered channel is considered. The fluid flow is described by linearized velocity potential theory and the ice sheet is treated as a thin elastic plate. The potential due to a source or the Green...

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Main Authors: Yang, YF, Wu, GX, Ren, K
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2021
Subjects:
Online Access:https://discovery.ucl.ac.uk/id/eprint/10136436/1/Yang%20Wu%20Ren%20%282021JFM%29_new.pdf
https://discovery.ucl.ac.uk/id/eprint/10136436/
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spelling ftucl:oai:eprints.ucl.ac.uk.OAI2:10136436 2023-12-24T10:17:35+01:00 Three-dimensional interaction between uniform current and a submerged horizontal cylinder in an ice-covered channel Yang, YF Wu, GX Ren, K 2021-12-10 text https://discovery.ucl.ac.uk/id/eprint/10136436/1/Yang%20Wu%20Ren%20%282021JFM%29_new.pdf https://discovery.ucl.ac.uk/id/eprint/10136436/ eng eng Cambridge University Press (CUP) https://discovery.ucl.ac.uk/id/eprint/10136436/1/Yang%20Wu%20Ren%20%282021JFM%29_new.pdf https://discovery.ucl.ac.uk/id/eprint/10136436/ open Journal of Fluid Mechanics , 928 , Article A4. (2021) Article 2021 ftucl 2023-11-27T13:07:31Z The problem of interaction of a uniform current with a submerged horizontal circular cylinder in an ice-covered channel is considered. The fluid flow is described by linearized velocity potential theory and the ice sheet is treated as a thin elastic plate. The potential due to a source or the Green function satisfying all boundary conditions apart from that on the body surface is first derived. This can be used to derive the boundary integral equation for a body of arbitrary shape. It can also be used to obtain the solution due to multipoles by differentiating the Green function with its position directly. For a transverse circular cylinder, through distributing multipoles along its centre line, the velocity potential can be written in an infinite series with unknown coefficients, which can be determined from the impermeable condition on a body surface. A major feature here is that different from the free surface problem, or a channel without the ice sheet cover, this problem is fully three-dimensional because of the constraints along the intersection of the ice sheet with the channel wall. It has been also confirmed that there is an infinite number of critical speeds. Whenever the current speed passes a critical value, the force on the body and wave pattern change rapidly, and two more wave components are generated at the far-field. Extensive results are provided for hydroelastic waves and hydrodynamic forces when the ice sheet is under different edge conditions, and the insight of their physical features is discussed. Article in Journal/Newspaper Ice Sheet University College London: UCL Discovery
institution Open Polar
collection University College London: UCL Discovery
op_collection_id ftucl
language English
description The problem of interaction of a uniform current with a submerged horizontal circular cylinder in an ice-covered channel is considered. The fluid flow is described by linearized velocity potential theory and the ice sheet is treated as a thin elastic plate. The potential due to a source or the Green function satisfying all boundary conditions apart from that on the body surface is first derived. This can be used to derive the boundary integral equation for a body of arbitrary shape. It can also be used to obtain the solution due to multipoles by differentiating the Green function with its position directly. For a transverse circular cylinder, through distributing multipoles along its centre line, the velocity potential can be written in an infinite series with unknown coefficients, which can be determined from the impermeable condition on a body surface. A major feature here is that different from the free surface problem, or a channel without the ice sheet cover, this problem is fully three-dimensional because of the constraints along the intersection of the ice sheet with the channel wall. It has been also confirmed that there is an infinite number of critical speeds. Whenever the current speed passes a critical value, the force on the body and wave pattern change rapidly, and two more wave components are generated at the far-field. Extensive results are provided for hydroelastic waves and hydrodynamic forces when the ice sheet is under different edge conditions, and the insight of their physical features is discussed.
format Article in Journal/Newspaper
author Yang, YF
Wu, GX
Ren, K
spellingShingle Yang, YF
Wu, GX
Ren, K
Three-dimensional interaction between uniform current and a submerged horizontal cylinder in an ice-covered channel
author_facet Yang, YF
Wu, GX
Ren, K
author_sort Yang, YF
title Three-dimensional interaction between uniform current and a submerged horizontal cylinder in an ice-covered channel
title_short Three-dimensional interaction between uniform current and a submerged horizontal cylinder in an ice-covered channel
title_full Three-dimensional interaction between uniform current and a submerged horizontal cylinder in an ice-covered channel
title_fullStr Three-dimensional interaction between uniform current and a submerged horizontal cylinder in an ice-covered channel
title_full_unstemmed Three-dimensional interaction between uniform current and a submerged horizontal cylinder in an ice-covered channel
title_sort three-dimensional interaction between uniform current and a submerged horizontal cylinder in an ice-covered channel
publisher Cambridge University Press (CUP)
publishDate 2021
url https://discovery.ucl.ac.uk/id/eprint/10136436/1/Yang%20Wu%20Ren%20%282021JFM%29_new.pdf
https://discovery.ucl.ac.uk/id/eprint/10136436/
genre Ice Sheet
genre_facet Ice Sheet
op_source Journal of Fluid Mechanics , 928 , Article A4. (2021)
op_relation https://discovery.ucl.ac.uk/id/eprint/10136436/1/Yang%20Wu%20Ren%20%282021JFM%29_new.pdf
https://discovery.ucl.ac.uk/id/eprint/10136436/
op_rights open
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