Generation of Gravity Waves by Pedal-Wavemakers

Experimental wave generation in channels is usually achieved through wavemakers (moving paddles) acting on the surface of the water. Although practical for engineering purposes, wavemakers have issues: they perform poorly in the generation of long waves and create evanescent waves in their vicinity....

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Main Authors: Isis Vivanco, Bruce Cartwright, A. Ledesma Araujo, Leonardo Gordillo, Juan F. Marin
Format: Article
Language:English
Published: MDPI AG 2021-06-01
Series:Fluids
Subjects:
Online Access:https://www.mdpi.com/2311-5521/6/6/222
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spelling doaj-81d76169beaf4fbabd1ccfc9483bc4942021-07-01T00:04:59ZengMDPI AGFluids2311-55212021-06-01622222210.3390/fluids6060222Generation of Gravity Waves by Pedal-WavemakersIsis Vivanco0Bruce Cartwright1A. Ledesma Araujo2Leonardo Gordillo3Juan F. Marin4Departamento de Física, Facultad de Ciencia, Universidad de Santiago de Chile, Usach, Av. Ecuador 3493, Estación Central, Santiago 9160000, ChilePacific Engineering Systems International, 277–279 Broadway, Glebe, NSW 2037, AustraliaDepartamento de Física, Facultad de Ciencia, Universidad de Santiago de Chile, Usach, Av. Ecuador 3493, Estación Central, Santiago 9160000, ChileDepartamento de Física, Facultad de Ciencia, Universidad de Santiago de Chile, Usach, Av. Ecuador 3493, Estación Central, Santiago 9160000, ChileDepartamento de Física, Facultad de Ciencia, Universidad de Santiago de Chile, Usach, Av. Ecuador 3493, Estación Central, Santiago 9160000, ChileExperimental wave generation in channels is usually achieved through wavemakers (moving paddles) acting on the surface of the water. Although practical for engineering purposes, wavemakers have issues: they perform poorly in the generation of long waves and create evanescent waves in their vicinity. In this article, we introduce a framework for wave generation through the action of an underwater multipoint mechanism: the pedal-wavemaking method. Our multipoint action makes each point of the bottom move with a prescribed pedalling-like motion. We analyse the linear response of waves in a uniform channel in terms of the wavelength of the bottom action. The framework naturally solves the problem of the performance for long waves and replaces evanescent waves by a thin boundary layer at the bottom of the channel. We also show that proper synchronisation of the orbital motion on the bottom can produce waves that mimic deep water waves. This last feature has been proved to be useful to study fluid–structure interaction in simulations based on smoothed particle hydrodynamics.https://www.mdpi.com/2311-5521/6/6/222gravity surface waveswave-makerswater-wave generationcomputational fluid dynamics
collection DOAJ
language English
format Article
sources DOAJ
author Isis Vivanco
Bruce Cartwright
A. Ledesma Araujo
Leonardo Gordillo
Juan F. Marin
spellingShingle Isis Vivanco
Bruce Cartwright
A. Ledesma Araujo
Leonardo Gordillo
Juan F. Marin
Generation of Gravity Waves by Pedal-Wavemakers
Fluids
gravity surface waves
wave-makers
water-wave generation
computational fluid dynamics
author_facet Isis Vivanco
Bruce Cartwright
A. Ledesma Araujo
Leonardo Gordillo
Juan F. Marin
author_sort Isis Vivanco
title Generation of Gravity Waves by Pedal-Wavemakers
title_short Generation of Gravity Waves by Pedal-Wavemakers
title_full Generation of Gravity Waves by Pedal-Wavemakers
title_fullStr Generation of Gravity Waves by Pedal-Wavemakers
title_full_unstemmed Generation of Gravity Waves by Pedal-Wavemakers
title_sort generation of gravity waves by pedal-wavemakers
publisher MDPI AG
series Fluids
issn 2311-5521
publishDate 2021-06-01
description Experimental wave generation in channels is usually achieved through wavemakers (moving paddles) acting on the surface of the water. Although practical for engineering purposes, wavemakers have issues: they perform poorly in the generation of long waves and create evanescent waves in their vicinity. In this article, we introduce a framework for wave generation through the action of an underwater multipoint mechanism: the pedal-wavemaking method. Our multipoint action makes each point of the bottom move with a prescribed pedalling-like motion. We analyse the linear response of waves in a uniform channel in terms of the wavelength of the bottom action. The framework naturally solves the problem of the performance for long waves and replaces evanescent waves by a thin boundary layer at the bottom of the channel. We also show that proper synchronisation of the orbital motion on the bottom can produce waves that mimic deep water waves. This last feature has been proved to be useful to study fluid–structure interaction in simulations based on smoothed particle hydrodynamics.
topic gravity surface waves
wave-makers
water-wave generation
computational fluid dynamics
url https://www.mdpi.com/2311-5521/6/6/222
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AT aledesmaaraujo generationofgravitywavesbypedalwavemakers
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AT juanfmarin generationofgravitywavesbypedalwavemakers
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