2019
DOI: 10.1103/physrevfluids.4.014808
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Hydroelastic wake on a thin elastic sheet floating on water

Abstract: We investigate the hydroelastic wake created by a perturbation moving at constant speed along a thin elastic sheet floating at the surface of deep water. Using a high-resolution cross-correlation imaging technique, we characterize the waves as a function of the perturbation speed, for different sheet thicknesses. The general theoretical expression for the dispersion relation of hydroelastic waves includes three components: gravity, bending and stretching. The bending modulus and the tension in the sheet are in… Show more

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Cited by 7 publications
(19 citation statements)
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“…As such, while we were focused on infinite-depth and finite-depth surface gravity waves due to a moving ship, our analysis can easily be adapted for applications with different dispersion relations. Typical examples that may be of interest include problems for which the effects of surface tension together with gravity are important [23,43,44], models for weakly damped ship waves [45], hydroelastic waves such as those on floating ice sheet [46,47], internal or surface waves due to a stratified fluid [13,48], and ship waves with constant vorticity [21,49] (although further modifications would be required in the latter case due to = (k, ψ )). Our results in Sec.…”
Section: Discussionmentioning
confidence: 99%
“…As such, while we were focused on infinite-depth and finite-depth surface gravity waves due to a moving ship, our analysis can easily be adapted for applications with different dispersion relations. Typical examples that may be of interest include problems for which the effects of surface tension together with gravity are important [23,43,44], models for weakly damped ship waves [45], hydroelastic waves such as those on floating ice sheet [46,47], internal or surface waves due to a stratified fluid [13,48], and ship waves with constant vorticity [21,49] (although further modifications would be required in the latter case due to = (k, ψ )). Our results in Sec.…”
Section: Discussionmentioning
confidence: 99%
“…As such, while we were focussed on infinite-depth and finite-depth surface gravity waves due to a moving ship, our analysis can easily be adapted for applications with different dispersion relations. Typical examples that may be of interest include problems for which the effects of surface tension together with gravity are important [22,34,39], models for weakly damped ship waves [40], hydroelastic waves such as those on floating ice sheet [41,42], internal or surface waves due to a stratified fluid [43], and ship waves with constant vorticity [20,44] (although further modifications would be required in the latter case due to Ω = Ω(k, ψ)). Our results in Sec.…”
Section: Discussionmentioning
confidence: 99%
“…Each arm of the "plus" shaped frame was clamped to a post and attached to crossed optical rails using translation stages. The hole was covered with a second Elastosil film, which becomes the "substrate" of the bilayer, with thicknesses of H = {20.9 ± 0.4, 51 ± 1, 104 ± 2, 213 ± 7, or 258 ± 2} µm as measured in reference [35]. Samples with intermediate substrate thickness were made by stacking Elastosil sheets with good adhesion between the films -sufficient that the films remained in good contact when strained.…”
Section: Experimental Methodsmentioning
confidence: 99%
“…We note that while there is no strain in the perpendicular direction, there is a tensile stress induced through Poisson's ratio which is smaller than that induced in the high-strain direction. The Elastosil films have a modulus E s = 1.11 ± 0.06 MPa [35], and making the reasonable assumption that the elastomer is incompressible then Poisson's ratio can be taken to be ν s = 0.5.…”
Section: Experimental Methodsmentioning
confidence: 99%