Barrier and bottom topography effects on hydroelastic response of floating elastic plate in a two-layer fluid

IF 1.1 4区 地球科学 Q3 ASTRONOMY & ASTROPHYSICS
N. Prasad, R. M. Prasad, Prashant Kumar, Pulkit Kumar, Chandra Mani Prasad
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引用次数: 0

Abstract

The prime intention of this article is to investigate the effect of variable bottom topography and a bottom-sitting porous barrier on the hydroelastic response of an elastic plate floating on a two-layer fluid using small amplitude wave theory. Galerkin's single-mode approximation in each layer for variable bottom topography and the method of eigenfunction expansion for the fluid region of uniform bottom topography are used as mathematical tools to detail the phenomena. In the variable bottom topography, a system of differential equations is solved. By applying matching conditions, jump conditions, and the appropriate boundary conditions, the solution is expressed as an algebraic linear system from which all the unknown constants are evaluated. The effects of different parameters related to the fluid, bottom topography, and porous barrier on the bending moment, shear force, and deflection of an elastic plate are explored. The variations in the bending moments, shear forces, and plate deflection with respect to fluid density are found to be in opposite trends, caused by surface and interfacial waves, respectively. Further, as the density ratio becomes closer to one, the bending moments, shear forces, and plate deflection tend to diminish for interfacial waves. The bottom effect on bending moments, shear forces, and plate deflection is minimal due to surface waves but significant due to interface waves with maximum amplitude in a concave up bottom. The plate deformation can be further reduced using a suitable barrier, as investigated in this article. The findings hold good potential for furthering our understanding of installing an elastic plate in a stratified fluid with fluctuating water depth.
屏障和底部地形对两层流体中浮动弹性板水弹性响应的影响
本文的主要目的是利用小振幅波理论研究变化的底部地形和底部的多孔屏障对浮在两层流体上的弹性板的水弹性响应的影响。采用变底地形的各层伽辽金单模近似法和均匀底地形流体区域的本征函数展开法作为数学工具来详细描述这一现象。在变底地形下,求解了一个微分方程组。通过应用匹配条件、跳跃条件和适当的边界条件,将解表示为一个代数线性系统,从中计算所有未知常数。探讨了流体、底部地形和多孔屏障等不同参数对弹性板的弯矩、剪力和挠度的影响。弯矩、剪力和板挠度随流体密度的变化趋势相反,分别由表面波和界面波引起。此外,当密度比接近于1时,界面波作用下的弯矩、剪力和板挠度趋于减小。由于表面波的作用,底部对弯矩、剪力和板挠度的影响最小,但由于底部凹向上的界面波的振幅最大,底部的影响很大。板的变形可以进一步减少使用适当的屏障,在本文中进行了研究。这一发现对于加深我们对在波动水深的分层流体中安装弹性板的理解具有良好的潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geophysical and Astrophysical Fluid Dynamics
Geophysical and Astrophysical Fluid Dynamics 地学天文-地球化学与地球物理
CiteScore
3.10
自引率
0.00%
发文量
14
审稿时长
>12 weeks
期刊介绍: Geophysical and Astrophysical Fluid Dynamics exists for the publication of original research papers and short communications, occasional survey articles and conference reports on the fluid mechanics of the earth and planets, including oceans, atmospheres and interiors, and the fluid mechanics of the sun, stars and other astrophysical objects. In addition, their magnetohydrodynamic behaviours are investigated. Experimental, theoretical and numerical studies of rotating, stratified and convecting fluids of general interest to geophysicists and astrophysicists appear. Properly interpreted observational results are also published.
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