Different approaches in scattering of water waves by two submerged porous plates over an elastic sea-floor

IF 1.1 4区 地球科学 Q3 ASTRONOMY & ASTROPHYSICS Geophysical and Astrophysical Fluid Dynamics Pub Date : 2022-02-07 DOI:10.1080/03091929.2022.2025792
Ayan Chanda, S. Bora
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引用次数: 5

Abstract

A hydroelastic model is presented here to look into the scattering of oblique water waves by two totally submerged vertical porous plates, placed at some distance from each other, in a homogeneous fluid flowing over an elastic sea-floor. Consideration of Euler–Bernoulli beam equation allows the elastic sea-floor to be approximated as a thin elastic plate whereas the porous plates follow the porous wave-maker theory. The complete analytical solution, under the assumption of small-amplitude theory and structural response, is obtained by employing eigenfunction expansion and least square method. Subsequently, numerical computation for the reflection and transmission coefficients and energy loss are carried out and discussed for different values of the elasticity of the sea-floor, porosity of the porous plates and other structural parameters. The present study establishes that reflection of the waves exhibits an oscillatory behaviour. It further shows that, due to an increase in the inertial effect of the porous plate, the minima in wave reflection occurs. The vertical porous plates are found to dissipate a significant portion of the wave energy when an increase in the inertial effect of the porous plates takes place. Furthermore, wave transmission decreases significantly due to the energy dissipation by the elastic sea-floor. Significant variation in the elastic specification of the sea-floor commands considerable influence when the propagating wave impinges upon the submerged vertical porous plates. In order to validate the present model, the obtained results are compared with available results which points towards a good agreement.
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弹性海底上两个浸没的多孔板对水波散射的不同方法
本文提出了一个水弹性模型来研究斜水波在均匀流体流过弹性海底时,两个完全浸没的垂直多孔板之间的散射,它们彼此相距一定距离。考虑欧拉-伯努利梁方程,可以将弹性海床近似为弹性薄板,而多孔板则遵循多孔造波理论。采用特征函数展开和最小二乘法,在小振幅理论和结构响应假设下,得到了完整的解析解。随后,对不同海底弹性、多孔板孔隙率等结构参数下的反射透射系数和能量损失进行了数值计算,并进行了讨论。目前的研究表明,波的反射表现出振荡行为。进一步表明,由于多孔板的惯性效应增加,波反射出现极小值。当多孔板的惯性效应增加时,发现垂直多孔板耗散了波能量的很大一部分。此外,由于弹性海底的能量耗散,波的传播显著降低。当传播波撞击水下垂直多孔板时,海底弹性特性的显著变化会产生相当大的影响。为了验证该模型,将所得结果与已有结果进行了比较,结果表明两者吻合较好。
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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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