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Effect of a submerged vertical barrier on flexural gravity waves
Published in
2011
Volume: 49
   
Issue: 8
Pages: 755 - 767
Abstract
An explicit solution is provided for the scattering of flexural gravity waves by a rigid vertical barrier submerged in an infinite depth of water. By applying recently developed mode-coupling relation for eigenfunctions, the mixed boundary value problem has been converted to solve dual integral equations with kernel consisting of trigonometric functions. And then complete analytical solutions are derived with an aid of singular integral equations whose solutions are bounded at the end points. The important hydrodynamical scattering quantities such as reflection and transmission coefficients associated with the flexural gravity wave scattering have been obtained analytically in terms of modified Bessel functions and Struve functions. It is observed that these quantities are sensitive to both combined as well as individual effect of plate thickness and barrier depth of submergence. Numerical results are computed and explained graphically for different parameters such as time period and non-dimensional wave length. Further, the effect of compressive force and plate thickness on the flexural gravity waves against a submerged vertical barrier is studied. © 2011 Elsevier Ltd. All rights reserved.
About the journal
JournalInternational Journal of Engineering Science
ISSN00207225
Open AccessNo
Concepts (26)
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    Analytical solutions
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    Compressive forces
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    DUAL INTEGRAL EQUATIONS
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    Eigen function
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    END POINTS
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    Explicit solutions
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    FLEXURAL-GRAVITY WAVES
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    Mixed boundary-value problem
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    MODE COUPLING
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    MODIFIED BESSEL FUNCTION
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    Numerical results
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    Plate thickness
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    Reflection and transmission coefficients
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    REFLECTION COEFFICIENT
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    SINGULAR INTEGRAL EQUATIONS
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    Time-periods
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    Trigonometric functions
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    Carrier concentration
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    Eigenvalues and eigenfunctions
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    Gravity waves
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    Harmonic analysis
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    Hydrodynamics
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    Integral equations
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    Scattering
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    Waves
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    Gravitational effects