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Original Research Paper

Surface gravity wave scattering by multiple energy absorbing structures of variable horizontal porosity

ORCID Icon, ORCID Icon & ORCID Icon
Pages 504-526 | Received 24 Oct 2019, Accepted 06 Jul 2020, Published online: 10 Sep 2020
 

ABSTRACT

The oblique wave scattering by fully-extended two-layered, three-layered and submerged two-layered porous structures occupying finite width is reported using an analytical model based on the eigenfunction expansion method. The fully extended two-layered structure is composed of two porosities and friction factors in the surface porous layer and the bottom porous layer. In addition, the three-layered energy-absorbing structure is composed of two-porous layers along with the bottom rigid layer to replace the natural seabed variation. Further, the study is extended for multiple energy-absorbing structures to report the impact of free spacing available between the two subsequent structures on fluid resonance. The two-layered porous structure dispersion relation is derived and solved using step approach and Newton-Raphson method. The derived analytical results are validated with the published results of notable authors. The effect of the surface and bottom layers porosity, friction factor, free spacing, structural width, number of structures, and angle of contact on the wave scattering is reported. Finally, the comparative study between the single and multiple energy absorbing structures of multiple horizontal layers is discussed. Further, the significance of the critical angle of contact and fluid resonance for better wave blocking is presented precisely, which is essential for the coastal engineers to design offshore structures.

Nomenclature

aj=

depth of each porous and rigid layers

bN=

positions of the energy absorbing structure

Cf=

turbulent resistant coefficient

dj=

width of each energy absorbing structure

d=

cumulative structural width

fj=

linearized friction factor in each of the porous layers

fjn=

vertical eigenfunction in each of the regions

g=

acceleration due to gravity

hj=

water depth in each region

i=

imaginary number

Kd=

energy dissipation

Kip=

intrinsic permeability

Kr=

reflection coefficient

Kt=

transmission coefficient

kjn=

wave number in the x-direction

l=

wave number in z-direction

M=

truncated number

N=

number of energy absorbing structures

q=

instantaneous Eulerian velocity vector

R10=

complex amplitude of the reflected wave

sj=

inertial force in each of the porous layer

T30=

complex amplitude of the transmitted wave

t=

time

ζj=

free surface wave elevation

ρ=

density of water

ω=

wave frequency

λ=

wavelength

ϕ=

velocity potential

δmn=

Kronecker delta

θ=

angle of contact

γjn=

wave number in y-direction

εj=

porosity in each of the porous layer

ν=

kinematic viscosity

Acknowledgments

The authors are grateful to the Ministry of Human Resources Development (MHRD) Government of India and the National Institute of Technology Karnataka Surathkal for providing necessary facilities for pursuing the research work. DK acknowledges Science and Engineering Research Board (SERB), India through research grant CRG/2018/004184.

Disclosure statement

No potential conflict of interest was reported by the authors.

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