Offshore Structures 1992
DOI: 10.1007/978-1-4471-3193-9_2
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Features of Offshore Structures

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Cited by 7 publications
(5 citation statements)
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“…Following Clauss et al (1992), the fluid–structure interaction problem with rigid bodies can be solved by assuming that the velocity gradients induced by the body in the surrounding fluid are negligible. Clauss et al (1992) determined that this condition arises when 2 R / λ < 0.2, as in this case.…”
Section: Numerical Simulation and Experimental Validationmentioning
confidence: 99%
See 1 more Smart Citation
“…Following Clauss et al (1992), the fluid–structure interaction problem with rigid bodies can be solved by assuming that the velocity gradients induced by the body in the surrounding fluid are negligible. Clauss et al (1992) determined that this condition arises when 2 R / λ < 0.2, as in this case.…”
Section: Numerical Simulation and Experimental Validationmentioning
confidence: 99%
“…Following Clauss et al (1992), the fluid–structure interaction problem with rigid bodies can be solved by assuming that the velocity gradients induced by the body in the surrounding fluid are negligible. Clauss et al (1992) determined that this condition arises when 2 R / λ < 0.2, as in this case. Therefore, we present the potential model results computed using the numerical package PETSc-FEM (Sonzogni et al , 2002; Storti et al , 2000; D’Elía et al , 2002) to add information for comparison.…”
Section: Numerical Simulation and Experimental Validationmentioning
confidence: 99%
“…Water is assumed to be incompressible, nonviscous and irrotational. A velocity potential Φ=Φ(x,y,z,t) can be used to describe the fluid velocity vector V (x, y, z, t)=(u, v, w) at time t at the point x =(x, y, z) in a Cartesian coordinate system48–69. Fig 14.…”
Section: Outline Of Design and Analysismentioning
confidence: 99%
“…Water is assumed to be incompressible, nonviscous and irrotational. A velocity potential Φ=Φ(x,y,z,t) can be used to describe the fluid velocity vector V (x,y,z,t)=(u,v,w) at time t at the point x = ( x, y, z ) in a Cartesian coordinate system48–69. The velocity vector V (x, y, z, t)=(u, v, w) can be expressed by the following equation under the assumption of linear wave theory of small amplitude where i , j , k are unit vectors along the x ‐, y ‐ and z ‐axes, respectively.…”
Section: Appendix: Amentioning
confidence: 99%
“…Most of the literature acknowledges that the wave spectrum of marine states has a period range from 3 s to 20 s (frequency from 0.33 Hz to 0.05 Hz) [1][2][3]. Wave loads are dynamic loads by nature, which are roughly described by wave theories or described by the wave spectrum (random waves).…”
Section: Introductionmentioning
confidence: 99%