Wave loads and seakeeping Flashcards
Draw a ship in a ship-fixed coordinate system. Show and give the names of the 6 degrees of freedom.
- η1: surge, translation along X axis
- η2: sway, translation about along Y axis
- η3: heave, translation along Z axis
- η4: roll, rotation about X axis
- η5: pitch, rotation about Y axis
- η6: yaw, rotation about Z axis
What is the main reason for using a ship-fixed coordinate system and not an earth-fixed coordinate system for the ship motion analysis?
The body xed coordinate system is better for ship motion analysis as the forces, moments, moments of inertia and products of inertia will not vary in time (which would be the case for the earth xed cooridnate system). On the downside the equations of motions gets more complicated for the body xed coordinate system
Describe the Strip-theory approach for solving the Seakeeping problem?
The ship can be represented by 2D strips for which the coeficients for added mass, damping and restoring force can be determined by
- A simple 2D potential own solution for each strip.
- Analytical solotion after coordinate transformation to circular 2d cylinder, (Lewis forms)
- Experiments for hull segment shaped 2D cylinder
A summation over strips will then give the properties for the hull.
The Strip-theory approach is based on a number of assumptions. Give 4 of them
- The ship is slender
- The hull is rigid
- Moderate speed, no planing
- The motions are small
- The ship hull sides are wall sided
- Deep water
- Waves are not disturbed by the hull
The ship motion problem is often split into a Seakeeping problem and a Manoeuvring problem. Give a motivation for this split based on the forces involved.
The separation into seakeeping is due to that this are moving out from the xy-plane
- η3, Heaving
- η4, Pitch
- η5, Roll
and manouvering problem moves only inside the xy-plane
- η1, Serch
- η2, Sway
- η6, Yaw
This is motivated by the small coupling between the degrees of freedom in the two problems
There is no copuling between manov and seakeep.
There are no restoring power in manov
Describe the physical effects behind the three forces that occur for forced heave in calm water.
Added mass (−a33η ̈3)
The added mass is in phase with the force necessary to accelerate the body and it depends on the frequency close to the water surface but far from it the added mass only depends on the shape of the body.
Radiation damping (−b33η ̇3)
The radiation damping is heave motion caused waves that are radioated out from the body. This is in phase with the velocity of the heave motion. The radiation damping coecient is zero for frequency of zero and innity and has its maximum somewhere inbetween.
Vertical restoring (−c33η3) The vertical restoring force is caused by the displacement of the body and is in phase with the vertical position.
Explain the “Small ship approximation
Small-body approximation
The body can be assumed small in comparison with the wavelength (B < λ/4)
Explain the “Small ship approximation
Wave attenuating eect, describes how the wave vanishes with depth (the decrease of dynamic pressure).
e^−kT describes how the exitation forces vanishes with the draught
What is a Response Amplitude Operator (RAO)?
A Response Amplitude Operator (RAO) is the ratio of a studied variable to the wave amplitude.
Describe the two free-surface boundary condition for free-surface gravity waves.
- The free surface kinematic boundary condition states that a particle on the surface will stay on the surface.
- The free surface dynamic boundary condition derives from the Bernoulli equation on the assumption that the pressure is constant on the free sur- face.
Write the expression for the wave form of a plane harmonic wave progressing in the x-direction. The wave amplitude is a.
The real progressive wave is given by
Re(ζ_c) = a cos(kx − ωt)
Draw a sketch of the fluid particle motion beneath a wave in deep water and in shallow water.
See gure 3.2 in the compendium.
The motion does not fully vanish in shallow water towards the bottom. The motion is not circular, which is the case in deep water, but elliptical with a longer horizontal length.
- The real valued pressure for deep water is
p = ρgaekz cos(kx − ωt) − ρgz - The real valued pressure for shallow water is
p = ρga cos(kx − ωt) − ρgz
Potential ow description of free-surface waves
Assumptions Potential ow assumes an inviscid, incompressible and irrota- tional ow. The boundary conditions are non-linear following the moving free surface and the simplest way to deal with this is to apply linear or small wave theory (Airy theory) which is based on the assumption that the wave amplitude, a, is small in comparison with the wavelength ,λ.
Show how to decompose the hydrodynamic problem for a floating body oscillating in an incident wave?
The problem can be decomposed into
- The reaction forces appearing when the body is forced to oscillate in calm water
- The wave excitation forces when the body is xed in regular waves
Tell in words what added mass is
Added mass is water surrounding the body that will be accelerated together with the body and is therefore in phase with the acceleration of the body.