28.02.2013 Views

Practical Ship Hydrodynamics

Practical Ship Hydrodynamics

Practical Ship Hydrodynamics

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

256 <strong>Practical</strong> <strong>Ship</strong> <strong>Hydrodynamics</strong><br />

and the diffraction problem are solved separately. The total solution is a linear<br />

combination of the solutions for each independent problem.<br />

The harmonic potential ⊲1⊳ is divided into the potential of the incident wave<br />

w , the diffraction potential d , and 6 radiation potentials:<br />

⊲1⊳ D d C w C<br />

6�<br />

iD1<br />

i ui<br />

It is convenient to decompose w and d into symmetrical and antisymmetrical<br />

parts to take advantage of the (usual) geometrical symmetry:<br />

Thus:<br />

w ⊲x, y, z⊳ D<br />

w w<br />

⊲x, y, z⊳ C ⊲x,<br />

� ��<br />

2<br />

w<br />

y, z⊳ ⊲x, y, z⊳<br />

C<br />

� �<br />

w<br />

⊲x,<br />

��<br />

2<br />

y, z⊳<br />

�<br />

w,s<br />

w,a<br />

d D d,s C d,a D 7 C 8<br />

⊲1⊳ D w,s C w,a C<br />

6�<br />

iD1<br />

i ui C 7 C 8<br />

The conditions satisfied by the steady flow potential<br />

from section 7.3 without further comment.<br />

⊲0⊳ are repeated here<br />

The particle acceleration in the steady flow is: Ea ⊲0⊳ D ⊲r ⊲0⊳r⊳r ⊲0⊳<br />

We define an acceleration vector Ea g Ea g DEa ⊲0⊳ Cf0, 0,ggT For convenience I introduce an abbreviation: B D 1<br />

a g<br />

3<br />

∂<br />

∂z ⊲r ⊲0⊳ Ea g ⊳<br />

In the whole fluid domain: 1 ⊲0⊳ D 0<br />

At the steady free surface: r ⊲0⊳ Ea g D 0<br />

1<br />

2 ⊲r ⊲0⊳ ⊳ 2 C g ⊲0⊳ D 1<br />

2 V2<br />

On the body surface: En⊲Ex⊳r ⊲0⊳ ⊲Ex⊳ D 0<br />

Also suitable radiation and decay conditions are observed.<br />

The linearized potential of the incident wave on water of infinite depth is<br />

expressed in the inertial system:<br />

w D Re<br />

� igh<br />

ω e ik⊲x cos y sin ⊳ kz e iωet<br />

�<br />

D Re⊲ O w e iωet<br />

⊳<br />

ω D p gk is the frequency of the incident wave, ωe Djω kV cos j the<br />

frequency of encounter. k is the wave number. The derivation of the expression<br />

for w assumes a linearization around z D 0. The same formula will be<br />

used now in the seakeeping computations, although the average boundary is<br />

at the steady wave elevation, i.e. different near the ship. This may be an<br />

inconsistency, but the diffraction potential should compensate this ‘error’.<br />

We write the complex amplitude of the incident wave as:<br />

O w D igh<br />

ω eExEd with Ed Df ik cos , ik sin , kzg T

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!