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Practical Ship Hydrodynamics

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<strong>Ship</strong> seakeeping 139<br />

The wave impact caused by slamming can be roughly classified into four types<br />

(Fig. 4.18):<br />

(1) Bottom slamming (2) 'Bow-flare' slamming<br />

(3) Breaking wave impact<br />

Figure 4.18 Types of slamming impact of a ship<br />

Catamaran<br />

(4) Wetdeck slamming<br />

1. Bottom slamming occurs when emerged bottoms re-enter the water surface.<br />

2. Bow-flare slamming occurs for high relative speed of bow-flare to the water<br />

surface.<br />

3. Breaking wave impacts are generated by the superposition of incident wave<br />

and bow wave hitting the bow of a blunt ship even for small ship motion.<br />

4. Wet-deck slamming occurs when the relative heaving amplitude is larger<br />

than the height of a catamaran’s wet-deck.<br />

Both bottom and bow-flare slamming occur typically in head seas with large<br />

pitching and heaving motions. All four water impacts are 3-d phenomena,<br />

but have been treated as 2-d for simplicity. For example, types 1 and 2 were<br />

idealized as 2-d wedge entry to the calm-water surface. Type 3 was also studied<br />

as 2-d phenomenon similar to wave impact on breakwaters. We will therefore<br />

review 2-d theories first.<br />

ž Linear slamming theories based on expanding thin plate approximation<br />

Classical theories approximate the fluid as inviscid, irrotational, incompressible,<br />

free of surface tension. In addition, it is assumed that gravity effects<br />

are negligible. This allows a (predominantly) analytical treatment of the<br />

problem in the framework of potential theory.<br />

For bodies with small deadrise angle, the problem can be linearized. Von<br />

Karman (1929) was the first to study theoretically water impact (slamming).<br />

He idealized the impact as a 2-d wedge entry problem on the calm-water<br />

surface to estimate the water impact load on a seaplane during landing<br />

(Fig. 4.19). Mass, deadrise angle, and initial penetrating velocity of the<br />

wedge are denoted as m, ˇ and V0. Since the impact is so rapid, von Karman<br />

assumed very small water surface elevation during impact and negligible<br />

gravity effects. Then the added mass is approximately mv D ⊲ 1<br />

2⊳ c2 . is<br />

the water density and c the half width of the wet area implicitly computed<br />

from dc/dt D V cot ˇ. The momentum before the impact mV0 must be equal<br />

to the sum of the wedge momentum mV and added mass momentum mvV,<br />

yielding the impact load as:<br />

P D V2 0<br />

�<br />

/ tan ˇ<br />

1 C c2<br />

2m<br />

� 3 Ð c

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