1.1 Hull-borne mode
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Statutory Documents - IMO Publications and Documents - International Codes - HSC 2000 Code - International Code of Safety for High-Speed Craft, 2000 – Resolution MSC.97(73) - Annex 6 - Stability of hydrofoil craft - 1 Surface-piercing hydrofoils - 1.1 Hull-borne mode

1.1 Hull-borne mode

  1.1.1 The stability shall be sufficient to satisfy the provisions of 2.3, 2.4 and 2.6 of this Code.

  1.1.2 Heeling moment due to turning

The heeling moment developed during manoeuvring of the craft in the displacement mode may be derived from the following formula:

where:
M R = moment of heeling;
V o = speed of the craft in the turn (m/s);
Δ = displacement (t);
L = length of the craft on the waterline (m);
KG = height of the centre of gravity above keel (m).

This formula is applicable when the ratio of the radius of the turning circle to the length of the craft is 2 to 4.

  1.1.3 Relationship between the capsizing moment and heeling moment to satisfy the weather criterion

The stability of a hydrofoil boat in the displacement mode can be checked for compliance with the weather criterion K as follows:

where:
M c = minimum capsizing moment as determined when account is taken of rolling;
M v = dynamically applied heeling moment due to the wind pressure.

  1.1.4 Heeling moment due to wind pressure

The heeling moment MV shall be taken as constant during the whole range of heel angles and calculated by the following expression:

where:
P V = wind pressure = 750 (V W/ 26)2 (N/m2)
A V = windage area including the projections of the lateral surfaces of the hull, superstructure and various structures above the waterline (m2)
Z = windage area lever (m) = the vertical distance to the geometrical centre of the windage area from the waterline
V W = the wind speed corresponding to the worst intended conditions (m/s).

  1.1.5 Evaluation of the minimum capsizing moment Mc in the displacement mode

The minimum capsizing moment is determined from the static and dynamic stability curves taking rolling into account.

  • .1 When the static stability curve is used, Mc is determined by equating the areas under the curves of the capsizing and righting moments (or levers) taking rolling into account, as indicated by figure 1, where θ z is the amplitude of roll and MK is a line drawn parallel to the abscissa axis such that the shaded areas S1 and S2 are equal.

    M c = OM, if the scale of ordinates represents moments,
    M c = OM x displacement, if the scale of ordinates represents levers.
  • .2 When the dynamic stability curve is used, first an auxiliary point A shall be determined. For this purpose the amplitude of heeling is plotted to the right along the abscissa axis and a point A' is found (see figure 2 ). A line AA' is drawn parallel to the abscissa axis equal to the double amplitude of heeling (AA' = 2θ z) and the required auxiliary point A is found. A tangent AC to the dynamic stability curve is drawn. From the point A the line AB is drawn parallel to the abscissa axis and equal to 1 radian (57.3°). From the point B a perpendicular is drawn to intersect with the tangent in point E. The distance is equal to the capsizing moment if measured along the ordinate axis of the dynamic stability curve. If, however, the dynamic stability levers are plotted along this axis, is then the capsizing lever, and in this case the capsizing moment M c is determined by multiplication of ordinate (in metres) by the corresponding displacement in tonnes

    M c = 9.81 Δ (kNm)

  • .3 The amplitude of rolling θ z is determined by means of model and full-scale tests in irregular seas as a maximum amplitude of rolling of 50 oscillations of a craft travelling at 90° to the wave direction in sea state for the worst design condition. If such data are lacking the amplitude is assumed to be equal to 15°.

  • .4 The effectiveness of the stability curves shall be limited to the angle of flooding.

Figure 1 Static Stability Curve

Figure 2 Dynamic Stability Curve


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