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By Mazlan Muslim, MEng, 
UniKL MIMET
 In general, a rigid body is considered to be in a state 
of static equilibrium when the resultants of all forces 
and moments acting on the body are zero. In dealing 
with static floating body stability, we are interested in 
that state of equilibrium associated with the floating 
body upright and at rest in a still liquid. In this ease, 
the resultant of all gravity forces (weights) acting 
downward and the resultant of the buoyancy forces 
acting upward on the body are of equal magnitude 
and are applied in the same vertical line. 
 Stable Equilibrium 
 If a floating body, initially at equilibrium, is disturbed 
by an external moment, there will be a change in its 
angular attitude. If upon removal of the external 
moment, the body tends to return to its original 
position, it is said to have been in stable equilibrium 
and to have positive stability.
 Neutral Equilibrium 
 If, on the other hand, a floating body that assumes a 
displaced inclination because of an external moment 
remains in that displaced position when the external 
moment is removed, the body is said to have been in 
neutral equilibrium and has neutral stability. A floating 
cylindrical homogeneous log would be in neutral 
equilibrium in heel. 
 Unstable Equilibrium 
 If, for a floating body displaced from its original angular 
attitude, the displacement continues to increase in the 
same direction after the moment is removed, it is said to 
have been in unstable equilibrium and was initially 
unstable. Note that there may be a situation in which the 
body is stable with respect to "small" displacements and 
unstable with respect to larger displacements from the 
equilibrium position. This is a very common situation for a 
ship, and we will consider cases of stability at small angles 
of heel (initial stability) and at large angles separately.
 This chapter deals with the forces and moments acting on a ship 
afloat in calm water. The forces consist primarily of gravity forces 
(weights) and buoyancy forces. Therefore, equations are usually 
developed using displacement, Δ, weight, W, and component 
weights, w. In the "English" system, displacement, weights, and 
buoyant forces are thus expressed in the familiar units of long 
tons (or lb.). When using the International System of Units (SI), the 
displacement or buoyancy force is still expressed as Δ=ρg∇, but 
this is units of newtons which, for most ships, will be an 
inconveniently large number. In order to deal with numbers of 
more reasonable size, we may express displacement in 
kilonewtons or meganewtons. 
 A non-SI force unit, the "metric ton force," or "tonnef," is defined 
as the force exerted by gravity on a mass of 1000 KG. If the 
weight or displacement is expressed in tonnef, its numerical value 
is approximately the same as the value in long tons, the unit 
traditionally used for expressing weights and displacement in ship 
work. Since the shipping and shipbuilding industries have a long 
history of using long tons and are familiar with the numerical 
values of weights and forces in these units, the tonnef (often 
written as just tonne) has been and is still commonly used for 
expressing weight and buoyancy. With this convention, righting 
and heeling moments are then expressed in units of metric ton-meters, 
t-m.
 The total weight, or displacement, of a ship can be 
determined from the draft marks and curves of 
form, as discussed in Geometry of Ships. The 
position of the center of gravity (CG) may be 
either calculated or determined experimentally. 
Both methods are used when dealing with ships. 
The weight and CG of a ship that has not yet been 
launched can be established only by a weight 
estimate, which is a summation of the estimated 
weights and moments of all the various items that 
make up the ship. In principle, all of the 
component parts that make up the ship could be 
weighed and recorded during the construction 
process to arrive at a finished weight and CG, but 
this is seldom done except for a few special craft 
in which the weight and CG are extremely critical. 
 After the ship is afloat, the weight and CG can be 
accurately established by an inclining experiment.
 To calculate the position of the CG of any object, it is 
assumed to be divided into a number of individual 
components or particles, the weight and CG of each being 
known. The moment of each particle is calculated by 
multiplying its weight by its distance from a reference 
plane, the weights and moments of all the particles added, 
and the total moment divided by the total weight of all 
particles, W The result is the distance of the CG from the 
reference plane. 
 The location of the CG is completely determined when its 
distance from each of three planes has been established. In 
ship calculations, the three reference planes generally used 
are a horizontal plane through the baseline for the vertical 
location of the center of gravity (VCG), a vertical transverse 
plane either through amidships or through the forward 
perpendicular for the longitudinal location (LCG), and a 
vertical plane through the centerline for the transverse 
position (TCG). (The TCG is usually very nearly in the 
centerline plane and is often assumed to be in that plane.)
 Displacement and Center of Buoyancy 
 It has been shown that the force of buoyancy is equal 
to the weight of the displaced liquid and that the 
resultant of this force acts vertically upward through a 
point called the center of buoyancy, which is the CG of 
the displaced liquid (centroid of the immersed 
volume). 
 Application of these principles to a ship, submarine, or 
other floating structure makes it possible to evaluate 
the effect of the hydrostatic pressure acting on the 
hull and appendages by determining the volume of the 
ship below the waterline and the centroid of this 
volume. The submerged volume, when multiplied by 
the specific weight of the water in which the ship 
floats is the weight of displaced liquid and is called the 
displacement, denoted by the Greek symbol Δ.
 The attitude of a floating object is determined by 
the interaction of the forces of weight and 
buoyancy. If no other forces are acting, it will 
settle to such a waterline that the force of 
buoyancy equals the weight, and it will rotate 
until two conditions are satisfied: 
 The centers of buoyancy B and gravity G are in 
the same vertical line, as in Fig. 1(a). 
 
Any slight clockwise rotation from this position, 
as from WL to W1L1 in Fig. 1(b), will cause the 
center of buoyancy to move to the right, and the 
equal forces of weight and buoyancy to generate 
a couple tending to move the object back to float 
on WL (this is the condition of stable 
equilibrium).
 For every object, with one exception as noted later, at 
least one position must exist for which these 
conditions are satisfied, since otherwise the object 
would continue to rotate indefinitely. There may be 
several such positions of equilibrium. The CG may be 
either above or below the center of buoyancy, but for 
stable equilibrium, the shift of the center of buoyancy 
that results from a small rotation must be such that a 
positive couple (in a direction opposing the rotation) 
results. 
 An exception to the second condition exists when the 
object is a body of revolution with its CG exactly on 
the axis of revolution, as illustrated in Fig. 2. When 
such an object is rotated to any angle, no moment is 
produced, since the center of buoyancy is always 
directly below the CG. It will remain at any angle at 
which it is placed (this is a condition of neutral 
equilibrium).
 A submerged object whose weight equals its 
buoyancy that is not in contact with the seafloor 
or other objects can come to rest in only one 
position. It will rotate until the CG is directly 
below the center of buoyancy. If its CG coincides 
with its center of buoyancy, as in the case of a 
homogeneous object, it would remain in any 
position in which it is placed since in this case it 
is in neutral equilibrium. 
 The difference in the action of floating and 
submerged objects is explained by the fact that 
the center of buoyancy of the submerged object 
is fixed relative to the body, while the center of 
buoyancy of a floating object will generally shift 
when the object is rotated as a result of the 
change in shape of the immersed part of the 
body.
 As an example, consider a watertight body 
having a rectangular section with dimensions 
and CG as illustrated in Fig. 3. Assume that it 
will float with half its volume submerged, as in 
Fig. 4. It can come to rest in either of two 
positions, (a) or (c), 180 degrees apart. In 
either of these positions, the centers of 
buoyancy and gravity are in the same vertical 
line. Also, as the body is inclined from (a) to 
(b) or from (c) to (d), a moment is developed 
which tends to rotate the body back to its 
original position, and the same situation 
would exist if it were inclined in the opposite 
direction.
 If the 20-cm dimension were reduced with the CG still 
on the centerline and 2.5 cm below the top, a situation 
would be reached where the center of buoyancy would 
no longer move far enough to be to the right of the CG 
as the body is inclined from (a) to (b). Then the body 
could come to rest only in position (c). 
 As an illustration of a body in the submerged 
condition, assume that the weight of the body shown 
in Fig. 3 is increased so that the body is submerged, as 
in Fig. 5. In positions (a) and (c), the centers of 
buoyancy and gravity are in the same vertical line. An 
inclination from (a) in either direction would produce a 
moment tending to rotate the body away from position 
(a), as illustrated in Fig. 5(b). An inclination from (c) 
would produce a moment tending to restore the body 
to position (c). Therefore, the body can come to rest 
only in position (c).
 A ship or submarine is designed to float in the 
upright position. This fact permits the 
definition of two classes of hydrostatic 
moments, illustrated in Fig. 6, as follows: 
 Righting moments: A righting moment exists 
at any angle of inclination where the forces of 
weight and buoyancy act to move the ship 
toward the upright position. 
 Overturning moments: An overturning 
moment exists at any angle of inclination 
where the forces of weight and buoyancy act 
to move the ship away from the upright 
position.
 The center of buoyancy of a ship or a surfaced submarine moves 
with respect to the ship, as the ship is inclined, in a manner that 
depends upon the shape of the ship in the vicinity of the 
waterline. The center of buoyancy of a submerged submarine, on 
the contrary, does not move with respect to the ship, regardless 
of the inclination or the shape of the hull, since it is stationary at 
the CG of the entire submerged volume. This constitutes an 
important difference between floating and submerged ships. The 
moment acting on a surface ship can change from a righting 
moment to an overturning moment, or vice versa, as the ship is 
inclined, but this cannot occur on a submerged submarine unless 
there is a shift of the ship's CG. 
 It can be seen from Fig. 6 that lowering of the CG along the ship's 
centerline increases stability. When a righting moment exists, 
lowering the CG along the centerline increases the separation of 
the forces of weight and buoyancy and increases the righting 
moment. When an overturning moment exists, sufficient lowering 
of the CG along the centerline would change the moment to a 
righting moment, changing the stability of the initial upright 
equilibrium from unstable to stable.
 In problems involving longitudinal stability of 
undamaged surface ships, we are concerned primarily 
with determining the ship's draft and trim under the 
influence of various upsetting moments, rather than 
evaluating the possibility of the ship capsizing in the 
longitudinal direction. If the longitudinal centers of 
gravity and buoyancy are not in the same vertical line, 
the ship will change trim as discussed in Section 8 and 
will come to rest as illustrated in Fig. 7, with the 
centers of gravity and buoyancy in the same vertical 
line. 
 A small longitudinal inclination will cause the center of 
buoyancy to move so far in a fore and aft direction 
that the moment of weight and buoyancy would be 
many times greater than that produced by the same 
inclination in the transverse direction. The longitudinal 
shift in buoyancy creates such a large longitudinal 
righting moment that longitudinal stability is usually 
very great compared to transverse stability.
 Thus, if the ship's CG were to rise along the 
centerline, the ship would capsize transversely long 
before there would be any danger of capsizing 
longitudinally. However, a surface ship could, 
theoretically, be made to founder by a downward 
external force applied toward one end, at a point near 
the centerline, and at a height near or below the 
center of buoyancy without capsizing. It is unlikely, 
however, that an intact ship would encounter a force 
of the required magnitude. 
 Surface ships can, and do, founder after extensive 
flooding as a result of damage at one end. The loss of 
buoyancy at the damaged end causes the center of 
buoyancy to move so far toward the opposite end of 
the ship that subsequent submergence of the 
damaged end is not adequate to move the center of 
buoyancy back to a position in line with the CG, and 
the ship founders, or capsizes longitudinally.
 In the case of a submerged submarine, the center of 
buoyancy does not move as the submarine is inclined 
in a fore-and-aft direction. Therefore, capsizing of an 
intact submerged submarine in the longitudinal 
direction is possible and would require very nearly 
the same moment as would be required to capsize it 
transversely. If the CG of a submerged submarine 
were to rise to a position above the center of 
buoyancy, the direction, longitudinal or transverse, in 
which it would capsize would depend upon the 
movement of liquids or loose objects within the ship. 
The foregoing discussion of submerged submarines 
does not take into account the stabilizing effect of 
the bow and stern planes which have an important 
effect on longitudinal stability while the ship is 
underway with the planes producing hydrodynamic 
lift.
 The magnitude of the upsetting forces, or 
heeling moments, that may act on a ship 
determines the magnitude of moment that must 
be generated by the forces of weight and 
buoyancy in order to prevent capsizing or 
excessive heel. 
 External upsetting forces affecting transverse 
stability may be caused by: 
 Beam winds, with or without rolling. 
 Lifting of heavy weights over the side. 
 High-speed turns. 
 Grounding. 
 Strain on mooring lines. 
 Towline pull of tugs.
 Internal upsetting forces include: 
 Shifting of on-board weights athwartship. 
 Entrapped water on deck. 
 The discussion below is general in nature and illustrates 
the stability principles involved when a ship is subjected to 
upsetting forces. 
 When a ship is exposed to a beam wind, the wind pressure 
acts on the portion of the ship above the water-line, and 
the resistance of the water to the ship's lateral motion 
exerts a force on the opposite side below the waterline. 
The situation is illustrated in Fig. 8. Equilibrium with 
respect to angle of heel will be reached when: 
 The ship is moving to leeward with a speed such that the 
water resistance equals the wind pressure, and 
 The ship has heeled to an angle such that the moment 
produced by the forces of weight and buoyancy equals the 
moment developed by the wind pressure and the water 
pressure.
 As the ship heels from the vertical, the wind pressure, water 
pressure, and their vertical separation remain substantially 
constant. The ship's weight is constant and acts at a fixed point. 
The force of buoyancy also is constant, but the point at which it 
acts varies with the angle of heel. Equilibrium will be reached 
when sufficient horizontal separation of the centers of gravity and 
buoyancy has been produced to cause a balance between heeling 
and righting moments. 
 When a weight is lifted over the side, as illustrated in Fig. 9, the 
force exerted by the weight acts through the outboard end of the 
boom, regardless of the angle of heel or the height to which the 
load has been lifted. Therefore, the weight of the sidelift may be 
considered to be added to the ship at the end of the boom. If the 
ship's CG is initially on the ship's centerline, as at G in Fig. 9, the 
CG of the combined weight of the ship and the sidelift will be 
located along the line GA and will move to a final position, G1 
when the load has been lifted clear of the pier. Point G1 will be off 
the ship's centerline and somewhat higher than G. The ship will 
heel until the center of buoyancy has moved off the ship's 
centerline to a position directly below point G1.
 Movement of weights already aboard the 
ship, such as passengers, liquids, or cargo, 
will cause the ship's CG to move. If a weight 
is moved from A to B in Fig. 10, the ship's CG 
will move from G to G1 in a direction parallel 
to the direction of movement of the shifted 
weight. The ship will heel until the center of 
buoyancy is directly below point G1.
 When a ship is executing a turn, the dynamic 
loads from the control surfaces and external 
pressure accelerate the ship towards the center of 
the turn. In a static evaluation, the resulting 
inertial force can be treated as a centrifugal force 
acting horizontally through the ship's CG. This 
force is balanced by a horizontal water pressure 
on the side of the ship, as illustrated in Fig. 11(a). 
 Except for the point of application of the heeling 
force, the situation is similar to that in which the 
ship is acted upon by a beam wind, and the ship 
will heel until the moment of the ship's weight and 
buoyancy equals that of the centrifugal force and 
water pressure.
 If a ship runs aground in such a manner that contact with 
the seafloor occurs over a small area (point contact), the 
sea bottom offers little restraint to heeling, as illustrated in 
Fig. 11(b), and the reaction between ship and seafloor of 
the bottom may produce a heeling moment. As the ship 
grounds, part of the energy due to its forward motion may 
be absorbed in lifting the ship, in which case a reaction, R, 
between the bottom and the ship would develop. 
 This reaction may be increased later as the tide ebbs. 
Under these conditions, the force of buoyancy would be 
less than the weight of the ship because the ship would be 
supported by the combination of buoyancy and the 
reaction at the point of contact. The ship would heel until 
the moment of buoyancy about the point of contact 
became equal to the moment of the ship's weight about the 
same point, when (W−R) × a equals W × b.
 There are numerous other situations in which external 
forces can produce heel. A moored ship may be 
heeled by the combination of strain on the mooring 
lines and pressure produced by wind or current. 
Towline strain may produce heeling moments in either 
the towed or towing ship. In each ease, equilibrium 
would be reached when the center of buoyancy has 
moved to a point where heeling and righting moments 
are balanced. 
 In any of the foregoing examples, it is quite possible 
that equilibrium would not be reached before the ship 
capsized. It is also possible that equilibrium would 
not be reached until the angle of heel became so large 
that water would be shipped through topside 
openings, and that the weight of this water, running 
to the low side of the ship, would contribute to 
capsizing which otherwise would not have occurred.
 Upsetting forces act to incline a ship in the longitudinal as well as 
the transverse direction. Since a surface ship is much stiffer, 
however, in the longitudinal direction, many forces, such as wind 
pressure or towline strain, would not have any significant effect in 
inclining the ship longitudinally. Shifting of weights aboard in a 
longitudinal direction can cause large changes in the attitude of 
the ship because the weights can be moved much farther than in 
the transverse direction. When very heavy lifts are to be 
attempted, as in salvage work, they are usually made over the 
bow or stern rather than over the side, and large longitudinal 
inclinations may be involved in these operations. 
 Stranding at the bow or stern can produce substantial changes in 
trim. In each ease, the principles are the same as previously 
discussed for transverse inclinations. When a weight is shifted 
longitudinally or lifted over the bow or stern, the CG of the ship 
will move, and the ship will trim until the center of buoyancy is 
directly below the new position of the CG. If a ship is grounded at 
the bow or stern, it will assume an attitude such that the 
moments of weight and buoyancy about the point of contact are 
equal.
 In the case of a submerged submarine, the center 
of buoyancy is fixed, and a given upsetting 
moment produces very nearly the same 
inclination in the longitudinal direction as it does 
in the transverse direction (Fig. 12). The only 
difference, which is trivial, is because of the effect 
of liquids aboard which may move to a different 
extent in the two directions. 
 A submerged submarine, however, is 
comparatively free from large upsetting forces. 
Shifting of the CG as the result of weight changes 
is carefully avoided. For example, when a torpedo 
is fired, its weight is immediately replaced by an 
equal weight of water at the same location.
Wk 1 intact stability elementary principles

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Wk 1 intact stability elementary principles

  • 1. By Mazlan Muslim, MEng, UniKL MIMET
  • 2.  In general, a rigid body is considered to be in a state of static equilibrium when the resultants of all forces and moments acting on the body are zero. In dealing with static floating body stability, we are interested in that state of equilibrium associated with the floating body upright and at rest in a still liquid. In this ease, the resultant of all gravity forces (weights) acting downward and the resultant of the buoyancy forces acting upward on the body are of equal magnitude and are applied in the same vertical line.  Stable Equilibrium  If a floating body, initially at equilibrium, is disturbed by an external moment, there will be a change in its angular attitude. If upon removal of the external moment, the body tends to return to its original position, it is said to have been in stable equilibrium and to have positive stability.
  • 3.  Neutral Equilibrium  If, on the other hand, a floating body that assumes a displaced inclination because of an external moment remains in that displaced position when the external moment is removed, the body is said to have been in neutral equilibrium and has neutral stability. A floating cylindrical homogeneous log would be in neutral equilibrium in heel.  Unstable Equilibrium  If, for a floating body displaced from its original angular attitude, the displacement continues to increase in the same direction after the moment is removed, it is said to have been in unstable equilibrium and was initially unstable. Note that there may be a situation in which the body is stable with respect to "small" displacements and unstable with respect to larger displacements from the equilibrium position. This is a very common situation for a ship, and we will consider cases of stability at small angles of heel (initial stability) and at large angles separately.
  • 4.  This chapter deals with the forces and moments acting on a ship afloat in calm water. The forces consist primarily of gravity forces (weights) and buoyancy forces. Therefore, equations are usually developed using displacement, Δ, weight, W, and component weights, w. In the "English" system, displacement, weights, and buoyant forces are thus expressed in the familiar units of long tons (or lb.). When using the International System of Units (SI), the displacement or buoyancy force is still expressed as Δ=ρg∇, but this is units of newtons which, for most ships, will be an inconveniently large number. In order to deal with numbers of more reasonable size, we may express displacement in kilonewtons or meganewtons.  A non-SI force unit, the "metric ton force," or "tonnef," is defined as the force exerted by gravity on a mass of 1000 KG. If the weight or displacement is expressed in tonnef, its numerical value is approximately the same as the value in long tons, the unit traditionally used for expressing weights and displacement in ship work. Since the shipping and shipbuilding industries have a long history of using long tons and are familiar with the numerical values of weights and forces in these units, the tonnef (often written as just tonne) has been and is still commonly used for expressing weight and buoyancy. With this convention, righting and heeling moments are then expressed in units of metric ton-meters, t-m.
  • 5.  The total weight, or displacement, of a ship can be determined from the draft marks and curves of form, as discussed in Geometry of Ships. The position of the center of gravity (CG) may be either calculated or determined experimentally. Both methods are used when dealing with ships. The weight and CG of a ship that has not yet been launched can be established only by a weight estimate, which is a summation of the estimated weights and moments of all the various items that make up the ship. In principle, all of the component parts that make up the ship could be weighed and recorded during the construction process to arrive at a finished weight and CG, but this is seldom done except for a few special craft in which the weight and CG are extremely critical.  After the ship is afloat, the weight and CG can be accurately established by an inclining experiment.
  • 6.  To calculate the position of the CG of any object, it is assumed to be divided into a number of individual components or particles, the weight and CG of each being known. The moment of each particle is calculated by multiplying its weight by its distance from a reference plane, the weights and moments of all the particles added, and the total moment divided by the total weight of all particles, W The result is the distance of the CG from the reference plane.  The location of the CG is completely determined when its distance from each of three planes has been established. In ship calculations, the three reference planes generally used are a horizontal plane through the baseline for the vertical location of the center of gravity (VCG), a vertical transverse plane either through amidships or through the forward perpendicular for the longitudinal location (LCG), and a vertical plane through the centerline for the transverse position (TCG). (The TCG is usually very nearly in the centerline plane and is often assumed to be in that plane.)
  • 7.  Displacement and Center of Buoyancy  It has been shown that the force of buoyancy is equal to the weight of the displaced liquid and that the resultant of this force acts vertically upward through a point called the center of buoyancy, which is the CG of the displaced liquid (centroid of the immersed volume).  Application of these principles to a ship, submarine, or other floating structure makes it possible to evaluate the effect of the hydrostatic pressure acting on the hull and appendages by determining the volume of the ship below the waterline and the centroid of this volume. The submerged volume, when multiplied by the specific weight of the water in which the ship floats is the weight of displaced liquid and is called the displacement, denoted by the Greek symbol Δ.
  • 8.  The attitude of a floating object is determined by the interaction of the forces of weight and buoyancy. If no other forces are acting, it will settle to such a waterline that the force of buoyancy equals the weight, and it will rotate until two conditions are satisfied:  The centers of buoyancy B and gravity G are in the same vertical line, as in Fig. 1(a).  Any slight clockwise rotation from this position, as from WL to W1L1 in Fig. 1(b), will cause the center of buoyancy to move to the right, and the equal forces of weight and buoyancy to generate a couple tending to move the object back to float on WL (this is the condition of stable equilibrium).
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  • 10.  For every object, with one exception as noted later, at least one position must exist for which these conditions are satisfied, since otherwise the object would continue to rotate indefinitely. There may be several such positions of equilibrium. The CG may be either above or below the center of buoyancy, but for stable equilibrium, the shift of the center of buoyancy that results from a small rotation must be such that a positive couple (in a direction opposing the rotation) results.  An exception to the second condition exists when the object is a body of revolution with its CG exactly on the axis of revolution, as illustrated in Fig. 2. When such an object is rotated to any angle, no moment is produced, since the center of buoyancy is always directly below the CG. It will remain at any angle at which it is placed (this is a condition of neutral equilibrium).
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  • 12.  A submerged object whose weight equals its buoyancy that is not in contact with the seafloor or other objects can come to rest in only one position. It will rotate until the CG is directly below the center of buoyancy. If its CG coincides with its center of buoyancy, as in the case of a homogeneous object, it would remain in any position in which it is placed since in this case it is in neutral equilibrium.  The difference in the action of floating and submerged objects is explained by the fact that the center of buoyancy of the submerged object is fixed relative to the body, while the center of buoyancy of a floating object will generally shift when the object is rotated as a result of the change in shape of the immersed part of the body.
  • 13.  As an example, consider a watertight body having a rectangular section with dimensions and CG as illustrated in Fig. 3. Assume that it will float with half its volume submerged, as in Fig. 4. It can come to rest in either of two positions, (a) or (c), 180 degrees apart. In either of these positions, the centers of buoyancy and gravity are in the same vertical line. Also, as the body is inclined from (a) to (b) or from (c) to (d), a moment is developed which tends to rotate the body back to its original position, and the same situation would exist if it were inclined in the opposite direction.
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  • 16.  If the 20-cm dimension were reduced with the CG still on the centerline and 2.5 cm below the top, a situation would be reached where the center of buoyancy would no longer move far enough to be to the right of the CG as the body is inclined from (a) to (b). Then the body could come to rest only in position (c).  As an illustration of a body in the submerged condition, assume that the weight of the body shown in Fig. 3 is increased so that the body is submerged, as in Fig. 5. In positions (a) and (c), the centers of buoyancy and gravity are in the same vertical line. An inclination from (a) in either direction would produce a moment tending to rotate the body away from position (a), as illustrated in Fig. 5(b). An inclination from (c) would produce a moment tending to restore the body to position (c). Therefore, the body can come to rest only in position (c).
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  • 18.  A ship or submarine is designed to float in the upright position. This fact permits the definition of two classes of hydrostatic moments, illustrated in Fig. 6, as follows:  Righting moments: A righting moment exists at any angle of inclination where the forces of weight and buoyancy act to move the ship toward the upright position.  Overturning moments: An overturning moment exists at any angle of inclination where the forces of weight and buoyancy act to move the ship away from the upright position.
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  • 20.  The center of buoyancy of a ship or a surfaced submarine moves with respect to the ship, as the ship is inclined, in a manner that depends upon the shape of the ship in the vicinity of the waterline. The center of buoyancy of a submerged submarine, on the contrary, does not move with respect to the ship, regardless of the inclination or the shape of the hull, since it is stationary at the CG of the entire submerged volume. This constitutes an important difference between floating and submerged ships. The moment acting on a surface ship can change from a righting moment to an overturning moment, or vice versa, as the ship is inclined, but this cannot occur on a submerged submarine unless there is a shift of the ship's CG.  It can be seen from Fig. 6 that lowering of the CG along the ship's centerline increases stability. When a righting moment exists, lowering the CG along the centerline increases the separation of the forces of weight and buoyancy and increases the righting moment. When an overturning moment exists, sufficient lowering of the CG along the centerline would change the moment to a righting moment, changing the stability of the initial upright equilibrium from unstable to stable.
  • 21.  In problems involving longitudinal stability of undamaged surface ships, we are concerned primarily with determining the ship's draft and trim under the influence of various upsetting moments, rather than evaluating the possibility of the ship capsizing in the longitudinal direction. If the longitudinal centers of gravity and buoyancy are not in the same vertical line, the ship will change trim as discussed in Section 8 and will come to rest as illustrated in Fig. 7, with the centers of gravity and buoyancy in the same vertical line.  A small longitudinal inclination will cause the center of buoyancy to move so far in a fore and aft direction that the moment of weight and buoyancy would be many times greater than that produced by the same inclination in the transverse direction. The longitudinal shift in buoyancy creates such a large longitudinal righting moment that longitudinal stability is usually very great compared to transverse stability.
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  • 23.  Thus, if the ship's CG were to rise along the centerline, the ship would capsize transversely long before there would be any danger of capsizing longitudinally. However, a surface ship could, theoretically, be made to founder by a downward external force applied toward one end, at a point near the centerline, and at a height near or below the center of buoyancy without capsizing. It is unlikely, however, that an intact ship would encounter a force of the required magnitude.  Surface ships can, and do, founder after extensive flooding as a result of damage at one end. The loss of buoyancy at the damaged end causes the center of buoyancy to move so far toward the opposite end of the ship that subsequent submergence of the damaged end is not adequate to move the center of buoyancy back to a position in line with the CG, and the ship founders, or capsizes longitudinally.
  • 24.  In the case of a submerged submarine, the center of buoyancy does not move as the submarine is inclined in a fore-and-aft direction. Therefore, capsizing of an intact submerged submarine in the longitudinal direction is possible and would require very nearly the same moment as would be required to capsize it transversely. If the CG of a submerged submarine were to rise to a position above the center of buoyancy, the direction, longitudinal or transverse, in which it would capsize would depend upon the movement of liquids or loose objects within the ship. The foregoing discussion of submerged submarines does not take into account the stabilizing effect of the bow and stern planes which have an important effect on longitudinal stability while the ship is underway with the planes producing hydrodynamic lift.
  • 25.  The magnitude of the upsetting forces, or heeling moments, that may act on a ship determines the magnitude of moment that must be generated by the forces of weight and buoyancy in order to prevent capsizing or excessive heel.  External upsetting forces affecting transverse stability may be caused by:  Beam winds, with or without rolling.  Lifting of heavy weights over the side.  High-speed turns.  Grounding.  Strain on mooring lines.  Towline pull of tugs.
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  • 27.  Internal upsetting forces include:  Shifting of on-board weights athwartship.  Entrapped water on deck.  The discussion below is general in nature and illustrates the stability principles involved when a ship is subjected to upsetting forces.  When a ship is exposed to a beam wind, the wind pressure acts on the portion of the ship above the water-line, and the resistance of the water to the ship's lateral motion exerts a force on the opposite side below the waterline. The situation is illustrated in Fig. 8. Equilibrium with respect to angle of heel will be reached when:  The ship is moving to leeward with a speed such that the water resistance equals the wind pressure, and  The ship has heeled to an angle such that the moment produced by the forces of weight and buoyancy equals the moment developed by the wind pressure and the water pressure.
  • 28.  As the ship heels from the vertical, the wind pressure, water pressure, and their vertical separation remain substantially constant. The ship's weight is constant and acts at a fixed point. The force of buoyancy also is constant, but the point at which it acts varies with the angle of heel. Equilibrium will be reached when sufficient horizontal separation of the centers of gravity and buoyancy has been produced to cause a balance between heeling and righting moments.  When a weight is lifted over the side, as illustrated in Fig. 9, the force exerted by the weight acts through the outboard end of the boom, regardless of the angle of heel or the height to which the load has been lifted. Therefore, the weight of the sidelift may be considered to be added to the ship at the end of the boom. If the ship's CG is initially on the ship's centerline, as at G in Fig. 9, the CG of the combined weight of the ship and the sidelift will be located along the line GA and will move to a final position, G1 when the load has been lifted clear of the pier. Point G1 will be off the ship's centerline and somewhat higher than G. The ship will heel until the center of buoyancy has moved off the ship's centerline to a position directly below point G1.
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  • 30.  Movement of weights already aboard the ship, such as passengers, liquids, or cargo, will cause the ship's CG to move. If a weight is moved from A to B in Fig. 10, the ship's CG will move from G to G1 in a direction parallel to the direction of movement of the shifted weight. The ship will heel until the center of buoyancy is directly below point G1.
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  • 32.  When a ship is executing a turn, the dynamic loads from the control surfaces and external pressure accelerate the ship towards the center of the turn. In a static evaluation, the resulting inertial force can be treated as a centrifugal force acting horizontally through the ship's CG. This force is balanced by a horizontal water pressure on the side of the ship, as illustrated in Fig. 11(a).  Except for the point of application of the heeling force, the situation is similar to that in which the ship is acted upon by a beam wind, and the ship will heel until the moment of the ship's weight and buoyancy equals that of the centrifugal force and water pressure.
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  • 34.  If a ship runs aground in such a manner that contact with the seafloor occurs over a small area (point contact), the sea bottom offers little restraint to heeling, as illustrated in Fig. 11(b), and the reaction between ship and seafloor of the bottom may produce a heeling moment. As the ship grounds, part of the energy due to its forward motion may be absorbed in lifting the ship, in which case a reaction, R, between the bottom and the ship would develop.  This reaction may be increased later as the tide ebbs. Under these conditions, the force of buoyancy would be less than the weight of the ship because the ship would be supported by the combination of buoyancy and the reaction at the point of contact. The ship would heel until the moment of buoyancy about the point of contact became equal to the moment of the ship's weight about the same point, when (W−R) × a equals W × b.
  • 35.  There are numerous other situations in which external forces can produce heel. A moored ship may be heeled by the combination of strain on the mooring lines and pressure produced by wind or current. Towline strain may produce heeling moments in either the towed or towing ship. In each ease, equilibrium would be reached when the center of buoyancy has moved to a point where heeling and righting moments are balanced.  In any of the foregoing examples, it is quite possible that equilibrium would not be reached before the ship capsized. It is also possible that equilibrium would not be reached until the angle of heel became so large that water would be shipped through topside openings, and that the weight of this water, running to the low side of the ship, would contribute to capsizing which otherwise would not have occurred.
  • 36.  Upsetting forces act to incline a ship in the longitudinal as well as the transverse direction. Since a surface ship is much stiffer, however, in the longitudinal direction, many forces, such as wind pressure or towline strain, would not have any significant effect in inclining the ship longitudinally. Shifting of weights aboard in a longitudinal direction can cause large changes in the attitude of the ship because the weights can be moved much farther than in the transverse direction. When very heavy lifts are to be attempted, as in salvage work, they are usually made over the bow or stern rather than over the side, and large longitudinal inclinations may be involved in these operations.  Stranding at the bow or stern can produce substantial changes in trim. In each ease, the principles are the same as previously discussed for transverse inclinations. When a weight is shifted longitudinally or lifted over the bow or stern, the CG of the ship will move, and the ship will trim until the center of buoyancy is directly below the new position of the CG. If a ship is grounded at the bow or stern, it will assume an attitude such that the moments of weight and buoyancy about the point of contact are equal.
  • 37.  In the case of a submerged submarine, the center of buoyancy is fixed, and a given upsetting moment produces very nearly the same inclination in the longitudinal direction as it does in the transverse direction (Fig. 12). The only difference, which is trivial, is because of the effect of liquids aboard which may move to a different extent in the two directions.  A submerged submarine, however, is comparatively free from large upsetting forces. Shifting of the CG as the result of weight changes is carefully avoided. For example, when a torpedo is fired, its weight is immediately replaced by an equal weight of water at the same location.