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Basics of Fluid Mechanics, 2014a

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4.6. BUOYANCY AND STABILITY 125<br />

on the ratio <strong>of</strong> t/R which similar analysis to the above. For a given ratio <strong>of</strong> t/R, the<br />

weight displaced by the sphere has to be same as the sphere weight. The volume <strong>of</strong> a<br />

sphere cap (segment) is given by<br />

V cap = πh2 (3R − h)<br />

3<br />

Where h is the sphere height above the water. The volume in the water is<br />

V water = 4 πR3<br />

3<br />

− πh2 (3R − h)<br />

3<br />

= 4 π ( R 3 − 3 Rh 2 + h 3)<br />

3<br />

(4.XXV.d)<br />

(4.XXV.e)<br />

When V water denotes the volume <strong>of</strong> the sphere in the water. Thus the Archimedes law<br />

is<br />

ρ w 4 π ( R 3 − 3 Rh 2 + h 3)<br />

= ρ s 4 π ( 3 tR 2 − 3 t 2 R + t 3)<br />

(4.XXV.f)<br />

3<br />

3<br />

or<br />

(<br />

R 3 − 3 Rh 2 + h 3) = ρ w<br />

(<br />

3 tR 2 − 3 t 2 R + t 3)<br />

(4.XXV.g)<br />

ρ s<br />

The solution <strong>of</strong> (4.XXV.g) is<br />

(√<br />

−fR (4 R3 − fR)<br />

h =<br />

−<br />

2<br />

) 1<br />

fR− 2 R3 3<br />

2<br />

+<br />

(√ ) 1<br />

−fR (4 R3 − fR) fR− 2 R3 3<br />

−<br />

2<br />

2<br />

(4.XXV.h)<br />

Where −fR = R 3 − ρ w<br />

(3 tR 2 − 3 t 2 R + t 3 ) There are two more solutions which<br />

ρ s<br />

contains the imaginary component. These solutions are rejected.<br />

End Solution<br />

Example 4.26:<br />

One <strong>of</strong> the common questions in buoyancy is the weight with variable cross section and<br />

fix load. For example, a wood wedge <strong>of</strong> wood with a fix weight/load. The general<br />

question is at what the depth <strong>of</strong> the object (i.e. wedge) will be located. For simplicity,<br />

assume that the body is <strong>of</strong> a solid material.<br />

Solution<br />

It is assumed that the volume can be written as a function <strong>of</strong> the depth. As it was<br />

shown in the previous example, the relationship between the depth and the displaced<br />

liquid volume <strong>of</strong> the sphere. Here it is assumed that this relationship can be written as<br />

R 2<br />

V w = f(d, other geometrical parameters)<br />

(4.XXVI.a)

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