N³ = -8(a + b), (29)

will give a possible state of motion of the axis of the body; and the

motion of the centre may then be inferred from (22).

50. The theory preceding is of practical application in the

investigation of the stability of the axial motion of a submarine boat,

of the elongated gas bag of an airship, or of a spinning rifled

projectile. In the steady motion under no force of such a body in a

medium, the centre of gravity describes a helix, while the axis

describes a cone round the direction of motion of the centre of gravity,

and the couple causing precession is due to the displacement of the

medium.

In the absence of a medium the inertia of the body to translation is the

same in all directions, and is measured by the weight W, and under no

force the C.G. proceeds in a straight line, and the axis of rotation

through the C.G. preserves its original direction, if a principal axis

of the body; otherwise the axis describes a cone, right circular if the

body has uniaxial symmetry, and a Poinsot cone in the general case.

But the presence of the medium makes the effective inertia depend on the

direction of motion with respect to the external shape of the body, and

on W´ the weight of fluid medium displaced.

Consider, for example, a submarine boat under water; the inertia is

different for axial and broadside motion, and may be represented by

c1 = W + W´[alpha], c2 = W + W´[beta], (1)

where [alpha], [beta] are numerical factors depending on the external

shape; and if the C.G. is moving with velocity V at an angle [phi]

with the axis, so that the axial and broadside component of velocity

is u = V cos [phi], v = V sin [phi], the total momentum F of the

medium, represented by the vector OF at an angle [theta] with the

axis, will have components, expressed in sec. lb.,

u V v V

F cos [theta] = c1 --- = (W + W´[alpha]) --- cos [phi], F sin [theta] = c2 --- = (W + W´[beta]) --- sin [phi]. (2)

g g g g

Suppose the body is kept from turning as it advances; after t seconds

the C.G. will have moved from O to O´, where OO´ = Vt; and at O´ the

momentum is the same in magnitude as before, but its vector is

displaced from OF to O´F´.

Encyclopaedia Britannica, 11th Edition, "Hydromechanics" to "Ichnography" Volume 14, Slice 2 · 第 72 / 120 题