For a real solution we must have k2 < 1, which is equivalent to 2BT > Γ2. If the initial conditions are such as to make 2BT < Γ2, we must interchange the forms of p and r in (7). In the present case the instantaneous axis returns to its initial position in the body whenever φ increases by 2π, i.e. whenever t increases by 4K/σ, when K is the “complete” elliptic integral of the first kind with respect to the modulus k.
The elliptic functions degenerate into simpler forms when k2 = 0 or k2 = 1. The former case arises when two of the principal moments are equal; this has been sufficiently dealt with in § 19. If k2 = 1, we must have 2BT = Γ2. We have seen that the alternative 2BT ≷ Γ2 determines whether the polhode cone surrounds the principal axis of least or greatest moment. The case of 2BT = Γ2, exactly, is therefore a critical case; it may be shown that the instantaneous axis either coincides permanently with the axis of mean moment or approaches it asymptotically.
When the origin of the moving axes is also in motion with a velocity whose components are u, v, w, the dynamical equations are
dξ | − r η + qζ = X, | dη | − pζ + r χ = Y, | dζ | − qχ + pη = Z, |
dt | dt | dt |
dλ | − r μ + qν − wη + vζ = L, | dμ | − pν + r λ- uζ + wξ = M, | dν | − qλ + pμ − vξ + uη = N. |
dt | dt | dt |
To prove these, we may take fixed axes O′x′, O′y′, O′z′ coincident
with the moving axes at time t, and compare the linear
and angular momenta ξ + δξ, η + δη, ζ + δζ, λ + δλ, μ + δμ, ν + δν
relative to the new position of the axes, Ox, Oy, Oz at time t + δt
with the original momenta ξ, η, ζ, λ, μ, ν relative to O′x′, O′y′,
O′z′ at time t. As in the case of (2), the equations are applicable
to any dynamical system whatever. If the moving origin coincide
always with the mass-centre, we have ξ, η, ζ = M0u, M0v,
M0w, where M0 is the total mass, and the equations simplify.
When, in any problem, the values of u, v, w, p, q, r have been determined as functions of t, it still remains to connect the moving axes with some fixed frame of reference. It will be sufficient to take the case of motion about a fixed point O; the angular co-ordinates θ, φ, ψ of Euler may then be used for the purpose. Referring to fig. 36 we see that the angular velocities p, q, r of the moving lines, OA, OB, OC about their instantaneous positions are
by § 7 (3), (4). If OA, OB, OC be principal axes of inertia of a solid, and if A, B, C denote the corresponding moments of inertia, the kinetic energy is given by
If A = B this reduces to
cf. § 20 (1).
§ 22. Equations of Motion in Generalized Co-ordinates.—Suppose we have a dynamical system composed of a finite number of material particles or rigid bodies, whether free or constrained in any way, which are subject to mutual forces and also to the action of any given extraneous forces. The configuration of such a system can be completely specified by means of a certain number (n) of independent quantities, called the generalized co-ordinates of the system. These co-ordinates may be chosen in an endless variety of ways, but their number is determinate, and expresses the number of degrees of freedom of the system. We denote these co-ordinates by q1, q2, . . . qn. It is implied in the above description of the system that the Cartesian co-ordinates x, y, z of any particle of the system are known functions of the q’s, varying in form (of course) from particle to particle. Hence the kinetic energy T is given by
2T | = Σ {m (ẋ2 + ẏ2 + ż2) } |
= a11q̇12 + a22q̇22 + . . . + 2a12q̇1q̇2 + . . ., |
where
arr = Σ [ m { ( | ∂x | 2 + | ∂y | 2 + | ∂z | 2 } ], |
∂qr | ∂qr | ∂qr |
ars = Σ { m | ∂x | ∂x | + | ∂y | ∂y | + | ∂z | ∂z | ) } = asr. | |||
∂qr | ∂qs | ∂qr | ∂qs | ∂qr | ∂qs |
Thus T is expressed as a homogeneous quadratic function of
the quantities q̇1, q̇2, . . . q̇n, which are called the generalized
components of velocity. The coefficients arr, ars are called the coefficients
of inertia; they are not in general constants, being
functions of the q’s and so variable with the configuration.
Again, If (X, Y, Z) be the force on m, the work done in an infinitesimal
change of configuration is
where
Qr = Σ X | ∂x | + Y | ∂y | + Z | ∂z | . |
∂qr | ∂qr | ∂qr |
The quantities Qr are called the generalized components of force.
The equations of motion of m being
we have
Σ { m ẍ | ∂x | + ÿ | ∂y | + z̈ | ∂z | ) } = Qr. |
∂qr | ∂qr | ∂qr |
Now
ẋ = | ∂x | q̇1 + | ∂x | q̇2 + . . . + | ∂x | q̇n, |
∂q1 | ∂q2 | ∂qn |
whence
∂ẋ∂q̇r = ∂x∂qr | (8) |
Also
d | ∂x | = | ∂2x | q̇1 + | ∂2x | q̇2 + . . . + | ∂2x | q̇r = | ∂ẋ | . | |
dt | ∂qr | ∂q1∂qr | ∂q2∂qr | ∂qn∂qr | ∂qr |
Hence
ẍ | ∂x | = | d | ẋ | ∂x | − ẋ | d | ∂x | = | d | ẋ | ∂ẋ | − ẋ | ∂ẋ | . | |
∂qr | dt | ∂qr | dt | ∂qr | dt | ∂q̇r | ∂qr |
By these and the similar transformations relating to y and z the
equation (6) takes the form
d | ∂T | − | ∂T | = Qr. | |
dt | ∂q̇r | ∂qr |
If we put r = 1, 2, . . . n in succession, we get the n independent equations of motion of the system. These equations are due to Lagrange, with whom indeed the first conception, as well as the establishment, of a general dynamical method applicable to all systems whatever appears to have originated. The above proof was given by Sir W. R. Hamilton (1835). Lagrange’s own proof will be found under Dynamics, § Analytical. In a conservative system free from extraneous force we have
where V is the potential energy. Hence
Qr = − | ∂V | , |
∂qr |
and
d | ∂T | − | ∂T | = − | ∂V | . | |
dt | ∂q̇r | ∂qr | ∂qr |
If we imagine any given state of motion (q̇1, q̇2 . . . q̇n) through
the configuration (q1, q2, . . . qn) to be generated instantaneously
from rest by the action of suitable impulsive forces, we find on
integrating (11) with respect to t over the infinitely short duration
of the impulse
∂T∂q̇r = Qr′, | (15) |
where Qr′ is the time integral of Qr and so represents a generalized component of impulse. By an obvious analogy, the expressions ∂T/∂q̇r may be called the generalized components of momentum; they are usually denoted by pr thus
Since T is a homogeneous quadratic function of the velocities q̇1, q̇2, . . . q̇n, we have
2T = | ∂T | q̇1 + | ∂T | q̇2 + . . . + | ∂T | q̇n = p1q̇2 + p2q̇2 + . . . + pnq̇n. |
∂q̇1 | ∂q̇2 | ∂q̇n |
Hence
2dTdt | = ṗ1q̇1 + ṗ2q̇2 + . . . + ṗnq̇n + ṗ1q̈1 + ṗ2q̈2 + . . . + ṗnq̈n | |||||||||||||
= | ∂T | + Q1 q̇1 + | ∂T | + Q2 q̇2 + . . . + | ∂T | + Qn q̇n + | ∂T | q̈1 + | ∂T | q̈2 + . . . + | ∂T | q̈n | ||
∂q̇1 | ∂q̇2 | ∂q̇n | ∂q̇1 | ∂q̇2 | ∂q̇n | |||||||||
=dTdt + Q1q̇1 + Q2q̇2 + . . . + Qnq̇n, |
or
dTdt = Q1q̇1 + Q2q̇2 + . . . + Qnq̇n. | (19) |