177 Basic rigid body dynamics
As an example, suppose we wish to use type I Euler angles as generalized coordinates in
the Lagrangian analysis of the rotational motion of an axially-symmetric body having no
applied moment about the axis of symmetry. The rotational kinetic energy can be written
in the form
T =
1
2
I
a
2
+
1
2
I
t
(
˙
θ
2
+
˙
ψ
2
cos
2
θ) (3.241)
where the moments of inertia are taken about the center of mass and the total spin is
constant. Let us apply Lagrange’s equation in the fundamental form
d
dt
∂T
∂
˙
q
i
−
∂T
∂q
i
= Q
i
(3.242)
where the qs are the Euler angles (ψ, θ, φ). If we assume that neither Q
ψ
nor Q
θ
are
functions of φ or
˙
φ, then it appears that the ψ and θ equations can be solved separately,
treating as a constant in the differentiations, and effectively reducing the number of
degrees of freedom to two.
This application of Lagrange’s equation would be incorrect, however, because the system
actually has three rotational degrees of freedom, but the third Euler angle φ has not entered
the analysis. Thus, we have not used a complete set of generalized coordinates. A correct
approach would be to substitute
=
˙
φ −
˙
ψ sin θ (3.243)
into (3.241) and obtain
T =
1
2
I
a
(
˙
φ −
˙
ψ sin θ )
2
+
1
2
I
t
(
˙
θ
2
+
˙
ψ
2
cos
2
θ) (3.244)
The use of this kinetic energy function in Lagrange’s equation (3.242) leads to correct
equations of motion. An alternate approach would be to notice that φ is an ignorable
coordinate and use the Routhian method.
The second restriction on the use of Lagrange’s equation in a form such as (3.242) is
that true
˙
qs must be used in writing the kinetic energy T (q,
˙
q, t), rather than using quasi-
velocities as velocity variables. A quasi-velocity u
j
is equal to a linear function of the
˙
qs
and has the form
u
j
=
n
i=1
ji
(q, t)
˙
q
i
+
jt
(q, t)(j = 1,...,n) (3.245)
where the right-hand side is not integrable.
A common example of quasi-velocities would be the body-axis components ω
x
,ω
y
,ω
z
of
the angular velocity ω of a rigid body. In terms of Euler angles, which are true coordinates,
we have
ω
x
=
˙
φ −
˙
ψ sin θ
ω
y
=
˙
ψ cos θ sin φ +
˙
θ cos φ (3.246)
ω
z
=
˙
ψ cos θ cos φ −
˙
θ sin φ