In order to introduce the concept of generalized coordinates, let us first consider a few simple examples.
Consider, first, the problem of a simple pendulum moving in the x-y plane. The pendulum has a length l and moves under the action of gravity, so that its potential energy is mgh. The system is illustrated in the figure below.
We could use Cartesian coordinaets x and y to describe the location of the pendulum bob, but x and y are not independent. In fact, since the length of the pendulum is constant, they are related by
This condition would need to be imposed as a constraint on the system,
which can be inconvenient. It is more natural to use the angle
that the pendulum makes with respect to the vertical to describe the
motion. But what would be the equation of motion for
?
In order to find out what this is, we only need to express the
Lagrangian in terms of
. Now, the Lagrangian in terms of x
and y is givn by
where we have introduced a general potential function, however, for this example, we know that the potential is given by U(x,y) = -mgy.
The Cartesian coordinates x and y are related to
by a
set of transformation equations:
In order to transform the kinetic energy, we need the time derivatives of the transformation equations:
Substituting the transformations and their derivatives into the Lagrangian gives
Now, given the Lagrangian, we just turn the crank on the Euler-Lagrange
equation and derive the equation of motion for
:
so that the equation of motion is
As another example, consider again a particle moving in the x-y plane
subject to a potential U that is a function only of the distance
of the particle from the origin of the coordinate system. This distance
is
, so that U = U(r). An example would be
a radial harmonic potential
, which is a ``bowl'' potential
shown below:
Of course, we can choose to work in Cartesian coordinates, x, and y. In this case, we would write down the Lagrangian
where the potential U(r) is expressed as a function of x and y through the dependence of r on x and y. Then, the equations of motion for x and y can be computed with forces obtained via the chain rule
which is perfectly correct. However, it obviscates some of the important
physics of the problem, which can be revealed by working in
polar coordinates r and
, which are more natural for this
problem. These are related to x and y via the transformations:
with time derivatives
Substituting into the kinetic energy gives, after some algebra
so that the Lagrangian can be expressed as
There will be two equations of motion for r and
given by
Thus, all we need to do to determine the equations of motion is turn the crank. For r, we have
We see immediately that if
, then
, and the particle will remain in circular
motion with a centripetal acceleration
.
For
, we have
which can also be written as
The last line is in the form of a conservation law, which states that
the quantity,
. This is
known as the conservation of areal velocity. The constant
is usually defined such that
or
Substitution of this conservation law into the radial equation gives an uncoupled equation for r alone:
The conservation law and uncoupled radial equation would have been difficult to decude directly in terms of Cartesian coordinates, however, the Lagrangian formulation allows these results to be derived rather easily using the machinery of the Euler-Lagrange equation.
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Mark Tuckerman