The GLE can be derived from the harmonic bath Hamiltonian by simply solving Hamilton's equations of motion, which take the form
This set of equations can also be written as second order differential equation:
In order to derive an equation for q, we solve explicitly for the
dynamics of the bath variables and then substitute into the equation for q.
The equation for
is a second order inhomogeneous differential equation,
which can be solved by Laplace transforms. We simply take the Laplace
transform of both sides. Denote the Laplace transforms of q and
as
and recognizing that
we obtain the following equation for
:
or
can be obtained by inverse Laplace transformation, which is
equivalent to a contour integral in the complex s-plane around a
contour that encloses all the poles of the integrand. This contour is
known as the Bromwich contour. To see how this works, consider the
first term in the above expression. The inverse Laplace transform is
The integrand has two poles on the imaginary s-axis at
.
Integration over the contour that encloses these poles picks up both
residues from these poles. Since the poles are simple poles, then, from
the residue theorem:
By the same method, the second term will give
. The last term
is the inverse Laplace transform of a product of
and
.
From the convolution theorem of Laplace transforms, the Laplace transform of
a convolution gives the product of Laplace transforms:
Thus, the last term will be the convolution of q(t) with
.
Putting these results together, gives, as the solution for
:
The convolution term can be expressed in terms of
rather than q
by integrating it by parts:
The reasons for preferring this form will be made clear shortly. The bath variables can now be seen to evolve according to
Substituting this into the equation of motion for q, we find
We now introduce the following notation for the sums over bath modes appearing in this equation:
Eq. (1) is known as the generalized Langevin equation. Note that
it takes the form of a one-dimensional particle subject to a potential
,
driven by a forcing function R(t) and with a nonlocal (in time) damping
term
, which depends, in general, on
the entire history of the evolution of q. The GLE is often taken as a
phenomenological equation of motion for a coordinate q coupled to a
general bath. In this spirit, it is worth taking a moment to discuss the physical
meaning of the terms appearing in the equation.