For classical systems with anharmonic forces, Newton's equations for partic
le trajectories are nonlinear, while Liouville's equation for the evolution
of functions of position and momentum is linear and is solved by construct
ing a basis of functions in which the Liouvillian is a tridiagonal matrix,
which is then diagonalized. For systems that are chaotic in the sense that
neighboring trajectories diverge exponentially, the initial conditions dete
rmine the solution to Liouville's equation for short times; but for long ti
mes, the solutions decay exponentially at rates independent of the initial
conditions. These are the relaxation rates of irreversible processes, and t
hey arise in these calculations as the imaginary parts of the frequencies w
here then are singularities in the analytic continuations of solutions to L
iouville's equation. These rates are calculated fur two examples: the inver
ted oscillator, which can be solved both analytically and numerically, and
a charged particle in a periodic magnetic field, which can only be solved n
umerically. In these systems, dissipation arises from traveling-wave soluti
ons to Liouville's equation that couple low and high wave-number modes allo
wing energy to Bow from disturbances that are coherent over large scales to
disturbances on ever smaller scales finally becoming incoherent over micro
scopic scales. These results suggest that dissipation in large scale motion
of the system is a consequence of chaos in the small scale motion. [S1063-
651X(99)07405-X].