A linear, homogeneous, time-invariant medium admits the plane monochromatic waves (complex notation; the physical signal is the real part) provided and satisfy the dispersion relation of the medium, , solved as or . For real the wave travels without deforming at the phase velocity
The medium is non-dispersive when does not depend on (then and every signal propagates undeformed — the d’Alembert equation) and dispersive otherwise.
Examples
Example 8.2 (Dispersive and non-dispersive)
(i) A string on an elastic bed (restoring force per unit length, or a chain of pendulums), : with — the Klein–Gordon relation, the same as a plasma’s and a waveguide’s (Chapters 14 and 16): , and no real below the cut-off . (ii) Deep-water gravity waves: (admitted), : long waves are faster — for , for . (iii) The chain of atoms, (Chapter 6). (iv) Light in glass, , which is why a prism spreads a spectrum.
Example 8.7 (Klein–Gordon: faster than light, and not)
For : and , so : the phase velocity exceeds (in the ionosphere, a wave’s crests move faster than light) but the group velocity, which carries the signal, stays below it. A phase velocity transports no energy and no information — the crests are like the spot of a lighthouse beam sweeping a distant cloud.