The phase velocity is the speed at which a point of constant phase on a sinusoidal wave moves through space. For a wave

a point of constant phase satisfies , so

Here is the angular frequency (rad/s) and is the phase constant (rad/m). The relation is universal — it works for transmission lines, plane waves, sound waves, water waves, anything sinusoidal.

On a transmission line

For a lossless Transmission line with distributed inductance and capacitance per unit length:

Since for any TEM line (a universal geometry-independent identity — see Transmission line):

For a non-magnetic dielectric ():

Common values: RG-58 coax has , giving m/s. Twisted-pair phone cable: . A “5 ns/m” rule of thumb for PCB FR-4 traces corresponds to .

The takeaway: signals on real lines travel slower than , by a factor of . Wavelength on the line is shortened by the same factor: .

In a uniform dielectric

For a Plane wave in an unbounded uniform medium, the same formula:

In free space, — exactly. (The defined speed of light, since 1983.)

Versus group velocity

Phase velocity is the speed of a single Fourier component. A real signal — a pulse, a wave packet — is built from many frequencies. If depends on (a dispersive medium), different components travel at different speeds and the pulse spreads. The pulse envelope moves at the group velocity:

different from . In non-dispersive media (where ), the two coincide.

In a dispersive medium, can exceed without violating relativity — phase velocity isn’t the speed of information transport. is closer to the physical signal speed, and stays at or below in normal media. Electromagnetics mostly works in the non-dispersive lossless regime where the distinction doesn’t matter; group velocity is properly introduced in a later wave-propagation course.

Why “phase” velocity

A snapshot of at is a sinusoid in . At , the same shape has shifted by . The pattern slides through space at speed — the speed at which “the same phase” (e.g., a particular zero crossing, or a peak) appears at successive points.

This is a kinematic quantity: it describes the geometry of the wave pattern, not the speed of energy or information.

Relation to wavelength and frequency

The standard wave-equation identities:

Given any two of , the third is fixed. On a transmission line you typically know (the source frequency) and (from the line’s , or equivalently , ); you compute .

For a 1 GHz signal on a coax with :

A quarter-wave stub on such a line is 5 cm — physically shorter than free-space cm by the same factor.

Why it shows up everywhere

The phase-velocity relation is the bridge between time-domain and space-domain wave behavior. Any time you want to translate “how fast does it oscillate?” () and “how packed are the wavelengths?” () into “how fast does it move?” (), this is the formula. It recurs in TL theory, plane-wave optics, waveguide cutoff analysis, antenna theory, and the dispersion relations of any wave system.