Phase Velocity, Group Velocity & Dispersion: Wave-Packet Theory and de-Broglie Waves

Phase Velocity & Group Velocity — In-depth (Dispersion, Wave Packets & de Broglie)

Phase Velocity & Group Velocity — Expanded Explanation

By Mohan Dangi Gold medalist

1. Intuition recap

Imagine a set of ripples (many sinusoidal waves) traveling together. Each ripple crest moves at its own phase velocity v_p. But if the ripples are slightly different in wavelength, groups of crests appear and disappear — those groups move at the group velocity v_g. The group carries the energy and the signal, while the phase rides inside the group.

2. Phase velocity (mathematical and geometric)

Plane wave:

y(x,t) = A cos(ω t − k x)

Set the phase constant: φ = ω t − k x = const. Differentiating w.r.t. t:

dφ/dt = ω − k (dx/dt) = 0 ⇒ dx/dt = ω/k = v_p

So geometrically a phase point (e.g., a crest) moves at v_p = ω/k. Note: v_p depends on k when the medium is dispersive (i.e., ω=ω(k)), so different spectral components move at different v_p.

3. Group velocity — derivation & physical meaning

Consider two close frequencies ω₁, ω₂ (carrier near ω̄) and wave numbers k₁, k₂. The superposition becomes:

y = 2A cos(Δω t / 2 − Δk x / 2) · sin(ω̄ t − k̄ x)

Maxima of the envelope satisfy Δω t/2 − Δk x/2 = const, so the envelope velocity is

v_g = (Δω/2) / (Δk/2) = Δω / Δk

In differential limit (narrowband around k₀):

v_g = dω/dk |_{k₀}

Physical meaning: For narrowband signals, v_g is the velocity of the packet center and usually the velocity of energy and information transfer.

4. Dispersion relation, Taylor expansion & pulse evolution

Start from the dispersion relation ω = ω(k) (exact for the medium). Expand around a central wave number k₀:

ω(k) ≈ ω₀ + ω'(k₀)(k−k₀) + 1/2 ω''(k₀)(k−k₀)² + ...

When building a wave packet from spectral components A(k), the field is

Ψ(x,t) = ∫ A(k) e^{i[k x − ω(k) t]} dk.

Inserting the Taylor expansion and pulling out carrier oscillation e^{i(k₀ x − ω₀ t)}:

Ψ(x,t) ≈ e^{i(k₀ x − ω₀ t)} ∫ A(k) e^{i[(k−k₀)(x − ω' t) − 1/2 ω'' (k−k₀)² t + ...]} dk.

The integral shows three effects:

  1. Carrier motion: the factor x − ω' t shows the envelope moves at v_g = ω'.
  2. Dispersion-induced spreading: the quadratic term −½ ω'' (k−k₀)² t causes the integral to broaden with time — this is group velocity dispersion (GVD).
  3. Higher-order distortion: higher derivatives of ω(k) cause asymmetry, pulse chirp, or shape changes.

Definition: GVD parameter is β₂ = ω''(k₀). If β₂ > 0 (normal dispersion) pulses broaden; if β₂ < 0 (anomalous) pulses can compress or form solitons in nonlinear media.

Practical note: Optical fiber engineers usually express dispersion via D(λ) (ps/(nm·km)) but it’s derived from ω'' via change of variables between k and λ.

5. Gaussian wave packet — exact spreading formula (quantum)

Consider a free particle of mass m with an initial Gaussian position wavefunction centered at x=0:

Ψ(x,0) = (1/(2π σ₀²))^{1/4} exp(−x²/(4 σ₀²) + i k₀ x)

Time evolution (using free-particle Schrödinger equation) gives a Gaussian at later times with width

σ_x(t) = σ₀ √{1 + ( (ħ t) / (2 m σ₀²) )² }

This formula shows:

  • At small t, σ_x(t) ≈ σ₀.
  • At large t, σ_x(t) ≈ (ħ t) / (2 m σ₀) — i.e., linear growth with time.

Interpretation: A sharply localized particle (small σ₀) has a large spread in momentum and thus spreads quickly. A wide initial packet spreads slowly.

This quantum spreading is the direct manifestation of GVD for matter waves: the dispersion relation ω(k)=ħ k²/(2m) has ω''≠0, so packets spread.

6. de Broglie waves: vp, vg and their relation

Using ω = E/ħ and k = p/ħ:

v_p = ω/k = E/p

For relativistic particle, E = γ m c² and p = γ m v, so

v_p = c² / v

Group velocity for the matter-wave packet equals the particle velocity:

v_g = dω/dk = d(E/ħ)/d(p/ħ) = dE/dp = v

Together they satisfy the elegant relation:

v_p · v_g = c²

So when the particle is slow (v_g ≪ c), the phase velocity is superluminal (v_p ≫ c) — but the product remains . Superluminal v_p carries no information.

7. Signal, front and information velocities (causality)

There are multiple velocities one might consider:

  • Phase velocity v_p: movement of phase surfaces; not an information carrier.
  • Group velocity v_g: usually the velocity of energy/information for narrowband signals.
  • Front velocity (or signal-front velocity): speed of the very first non-zero part of a signal — this obeys causality and cannot exceed the universal limit (e.g., c in vacuum).

In media with anomalous dispersion, v_g can exceed c or be negative for certain narrowband pulses — but the front velocity and causal signal velocity remain ≤ c. The apparent superluminal effects are due to reshaping of the pulse by the medium, not real superluminal transport of new information.

Mathematically, causality of the medium's response function ensures the Kramers–Kronig relations hold; these guarantee that information velocity stays causal despite unusual group velocity behavior.

8. Worked numeric examples

Example 1 — de Broglie velocities

Take an electron with classical speed v = 0.01 c (~3×10⁶ m/s):

v_p = c² / v = (3×10⁸ m/s)² / (3×10⁶ m/s) = 3×10¹⁰ m/s ≈ 100 c
v_g = v = 0.01 c

Phase velocity is enormous, but group velocity (the particle speed) is subluminal.

Example 2 — optical pulse in normal dispersion

For an optical fiber with β₂ = +20 ps²/km and an initial Gaussian pulse of 1 ps width, the dispersive broadening after L = 10 km roughly scales as

Δτ(L) ≈ τ₀ √{1 + ( (β₂ L) / τ₀² )² } ≈ τ₀ √{1 + ( (20 ps²/km × 10 km) / (1 ps)² )² } ≈ large

This shows why long-distance pulse propagation requires dispersion compensation.

9. Applications and experiments

  • Optical communications: Dispersion management (fiber Bragg gratings, dispersion compensating fibers) is essential to prevent pulse overlap and bit errors.
  • Ultrafast optics: Chirped pulse amplification and pulse compression exploit GVD and nonlinearities.
  • Electron microscopy: Electron wave packet spreading limits temporal resolution in ultrafast electron diffraction.
  • Quantum wave-packet experiments: Direct measurements of packet spreading and dispersion relations verify these theoretical predictions.

10. FAQ and common confusions (expanded)

Q: If phase velocity can exceed c, why can't we send messages faster?

A: Because phase velocity describes motion of constant-phase surfaces which carry no new information — only the modulation (envelope) and the signal front can carry information. The front is constrained by causality.

Q: Is group velocity always equal to energy velocity?

A: Usually in weakly dispersive, lossless media, yes — energy propagates at vg. But in strongly absorbing or highly dispersive media the relation can be more complicated; one must compute the Poynting vector or energy flux directly.

Q: What about negative group velocity?

A: Negative vg means the peak of a reshaped pulse appears to exit a sample before it enters — again caused by pulse reshaping and not superluminal information transfer.

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