10.3 Wave impedance

Impedance is the ratio of a driving quantity to the response it produces — pressure to velocity, force to velocity, voltage to current. For a wave it is not an independent property but a consequence of the wave equation itself: the two fields that make up a wave are locked together in a fixed ratio set by the medium. This lesson derives that ratio and generalises it.

Acoustic impedance, derived

In a plane sound wave the pressure and the particle velocity are not free to vary independently; the equation of motion ties them.

Z = ρ₀c from linearised Euler Derivation

Take a plane wave p=P0ei(kxωt)p' = P_0\,e^{i(kx-\omega t)} and u=U0ei(kxωt)u' = U_0\,e^{i(kx-\omega t)}. The linearised Euler equation relates them:

ρ0ut=px        ρ0(iω)U0=(ik)P0        U0=kωρ0P0.\rho_0\frac{\partial u'}{\partial t} = -\frac{\partial p'}{\partial x} \;\;\Longrightarrow\;\; \rho_0(-i\omega)U_0 = -(ik)P_0 \;\;\Longrightarrow\;\; U_0 = \frac{k}{\omega\rho_0}P_0.

The acoustic dispersion is ω=ck\omega = ck, so k/ω=1/ck/\omega = 1/c, giving

P0U0=ρ0cZ.\frac{P_0}{U_0} = \rho_0 c \equiv Z.
where
ZZ
specific acoustic impedance Pa·s/m
ρ0\rho_0
equilibrium density of the medium kg/m³
cc
speed of sound m/s

The specific acoustic impedance Z=ρ0cZ = \rho_0 c is a property of the medium alone — it depends on the density and sound speed, not on the wave’s amplitude or frequency.

p′P₀ = 1.00 Pau′U₀ = 2.430 mm/sp′ and u′ are in phasep′ / u′ = Z = ρ₀ c = 411.6 kg/(m²·s)
ρ₀1.20
c343
P₀1.00 Pa
Z = ρ₀ c411.6

Substituting a plane-wave ansatz into linearised Euler (ρ₀ ∂u′/∂t = −∂p′/∂x) together with the wave dispersion ω = ck gives U₀ = P₀ / (ρ₀ c) ≡ P₀ / Z. The impedance Z = ρ₀c is a *medium property*, not a wave property: it depends on ρ₀ and c, not on the specific wave. Water has Z ≈ 1.5 × 10⁶, air ≈ 410 — a factor-of-3500 mismatch that the middle-ear ossicles are built to bridge.

The numbers matter for what follows. Water has Z1.5×106Pa⋅s/mZ\approx 1.5\times10^6\,\text{Pa·s/m}; air has Z410Z\approx 410. Their ratio, some 3500, is a severe impedance mismatch, and — as the reflection lesson will show — it is why almost no airborne sound crosses into water, and why any device transferring sound between such mismatched media needs an impedance-matching stage.

Mechanical impedance, generalised

The same idea applies to any linear system where a sinusoidal force FF drives a sinusoidal velocity vv: the mechanical impedance is Zmech=F/vZ_\text{mech} = F/v. For a damped, driven harmonic oscillator,

Zmech(ω)  =  b  +  i ⁣(ωmkω).Z_\text{mech}(\omega) \;=\; b \;+\; i\!\left(\omega m - \frac{k}{\omega}\right).
where
bb
damping coefficient N·s/m
mm
mass kg
kk
stiffness N/m
10-1100101102|Z(ω)|-90°90°∠Z(ω)10-1100101102ω₀ = √(k/m)stiffness-controlled (~k/ω)damping-controlled (~b)mass-controlled (~ωm)
b (damping)0.50
m (mass)1.00
k (stiffness)4.00
ω₀ = √(k/m)2.00

Below ω₀ the stiffness term k/ω dominates and the impedance is *capacitive* (phase −90°); above ω₀ the mass term ωm dominates and the impedance is *inductive* (+90°). At ω₀ the reactive parts cancel and only the damping b remains. The complex impedance is the operative model for the basilar membrane in [Hearing Ch 4.3](/hearing/cochlea/traveling-wave).

Three frequency regimes divide the response, split at the natural frequency ω0=k/m\omega_0 = \sqrt{k/m}:

This impedance is the frequency-domain fingerprint of every driven damped oscillator, and its resonant cancellation of reactances is the same phenomenon that governs electrical RLCRLC circuits and acoustic resonators alike.