7.1 Reflection at a boundary (normal incidence)

A plane wave in medium 1 of impedance Z1=ρ1c1Z_1 = \rho_1 c_1 encounters a flat boundary with medium 2 of impedance Z2=ρ2c2Z_2 = \rho_2 c_2. At normal incidence (the wave travels along the surface normal), what happens?

The boundary conditions

Two physical requirements at the interface:

  1. Pressure continuity. The pressure on the two sides of an infinitesimally thin interface must match — otherwise an infinite force per unit volume would act on the interface. So p1=p2p_1' = p_2' at the boundary.

  2. Normal velocity continuity. The fluids on the two sides must move together at the interface — otherwise a vacuum or interpenetration would form. So v1,n=v2,nv_{1,n}' = v_{2,n}' at the boundary.

These two conditions, applied to plane-wave fields, determine the reflection coefficient RR (ratio of reflected to incident pressure amplitudes) and transmission coefficient TT (ratio of transmitted to incident).

Plane-wave decomposition

In medium 1, the field is incident plus reflected:

p1(x,t)  =  Piei(ωtk1x)  +  Prei(ωt+k1x).p_1'(x, t) \;=\; P_i\, e^{i(\omega t - k_1 x)} \;+\; P_r\, e^{i(\omega t + k_1 x)}.

The velocity is in phase with each separately, with the right sign:

v1(x,t)  =  1Z1 ⁣[Piei(ωtk1x)Prei(ωt+k1x)].v_1'(x, t) \;=\; \frac{1}{Z_1}\!\left[P_i\, e^{i(\omega t - k_1 x)} - P_r\, e^{i(\omega t + k_1 x)}\right].

(Note the minus on the reflected wave: it travels in x-x, so its velocity points in x-x.)

In medium 2, only the transmitted wave (no source in medium 2, no reflection from infinity):

p2(x,t)  =  Ptei(ωtk2x),v2(x,t)  =  PtZ2ei(ωtk2x).p_2'(x, t) \;=\; P_t\, e^{i(\omega t - k_2 x)}, \qquad v_2'(x, t) \;=\; \frac{P_t}{Z_2}\, e^{i(\omega t - k_2 x)}.

Matching at x=0x = 0

Pressure continuity gives Pi+Pr=PtP_i + P_r = P_t. Velocity continuity gives (PiPr)/Z1=Pt/Z2(P_i - P_r)/Z_1 = P_t/Z_2. Two linear equations, two unknowns (Pr/PiP_r/P_i and Pt/PiP_t/P_i). Solving:

    R  =  PrPi  =  Z2Z1Z2+Z1,T  =  PtPi  =  2Z2Z2+Z1.    \boxed{\;\;R \;=\; \frac{P_r}{P_i} \;=\; \frac{Z_2 - Z_1}{Z_2 + Z_1}, \qquad T \;=\; \frac{P_t}{P_i} \;=\; \frac{2 Z_2}{Z_2 + Z_1}.\;\;}

These are the Fresnel-like coefficients for normal-incidence acoustic reflection. They are the most-used formulas in this chapter.

Working through the algebra

From Pi+Pr=PtP_i + P_r = P_t and (PiPr)/Z1=Pt/Z2(P_i - P_r)/Z_1 = P_t/Z_2:

Substituting the first into the second: (PiPr)/Z1=(Pi+Pr)/Z2(P_i - P_r)/Z_1 = (P_i + P_r)/Z_2. Multiply out: Z2(PiPr)=Z1(Pi+Pr)Z_2(P_i - P_r) = Z_1(P_i + P_r), i.e. (Z2Z1)Pi=(Z1+Z2)Pr(Z_2 - Z_1) P_i = (Z_1 + Z_2) P_r. Divide: R=Pr/Pi=(Z2Z1)/(Z2+Z1)R = P_r/P_i = (Z_2 - Z_1)/(Z_2 + Z_1).

Then T=1+R=2Z2/(Z1+Z2)T = 1 + R = 2 Z_2 / (Z_1 + Z_2).

Three regimes

Power reflection and transmission

The power reflection and transmission coefficients are

RP=R2=(Z2Z1Z2+Z1)2,TP=1RP=4Z1Z2(Z1+Z2)2.R_P = |R|^2 = \left(\frac{Z_2 - Z_1}{Z_2 + Z_1}\right)^2, \qquad T_P = 1 - R_P = \frac{4 Z_1 Z_2}{(Z_1 + Z_2)^2}.

The sum RP+TP=1R_P + T_P = 1 — energy conservation across a non-absorbing boundary.

For air-to-water (huge impedance ratio \sim 3600), RP0.999R_P \approx 0.999 — about 99.9% of incident sound is reflected at the air-water interface. This is why you can’t hear someone underwater from above the surface, or vice versa, and why the middle ear’s impedance-matching mechanism (lever ratio of 22:1 in human ossicles) is so important.

Looking ahead

We’ve done the simplest case: normal incidence. The general angle of incidence requires accounting for the direction of the wavevectors on both sides. That’s the next lesson — and the resulting law turns out to be a direct analogue of Snell’s law in optics.