The energy in an acoustic field doesn’t just sit there — it flows. The rate at which it flows, per unit area perpendicular to the flow direction, is the acoustic intensity:
I(r,t)=p′(r,t)v′(r,t).
This is a vector (because v′ is) with units of W/m².
Why pressure-times-velocity is the energy flux
Consider a surface element dA with normal n^. The fluid on one side of dA exerts a force p′dAn^ on the fluid on the other side. The fluid on the other side moves at velocity v′. The rate at which work is done by the first fluid on the second is force times velocity in the direction of force:
dPwork=p′dA(n^⋅v′)=(p′v′)⋅n^dA.
So the energy flux vector is exactly I=p′v′ — work done per unit area per unit time. This satisfies the energy continuity equation ∂tE+∇⋅I=0 identically for the linearised acoustic system (a direct calculation from Euler + continuity).
Time-averaged intensity
Most measurements care about the average intensity, not the instantaneous value. For a plane wave with p′=P0cos(ωt−kx) and v′=(P0/ρ0c)cos(ωt−kx):
⟨I⟩=⟨p′v′⟩=ρ0cP02⟨cos2⟩=2ρ0cP02.
In complex notation, using the rule ⟨Re[A~eiωt]Re[B~eiωt]⟩=21Re[A~B~∗] from lesson 2.2:
⟨I⟩=21Re[p~′v~′∗]=2ρ0cP02k^.
For a plane wave, intensity points in the propagation direction, and its magnitude is P02/(2ρ0c).
▶The factor $\tfrac12$ is the time-average of $\cos^2$
For any pair of real sinusoidal signals A(t)=A0cos(ωt+α) and B(t)=B0cos(ωt+β), the time average over one period is
⟨AB⟩=T1∫0TA0B0cos(ωt+α)cos(ωt+β)dt.
Using cosxcosy=21[cos(x−y)+cos(x+y)], the integrand has a constant piece 21A0B0cos(α−β) and an oscillating piece 21A0B0cos(2ωt+α+β). The oscillating piece integrates to zero over a full period. The constant piece gives
⟨AB⟩=21A0B0cos(α−β)=21Re[A~B~∗].
For A=B (same signal), this is 21A02 — the time-average of cos2 is 1/2.
Intensity, energy density, and the speed of sound
Look at the ratio:
⟨E⟩⟨I⟩=P02/2ρ0c2P02/2ρ0c=c.
The intensity is the energy density times the propagation speed. This is the only thing it could be — energy density is energy per volume, intensity is energy per area per time; their ratio must have units of velocity, and for a non-dispersive wave the only velocity in the problem is c. The energy density is transported at the wave’s group velocity, which for acoustic plane waves equals the phase velocity, which equals c.
Numerical scale
For conversational pressure (P0=10−2 Pa):
⟨I⟩=2⋅1.2⋅343(10−2)2≈1.2×10−7W/m2.
Tenths of a microwatt per square metre. For comparison:
Threshold of hearing at 1 kHz: ∼10−12 W/m² (the standard reference).
Conversational speech: ∼10−7 W/m² (above).
Busy street: ∼10−5 W/m².
Painfully loud: ∼1 W/m².
Jet engine at 30 m: ∼10 W/m².
The dynamic range from threshold to pain is 13 orders of magnitude in intensity — or 26 orders in pressure squared. This is why we use decibels.
Next lesson: the impedance ρ0c that keeps appearing, and what it means.