GRE Physics Companion: Acoustic Waves, Sound Intensity, and Acoustic Impedance
For a plane acoustic wave in a fluid,
The pressure and particle-velocity amplitudes satisfy
for positive-direction propagation.
The average intensity is
Figure 1. A compact acoustics strategy: identify the medium properties, compute c and ρ0c,
connect pressure to particle velocity, use RMS quantities for intensity, and apply pressure and
velocity continuity at an interface.
1 High-value GRE facts
- c2 = (∂p∕∂ρ)
s.
- For an ideal gas, c =
.
- z0 = ρ0c.
- For a right-moving plane wave, p′ = z0u.
- ⟨I⟩ = prms2∕z
0 = z0urms2.
- LI = 10 log 10(I∕Iref).
- Lp = 20 log 10(prms∕pref).
- Doubling ideal free-field distance lowers level by about 6 dB.
- Pressure reflection at a fluid interface is (z2 − z1)∕(z1 + z2).
- A rigid wall is a pressure antinode and particle-velocity node.
Part I: Original GRE-style problems
Problem 1: characteristic impedance
For a progressive plane wave in a fluid, the characteristic specific acoustic impedance
is
- ρ0∕c
- ρ0c
- c∕ρ0
- ρ0c2
- 1∕(ρ0c)
Problem 2: intensity
The average intensity of a harmonic plane wave is
- prmsρ0c
- prms2∕(ρ
0c)
- prms∕(ρ0c)
- ρ0c∕prms2
- independent of pressure
Problem 3: right-moving pressure and velocity
For a right-moving progressive plane wave,
- pressure and particle velocity differ by 90∘
- pressure and particle velocity are in phase
- particle velocity is always zero
- pressure is always zero
- pressure and particle velocity have unrelated frequencies
Problem 4: intensity level
Increasing intensity by a factor of
changes the sound intensity level by
- 2 dB
- 10 dB
- 20 dB
- 40 dB
- 100 dB
Problem 5: pressure level
Increasing RMS pressure by a factor of
at fixed impedance changes sound pressure level by
- 3 dB
- 6 dB
- 10 dB
- 20 dB
- 100 dB
Problem 6: distance doubling
For an ideal isotropic point source in a lossless free field, doubling distance changes the intensity
level by approximately
- +6 dB
- −6 dB
- +3 dB
- −3 dB
- 0 dB
Problem 7: pressure reflection
At Normal incidence from medium 1 to medium 2, the pressure reflection coefficient
is
- (z1 − z2)∕(z1 + z2)
- (z2 − z1)∕(z1 + z2)
- 2z1∕(z1 + z2)
- 2z2∕(z1 + z2)
- z1z2
Problem 8: matched interface
If
then the pressure reflection coefficient is
- −1
- +1
- 0
- 1∕2
- infinite
Problem 9: rigid wall
At an ideal rigid wall,
- pressure is a node and particle velocity an antinode
- pressure is an antinode and particle velocity a node
- both pressure and particle velocity are nodes
- both are antinodes
- no reflection occurs
Problem 10: air intensity
Take
and
The intensity is closest to
- 9.7 × 10−7 W∕m2
- 9.7 × 10−5 W∕m2
- 4.1 × 10−2 W∕m2
- 0.200 W∕m2
- 413 W∕m2
Problem 11: pressure level
For
and
the sound pressure level is
- 20 dB
- 40 dB
- 60 dB
- 80 dB
- 100 dB
Problem 12: two equal incoherent sources
Two independent incoherent sources each produce intensity
Together they increase the level by approximately
- 1 dB
- 3 dB
- 6 dB
- 10 dB
- 20 dB
Part II: Complete worked solutions
Solution 1
For a progressive plane wave,
Answer: (B).
Solution 2
Using RMS pressure,
Answer: (B).
Solution 3
For positive-direction propagation,
Thus pressure and particle velocity are in phase. Answer: (B).
Solution 4
Answer: (C).
Solution 5
Answer: (D).
Solution 6
Ideal spherical spreading gives
Doubling distance gives
Answer: (B).
Solution 7
Pressure and normal particle-velocity continuity give
Answer: (B).
Solution 8
If
then
Answer: (C).
Solution 9
A rigid wall requires
Thus particle velocity is a node and pressure is an antinode. Answer: (B).
Solution 10
First,
Then
| ⟨I⟩ | =  | (24)
|
| ≈ 9.7 × 10−5 W∕m2. | (25) |
Answer: (B).
Solution 11
| Lp | = 20 log 10 | (26)
|
| = 20 log 10(104) | (27)
|
| = 80 dB. | (28) |
Answer: (D).
Solution 12
The total intensity is
Thus
Answer: (B).
2 GRE checklist
- Distinguish wave speed from particle velocity.
- Use ρ0c as the plane-wave specific acoustic impedance.
- Use RMS pressure in the standard intensity formula.
- Remember the different logarithmic factors: 10 for intensity, 20 for pressure amplitude.
- Apply pressure and normal particle-velocity continuity at a fluid interface.
- Use the acoustic pressure reflection sign, not the string displacement sign.
- A rigid wall is a pressure antinode and velocity node.
- Add physical intensities before converting independent-source results back to decibels.
References
References
[1] PhysicsLibrary, M06-10, Fourier Analysis, Wave Packets, and Dispersion.
[2] PhysicsLibrary, M06-09, Waves on Strings: Reflection, Transmission, and Mechanical
Impedance.
[3] A. P. French, Vibrations and Waves, W. W. Norton, 1971.
[4] L. E. Kinsler, A. R. Frey, A. B. Coppens, and J. V. Sanders, Fundamentals of
Acoustics, 4th ed., Wiley, 2000.