This is a rapid-fire concept check for Acoustic Loads — SPL, Octave Band Analysis. Each line is a Question ::: Answer reveal. Cover the card, say your reasoning out loud, then reveal. If your answer is a bare "yes/no" without a because, count it as a miss — the whole point of acoustics is understanding why the logs and squares behave the way they do.
Every decibel (dB) below refers to Sound Pressure Level relative to pref=20μPa.
Two uncorrelated 140 dB sources combine to 280 dB.
False. Decibels are logarithms of intensity, and logs don't add linearly; uncorrelated sources add in intensity, so doubling gives only +10log10(2)≈+3 dB → 143 dB.
A +6 dB change means the sound pressure has doubled.
True. Since SPL=20log10(p/pref) and 20log10(2)≈6, +6 dB is exactly a factor-2 rise in prms (but a factor-4 rise in intensity).
A +6 dB change means the acoustic intensity has doubled.
False. Intensity ∝p2, so +6 dB (pressure ×2) means intensity ×4. It is +3 dB that doubles intensity, because 10log10(2)≈3.
The OASPL of a spectrum is just the arithmetic average of its octave-band levels.
False. You must convert each band to intensity, sum them, then convert back: LOASPL=10log10(∑10Li/10). The sum is dominated by the loudest band, not the mean.
Adding a band that is 20 dB quieter than the peak changes the OASPL by less than 0.1 dB.
True. A 20 dB deficit means 1/100 the intensity of the peak; adding 1% to the total intensity raises the level by 10log10(1.01)≈0.04 dB — negligible.
Increasing the SPL by 3 dB requires you to double the number of identical uncorrelated engines.
True. Each doubling of independent sources adds intensity, and 10log10(2)≈3 dB, regardless of the starting level.
The 632 Pa peak pressure at 150 dB would crush the spacecraft like a vice.
False. It is a small oscillating modulation on top of ∼105 Pa atmosphere (about 0.6%); the danger is fatigue and resonance from the shaking force, not static crushing.
A one-third-octave analysis of the same launch spectrum always reports a lower OASPL than octave analysis.
False. OASPL is the total energy however you slice it; finer bands just redistribute the same intensity, so the summed OASPL is unchanged (up to rounding).
"To combine two 145 dB sources, average their pressures: (632+632)/2=632 Pa, so still 145 dB."
The error is averaging pressures. Uncorrelated pressures add in quadrature (ptot2=p12+p22), giving 2×632 Pa → 148 dB, not 145.
"SPL uses 10log10 because the reference is a pressure."
Backwards. SPL uses 20log10because it references pressure; the 20 comes from I∝p2, so log of p2 pulls the exponent 2 out front. Intensity level uses 10log10.
"An octave band centered at 500 Hz runs from 250 Hz to 750 Hz."
The limits are wrong. The band spans fc/2 to fc2, i.e. 354 Hz to 707 Hz, whose ratio is exactly 2:1. 250–750 Hz has a ratio of 3:1.
"The band center is the arithmetic mean of the limits: fc=(fL+fU)/2."
It is the geometric mean: fc=fLfU. That makes the band logarithmically centered, matching how we hear and how frequency ratios (octaves) work.
"Because pressures add, two 632 Pa waves give 1264 Pa, i.e. +6 dB."
Only correlated, in-phase waves add pressures directly. Launch acoustic sources are uncorrelated, so intensities add and the rise is +3 dB, not +6 dB.
"The reference pressure 20μPa is arbitrary, so SPL numbers have no physical anchor."
It is not arbitrary: it corresponds to Iref=10−12 W/m² via pref=Irefρc, the human threshold of hearing at 1 kHz. It fixes 0 dB.
"Acoustic loads and mechanical vibration are the same test, so we only need one."
They excite differently: mechanical vibration enters through mounting points, while acoustic loads press on all exposed surfaces at once — see 3.6.11 Random Vibration — PSD, Miles' Equation for the mounting-point route and 3.6.14 Combined Environmental Testing for why both matter.
Human-relevant pressures span roughly 20μPa to 200 Pa — a 10-million-fold range. Logarithms compress this into a readable 0–140 dB, and match the roughly multiplicative way we perceive loudness.
Why do intensities (not pressures) add for uncorrelated launch sources?
With random relative phase, the cross-term in ⟨(p1+p2)2⟩ time-averages to zero, leaving ⟨p12⟩+⟨p22⟩. Since I∝p2, the intensities — the energy carriers — simply sum.
Why does the OASPL usually sit only a few dB above the loudest single band?
Because the sum ∑10Li/10 is dominated by the largest term; quieter bands contribute exponentially less intensity, so their combined effect adds at most a few dB.
Why do we care which octave band holds the most energy, rather than just the OASPL?
A structure amplifies violently only near its natural frequency. Energy in a band that lands on that resonance does far more damage than the same energy elsewhere — see 3.6.10 Structural Natural Frequencies and Mode Shapes.
Why is ρc (the characteristic impedance) the quantity linking pressure to intensity?
For a plane wave, pressure and particle velocity obey p=ρcv, so ρc is the "acoustic resistance." It turns the pressure squared into transmitted power: I=prms2/(ρc). See 2.5.8 Acoustic Impedance and Transmission.
Why is the band center defined as the geometric mean of the limits?
So the band is symmetric in log-frequency: equal musical/octave distance on each side. Arithmetic centering would bias every band toward its high-frequency edge.
Why can acoustic loads produce amplification factors of 10–50× in a thin panel?
At resonance the panel's response is set by its quality factor Q; a lightly damped panel (Q=10–50) stores energy each cycle, so a modest pressure builds into large displacements before losses catch up.
20log10(1)=0 dB. The reference pressure is defined as the 0 dB point (threshold of hearing), not silence.
What does the SPL formula give for perfect silence, prms=0?
log10(0)→−∞, so SPL →−∞ dB. Mathematically it never reaches a finite floor; physically, background noise always sets a real, finite minimum.
What is the OASPL if every one of N bands has the identical level L?
LOASPL=L+10log10(N). All bands add in intensity, so N equal bands raise the total by 10log10N dB.
Combining a 150 dB source with a 100 dB source — what is the result?
Essentially 150 dB. The quieter source is 50 dB down (10−5 of the intensity), so it adds 10log10(1.00001)≈0.00004 dB — undetectable.
Two perfectly correlated, in-phase identical sources — how much do they add?
+6 dB. Correlated pressures add directly (p→2p), and 20log10(2)≈6. This is the correlated exception to the usual +3 dB rule.
Two identical sources exactly out of phase (180°) at the same point — what happens?
They cancel: p1+p2=0, so SPL →−∞ there. Real fields are only partially correlated, so full cancellation happens at isolated nodes, not everywhere.
What OASPL do you get from a single band?
Exactly that band's level: 10log10(10L/10)=L. With one term the log and exponent undo each other — a useful sanity check on the summation formula.
If a band's level is reported as "−∞ dB" (no energy), how does it affect the OASPL?
Not at all: 10−∞/10=0 contributes nothing to the intensity sum, so the OASPL is unchanged. Empty bands are silent partners.
Recall One-line rules to carry away
+3 dB ::: doubles intensity (two uncorrelated equal sources).
+6 dB ::: doubles pressure (or two correlated in-phase sources).
+10 dB ::: ten times the intensity.
+20 dB ::: ten times the pressure.
OASPL ::: dominated by the loudest band, always ≥ any single band.
Next stops: 3.6.13 Shock Loads and SRS for the transient cousin of these steady-state loads, and 3.6.14 Combined Environmental Testing for how acoustic, random-vibration, and shock environments are qualified together.