Eyring Reverberation Time

Also known as Eyring equation · Norris-Eyring · Eyring-Norris reverberation · reverberation time in a dead room · Sabine correction

T60=0.161 V−S ln⁡(1−αˉ)T_{60} = \frac{0.161\,V}{-S\,\ln(1-\bar{\alpha})}

Worked example: 1000 m³, 600 m² of surface at ᾱ = 0.50 → 0.387 s (Sabine would say 0.537) — press Try an example to run it live, then adjust anything.

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Eyring Reverberation Time explained

VSᾱᾱᾱT60

Sabine's equation has a flaw that only shows up in the rooms people pay to have treated: it never lets the sound stop. Push the absorption coefficient to 1.0 — every surface a perfect absorber, a sound field that cannot survive its first reflection — and Sabine still returns a finite reverberation time. It has to, because it treats absorption as a steady leak proportional to αˉ\bar{\alpha} rather than as something that happens discretely, at each bounce.

Carl Eyring's 1930 paper fixed the accounting. If a fraction αˉ\bar{\alpha} of the energy is lost at every reflection, then a fraction (1−αˉ)(1-\bar{\alpha}) survives, and after nn reflections the surviving energy is (1−αˉ)n(1-\bar{\alpha})^n. That is exponential decay in the number of reflections, and taking its logarithm replaces Sabine's αˉ\bar{\alpha} with −ln⁡(1−αˉ)-\ln(1-\bar{\alpha}). The correction is the honest version and Sabine's is its small-absorption approximation, because −ln⁡(1−x)≈x-\ln(1-x) \approx x when xx is small.

How small is small enough is the practical question. At αˉ=0.1\bar{\alpha} = 0.1 the two forms differ by about 5 %, less than the uncertainty in the coefficients themselves. At 0.3 the gap is 19 %, at 0.5 it is 39 %, and at 0.8 Sabine overstates the reverberation by nearly a factor of two. The working rule is Sabine below 0.2 and Eyring above it — and at αˉ=1\bar{\alpha} = 1 Eyring correctly returns zero, because ln⁡(0)\ln(0) diverges and no sound survives the first reflection.

Neither equation rescues a room whose absorption is all in one place. Both assume the sound field is diffuse, and a treated ceiling over a hard floor and hard walls is emphatically not: the horizontal reflections between parallel hard walls persist long after the vertical ones have died, and the measured decay curve bends rather than falling straight. Millington and Sette proposed a refinement that applies the logarithm surface by surface rather than to the average, which behaves better with mixed materials but misbehaves with any surface at α=1\alpha = 1. In an awkward room, all of these are estimates, and a ray-tracing model or an in-situ measurement is what settles the argument.

Eyring Reverberation Time formula

T60=0.161 V−S ln⁡(1−αˉ)T_{60} = \frac{0.161\,V}{-S\,\ln(1-\bar{\alpha})}
Where
  • T60T_{60}= Reverberation time (s)
  • VV= Room volume (m³)
  • SS= Total surface area (m²)
  • αˉ\bar{\alpha}= Average absorption coefficient

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