Theory
Sound in air is absorbed by two mechanisms:
- viscosity and heat conduction (classical and rotational absorption);
- vibrational relaxation of oxygen and nitrogen molecules, whose relaxation frequencies depend on the water-vapour content and the temperature.
The program computes the pure-tone attenuation coefficient of ISO 9613-1, equation (1), with the relaxation frequencies of equations (2) and (3). At the default distance of 0.5 m the absorption is small (hundredths of a dB at a few kHz); it becomes significant at large distances and high frequencies.
Equations
| where | meaning | unit |
|---|---|---|
| Attenuation coefficient | dB/m | |
| Frequency | Hz | |
| Ambient pressure | kPa | |
| Reference pressure, 101.325 | kPa | |
| Air temperature (this setting, in kelvin) | K | |
| Reference temperature, 293.15 | K | |
| Relaxation frequencies of oxygen and nitrogen | Hz | |
| Molar concentration of water vapour (Relative humidity) | % |
Default and rule
- Default
- 25 °CMeasured
- Rule
25 °C.
- Source
The equations are those of ISO 9613-1, eqs. (3)-(5). The implementation was verified against a tabulation of the attenuation coefficients (relative humidity 10-100 %, the temperatures of the input range, the tabulated frequencies): 1789 of 1848 values agree within 0.5 % (median 0.07 %). The remaining 59 differ because of transcription errors in the tabulation (decade or digit errors, e.g. 0.897 where 0.0897 is correct at 20 °C / 63 Hz / 70 %). The input range 15-40 °C is the program's.
Valid range -40 to 60 °C (radiated SPL: 15 to 40 °C)
Values
-40 to 60 °C, the range of the insertion loss's outside air.
Radiated SPL
The radiated SPL accepts 15 to 40 °C only: a run that computes it is refused outside that range.