Theory
Champoux and Allard (Champoux and Allard, 1991) defined as twice the ratio of pore volume to pore surface. At low frequency the gas in the pores exchanges heat with the fibres and is compressed isothermally (bulk modulus ); at high frequency it is compressed adiabatically (). The transition is controlled by the thermal length and, in JCAL, by the static thermal permeability, equation (1). In JCA, is not an input but follows from , equation (2).
Equations
| where | meaning | unit |
|---|---|---|
| Thermal characteristic length (this setting) | m | |
| Viscous characteristic length | m | |
| Static thermal permeability | m² | |
| Equivalent bulk modulus | Pa | |
| Gas: ratio of specific heats, absolute pressure, viscosity, Prandtl number, density | SI | |
| Porosity | - | |
| Angular frequency | rad/s |
Default and rule
- Default
- blank = 2 × viscous lengthComputed by the program
- Rule
Blank: , the usual ratio for fibrous materials.
- Source
The equations are cross-checked against Atalla and Panneton (2000); the thermal length is defined by Champoux and Allard (1991). The ratio 2 is a common estimate for fibrous materials; it is not taken from a cited source.
Valid range > 0; ≥ viscous length
Values
Above 0; entered in µm.
Shorter than the viscous length
The QA gate warns when .
Verified
Checked in a full acoustic run of a packed resonator (2026-11-11): every quality check passes; with estimated parameters the TL agrees with Miki within about 1 dB below 1 kHz and falls 7-9 dB below it at 2 kHz.
Related 4
References 2
- Atalla, Y. and Panneton, R. (2000). Inverse characterization of the geometrical macroscopic parameters of porous materials. Canadian Acoustics, 28(3), 80-81. Web page
- Champoux, Y. and Allard, J.-F. (1991). Dynamic tortuosity and bulk modulus in air-saturated porous media. Journal of Applied Physics, 70(4), 1975-1979. DOI 10.1063/1.349482