Theory
At high frequency the viscous boundary layers in the pores are thin and the gas moves as an inviscid fluid around the fibres; its effective density tends to . A straight-pore material has ; fibrous packings are close to 1 (about 1.0-1.1), foams higher. In the JCA/JCAL density (Johnson et al., 1987) the tortuosity multiplies the inertial term and also appears in the viscous correction, equation (1), and in the estimate of Viscous characteristic length (JCA / JCAL) when that is blank, equation (2). It does not enter the bulk modulus.
Equations
| where | meaning | unit |
|---|---|---|
| Tortuosity (this setting) | - | |
| Equivalent density of the packing | kg/m³ | |
| Density and viscosity of the local gas | kg/m³, Pa·s | |
| Porosity | - | |
| Flow resistivity at the local temperature | Pa·s/m² | |
| Viscous characteristic length | m | |
| Angular frequency | rad/s |
Default and rule
- Default
- 1.0
- Rule
1.0 (straight pores), a close approximation for fibrous wools.
- Source
The equivalent density follows Johnson et al. Johnson et al. (1987) in the form given by Atalla and Panneton Atalla and Panneton (2000). The typical values quoted above are indicative; they are not taken from a cited source.
Valid range ≥ 1; warning above 3
Values
(refused below 1).
High tortuosity
Above 3 the acoustic QA gate warns: high for a fibrous packing (typically 1.0-1.5).
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 5
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
- Johnson, D. L., Koplik, J. and Dashen, R. (1987). Theory of dynamic permeability and tortuosity in fluid-saturated porous media. Journal of Fluid Mechanics, 176, 379-402. DOI 10.1017/S0022112087000727