Theory
Johnson et al. (Johnson et al., 1987) defined as twice the pore volume to pore surface ratio weighted by the squared velocity of the inviscid flow; it fixes the high-frequency limit of the viscous loss. In the equivalent density, equation (1), it appears in the square root that blends the low-frequency Darcy behaviour (controlled by ) into the high-frequency one.
When the field is blank the program uses the estimate of equation (2), which corresponds to a pore-shape factor of 1 (cylindrical pores), evaluated with the local gas viscosity and the temperature-scaled flow resistivity. The value used is listed in the acoustic QA table.
Equations
| where | meaning | unit |
|---|---|---|
| Viscous characteristic length (this setting) | m | |
| Viscosity of the local gas | Pa·s | |
| Flow resistivity at the local temperature | Pa·s/m² | |
| Tortuosity, porosity | - |
Default and rule
- Default
- blank = estimated from the flow resistivityComputed by the program
- Rule
Blank: the estimate of equation (2). Because the scaled resistivity is proportional to , the estimate does not change with temperature. Example: air at 20 °C ( Pa·s), Pa·s/m², , gives µm.
- Source
The equations and the estimate follow Johnson et al. Johnson et al. (1987) in the form given by Atalla and Panneton Atalla and Panneton (2000).
Valid range > 0; should not exceed the thermal length
Values
Above 0; entered in µm.
Consistency
The QA gate warns when Thermal characteristic length (JCA / JCAL) is shorter than (real materials have ).
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