Theory
An incompressible run assumes one uniform temperature: the density follows the ideal-gas law at the ambient (or mean) pressure, equation (1), and the viscosity Sutherland's law, equation (2), which depends on the temperature only. A hot exhaust gas is much less dense and more viscous than cold air: at 700 °C and 1 atm air has a density of about 0.36 kg/m³ against 1.20 kg/m³ at 20 °C, so the same mass flow is more than three times faster.
For the compressible solver the temperature is the starting value of the temperature field and the inlet temperature, unless an inlet sets its own (Inlet temperature, which follows this value when left empty). The solver then computes the temperature everywhere, so it may differ from this value inside the muffler.
The acoustics use the speed of sound at this temperature when the acoustic medium is uniform; with the medium mapped from a compressible CFD run they use the solved temperature field instead.
Equations
| where | meaning | unit |
|---|---|---|
| Gas temperature | K | |
| Density | kg/m³ | |
| Ambient pressure | Pa | |
| Gauge reference pressure (0, or half the previous static pressure drop, see the density reference) | Pa | |
| Molar mass of the gas | kg/kmol | |
| Universal gas constant, 8314.47 | J/(kmol K) | |
| Dynamic viscosity | Pa s | |
| Sutherland coefficient | kg/(m s K^0.5) | |
| Sutherland temperature | K |
| where | meaning | unit |
|---|---|---|
| Speed of sound | m/s | |
| Ratio of heat capacities | - | |
| Specific heat capacity at constant pressure | J/(kg K) |
Default and rule
- Default
- 20 °C
- Rule
20 °C.
- Source
The ideal-gas law and the ideal-gas speed of sound; Sutherland's law (Sutherland, 1893).
Valid range above -273.15 °C; the temperature-dependent heat capacity covers 200-3000 K
Values
Above -273.15 °C. Older case files that stored the temperature in kelvin are converted on loading.
One temperature
An incompressible run has no energy equation: a muffler that cools the gas noticeably needs the compressible solver with heat transfer for a temperature that changes along the flow.