One over the compressibility βs measured at constant entropy. The adiabatic bulk modulus is denoted
Ks and gives a measure of the compressibility of the fluid and is directly related to the speed of sound
cs in the fluid. SI unit: Pa.
RMS instantaneous sound pressure at a point during a time interval, T, long enough that the measured value is effectively independent of small changes in
T. SI unit: Pa = N/m
2.
The matrix D relating strain to stresses:
Nonlinear strain measure used in large-deformation analysis. In a small strain, large rotation analysis, the Green–Lagrange strain corresponds to the engineering strain, with the strain values interpreted in the original directions. The
Green–Lagrange strain is a natural choice when formulating a problem in the undeformed state. The conjugate stress is the
second Piola–Kirchhoff stress.
A velocity field u that has the property of having rotation
∇ ×
u = 0 everywhere, where the first term is the vorticity of the fluid. In such a fluid the viscous stress does not contribute to the acceleration of the fluid. The mean pressure in this fluid is described by
Bernoulli’s equation.
Conjugate stress to Green–Lagrange strain used in large deformation analysis.
Average rate of sound energy transmitted in a specified direction at a point through a unit area normal to this direction. SI unit: W/m
2.
Absolute instantaneous sound pressure in any given cycle of a sound wave at some specified time. SI unit: W/m
2.
The interaction between thermodynamic and acoustic phenomena, which takes into account the temperature oscillations that accompany the acoustic pressure oscillations. The combination of these oscillations produces thermoviscous acoustic effects. Thermoviscous acoustic phenomena are modeled by solving the full linearized Navier–Stokes equation (momentum equation), the continuity equation, and the energy equation. Thermoviscous acoustics is also known as viscothermal acoustics or thermoacoustics.
When a flow is irrotational ∇ ×
u = 0 the vector field (velocity field) can always be derived from a scalar potential
ϕ(x) as
u = ∇ϕ, where
ϕ is the velocity potential. See also
irrotational background velocity field.