When coupling from Pressure Acoustics, Frequency Domain, an effective theory is used to include the effects of viscous boundary layers. It is a theory that has been developed for modeling acoustics in microfluidic devices, a research area called Acoustofluidics, see
Ref. 4,
Ref. 6, and
Ref. 7. The theory solves the acoustic fields with pressure acoustics and use the Thermoviscous Boundary Layer Impedance boundary condition to include the effects from the viscous boundary layers. It then computes the force contribution from the viscous boundary layers from an analytical expression and impose it as slip velocity on the boundary. This model is valid if the viscous boundary layer thickness is a lot smaller than the acoustic and the characteristic geometry length scales. The benefits of this model is that it is not necessary to numerically resolve the viscous boundary layers.
The acoustic body force faco contains the term that gives rise to traditional Eckart streaming and terms that depend on the gradient of the material parameters (
Ref. 6). The gradients in material parameters can either be caused by a solvent (
Ref. 5) or a temperature gradient (
Ref. 8) and are the source terms for thermoacoustic and baroclinic streaming. The slip velocity
vslip is given by the acoustic pressure field
p1.
The effective theory is used when coupling from Pressure Acoustics, Frequency Domain. It has been validated against a full model and experiments in the research area of acoustics in microfluidic devices, see
Ref. 4,
Ref. 6, and
Ref. 8. For more information on the theoretical derivation see
Ref. 4 and
Ref. 6.