The acoustic radiation force on a spherical thermoviscous particle in a thermoviscous fluid including scattering and microstreaming
Bjørn G. Winckelmann, Henrik Bruus
TL;DR
This study extends the analytical theory of the acoustic radiation force on a single spherical particle by incorporating elastic solids, temperature- and density-dependent viscosities, tangential Stokes-drift boundary conditions, and inner streaming inside droplets. Using unified potential theory and partial-wave expansions, the authors derive general first- and second-order solutions for both fluids and solids and obtain closed-form long-wavelength expressions for F^rad = F^rad_{11} + F^rad_{2,\text{in}}. They show that microstreaming can dominate F^rad for small particles and provide detailed comparisons with Gor'kov, Settnes–Bruus, Karlsen–Bruus, and Doinikov in various limiting cases, highlighting the importance of boundary-layer effects and thermal coupling. The results refine predictions for acoustofluidic manipulation and aerosol dynamics, particularly in regimes where boundary layers are non-negligible or where viscosity depends on temperature and density.
Abstract
We derive general analytical expressions for the time-averaged acoustic radiation force on a small spherical particle suspended in a fluid and located in an axisymmetric incident acoustic wave. We treat the cases of the particle being either an elastic solid or a fluid particle. The effects of particle vibrations, acoustic scattering, acoustic microstreaming, heat conduction, and temperature-dependent fluid viscosity are all included in the theory. Acoustic streaming inside the particle is also taken into account for the case of a fluid particle. No restrictions are placed on the widths of the viscous and thermal boundary layers relative to the particle radius. We compare the resulting acoustic radiation force with that obtained from previous theories in the literature, and we identify limits, where the theories agree, and specific cases of particle and fluid materials, where qualitative or significant quantitative deviations between the theories arise.
