Abstract

While boundary-driven acoustic streaming resulting from the interaction of sound, fluids and walls in symmetric acoustic resonances have been intensively studied in the literature, the acoustic streaming fields driven by asymmetric acoustic resonances remain largely unexplored. Here, we present a theoretical and numerical analysis of outer acoustic streaming flows generated over a fluid–solid interface above which a symmetric or asymmetric acoustic standing wave is established. The asymmetric standing wave is defined by a shift of acoustic pressure in its magnitude, i.e., , and the resulting outer acoustic streaming is analyzed using the limiting velocity method. We show that, in symmetric acoustic resonances (), on a slip-velocity boundary, the limiting velocities always drive fluids from the acoustic pressure node towards adjacent antinodes. In confined geometry where a slip-velocity condition is applied to two parallel walls, the characteristics of the obtained outer acoustic streaming replicates that of Rayleigh streaming. In an asymmetric standing wave where , however, it is found that the resulting limiting velocity node (i.e., the dividing point of limiting velocities) on the slip-velocity boundary locates at a different position to acoustic pressure node and, more importantly, is shown to be independent of , enabling spatial separation of acoustic radiation force and acoustic streaming flows. The results show the richness of boundary-driven acoustic streaming pattern variations that arise in standing wave fields and have potentials in many microfluidics applications such as acoustic streaming flow control and particle manipulation.

Highlights

  • Acoustic streaming is the steady flow driven by acoustic energy dissipation in a viscous fluid

  • We have demonstrated here that outer acoustic streaming flows driven by 1D symmetric and asymmetric standing wave fields near a fluid–solid interface (FSI) could behave very differently

  • The results for symmetric acoustic resonances replicate the characteristics of Rayleigh streaming: Nodes of acoustic pressure and limiting velocity share same locations; that is, on a slip-velocity boundary which drives circulations of outer acoustic streaming the direction of limiting velocity always goes from acoustic pressure nodes to adjacent antinodes

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Summary

Introduction

Acoustic streaming is the steady flow driven by acoustic energy dissipation in a viscous fluid. The resulting streaming from the former case is known as boundary-driven acoustic streaming, which is usually observed in standing wave fields near walls or suspended objects, while the streaming produced by the latter case is called ‘quartz wind’ or Eckart streaming [2], which is typically observed in the bulk of channels much larger than the acoustic wavelength [3]. Understanding the driving mechanisms of acoustic streaming and its variations is important for the design of acoustofluidic devices to enhance or to suppress its effect for lab-on-achip applications [4], such as heat and mass transfer enhancement, microfluidic actuation, sensing, sonoporation and drug delivery, and particle manipulation. In most micro-acoustofluidic systems of interest where standing waves are typically generated, the acoustic streaming fields are generally dominated by boundary-driven acoustic streaming.

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