2018
DOI: 10.1103/physrevlett.120.054501
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Acoustic Streaming and Its Suppression in Inhomogeneous Fluids

Abstract: We present a theoretical and experimental study of boundary-driven acoustic streaming in an inhomogeneous fluid with variations in density and compressibility. In a homogeneous fluid this streaming results from dissipation in the boundary layers (Rayleigh streaming). We show that in an inhomogeneous fluid, an additional nondissipative force density acts on the fluid to stabilize particular inhomogeneity configurations, which markedly alters and even suppresses the streaming flows. Our theoretical and numerical… Show more

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Cited by 73 publications
(91 citation statements)
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“…As discussed more fully in § 2, the mechanism underlying this large-amplitude streaming is the baroclinic production of sound-wave vorticity arising from the misalignment of fluctuating isobars and mean isopycnals. Similarly, non-classical streaming phenomena have been observed in microfluidic systems with gradients in density; in particular, Karlsen et al (2016Karlsen et al ( , 2018 recently obtained a local expression for the acoustic force density driving the streaming flow as a function of the acoustic-wave characteristics.…”
Section: Introductionmentioning
confidence: 84%
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“…As discussed more fully in § 2, the mechanism underlying this large-amplitude streaming is the baroclinic production of sound-wave vorticity arising from the misalignment of fluctuating isobars and mean isopycnals. Similarly, non-classical streaming phenomena have been observed in microfluidic systems with gradients in density; in particular, Karlsen et al (2016Karlsen et al ( , 2018 recently obtained a local expression for the acoustic force density driving the streaming flow as a function of the acoustic-wave characteristics.…”
Section: Introductionmentioning
confidence: 84%
“…Indeed, by numerically integrating the streaming equations (2.15)-(2.19) together with the wave amplitude equation (3.16) and eigenvalue problem (3.9), the instantaneous dynamics need not be simulated using supercomputing resources (e.g. as in Loh et al (2002)) nor approximated by alternatively time-advancing the wave dynamics and the streaming flow (Karlsen et al 2018). Our algorithm thereby enables accurate and inexpensive numerical simulations over several thousand acoustic-wave periods to be performed in a regime where the waves and streaming flow are strongly coupled.…”
Section: Discussionmentioning
confidence: 99%
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“…The cross-over from boundary-to bulk-driven horizontal streaming rolls may be characterized by the height-towidth ratio B = lL z /L : we compute the critical value B crit , where the velocity ratio (39) is unity, and thus, l L z L < B crit , boundary-driven streaming dominates, l L z L > B crit , bulk-driven streaming dominates. (40) For water, Eq. (39) leads to the ratio B crit water = 0.35, and since L z = 0.1L in the setup of Figs.…”
Section: Bulk-driven Versus Boundary-driven Streaming Rollsmentioning
confidence: 99%