2021
DOI: 10.1016/j.euromechflu.2020.11.005
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Acoustic streaming outside spherical particles and parameter analysis of heat transfer enhancement

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Cited by 9 publications
(3 citation statements)
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“…Recent experiments and numerical simulations revealed complexity and difficulties in capturing the streaming phenomenon [7,[21][22][23][24][25][26][27][28]. Natural convection and acoustic streaming were shown to be difficult to separate in the laboratory and numerical challenges resulted from the need to capture compressible fluid dynamics on temporal scales ranging from the acoustic-wave period to the slow time scale over which the streaming flow evolves.…”
Section: Introductionmentioning
confidence: 99%
“…Recent experiments and numerical simulations revealed complexity and difficulties in capturing the streaming phenomenon [7,[21][22][23][24][25][26][27][28]. Natural convection and acoustic streaming were shown to be difficult to separate in the laboratory and numerical challenges resulted from the need to capture compressible fluid dynamics on temporal scales ranging from the acoustic-wave period to the slow time scale over which the streaming flow evolves.…”
Section: Introductionmentioning
confidence: 99%
“…Next, we show that the sudden increase in the liquid water volume can also be attributed to the rapid enhancement in heat transfer due to stronger acoustic streaming. Enhancement of heat transfer during acoustic streaming is reported in the literature. When the ice detaches from the substrate and starts rotating with the acoustic streaming flow, the temperature of the drop is observed to rapidly increase with time, leading to a sharp increase in the water volume. We calculate the variation in the heat transfer coefficient at the ice and water interface by equating the convective heat transfer between water and ice and the thermal energy responsible for the melting of the ice as follows, h A normald ( T avg i , t T avg w , t ) = L where T avg i , t and T avg w , t are respectively the average temperature of ice and water at time t , m ̇ denotes the mass of ice drop at different time intervals and is calculated from the equation: = prefix− ρ i normald V i , t normald t The variation of the heat transfer coefficient with time is presented in Figure d.…”
Section: Resultsmentioning
confidence: 92%
“…It is particularly difficult to separate the natural convection from the acoustic streaming. This requires considering the dynamics of compressible fluids on temporal scales ranging from the acoustic wave period to the slow time scale over which the streaming flow evolves (Hyun et al 2005, Aktas and Ozgumus 2010, Parvizian et al 2014, Wada et al 2014, Karlsen et al 2018, Michel and Chini 2019, Chen et al 2021, El Ghani et al 2021, Jiang et al 2021.…”
Section: Introductionmentioning
confidence: 99%