Abstract

We consider the size spectrum of entrained bubbles under strong free-surface turbulence (SFST). We investigate the entrainment bubble-size spectrum per unit (mean) interface area, , with dimension length , and develop a physical/mechanistic model for through energy arguments. The model obtains two distinct regimes of , separated by bubble-size scale . For bubble radius , the effects of gravity dominate those of the surface tension force , and , where is the turbulence dissipation rate. For , surface tension is more important and . From the model, we show that , the capillary length scale, and not the generally assumed Hinze scale . For an air–water interface and Earth gravity, 1.5 mm. The model provides an – entrainment regime map that identifies a critical dissipation rate (constant for given and ) above which there is appreciable air entrainment, thus separating SFST and weak FST. We confirm the theoretical model and its predictions using two-phase, high-fidelity direct numerical simulations of a canonical FST flow using the conservative volume-of-fluid method: the respective power laws of and for and ; the value ; the scaling ; and the predictions of the – entrainment regime map.

Highlights

  • Air entrainment occurs and plays important roles in both natural processes and engineering applications

  • We investigate the air entrainment across a free surface induced by underlying strong free-surface turbulence (SFST), its bubble-size

  • The selected direct numerical simulations (DNS) cases with/without air entrainment correctly fall into the predicted regions of strong/weak FST, substantially confirming the predictions of § 2

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Summary

Introduction

Air entrainment occurs and plays important roles in both natural processes and engineering applications. For the air entrainment phase, other researchers (Loewen, O’Dor & Skafel 1996; Rojas & Loewen 2007; Blenkinsopp & Chaplin 2010; Deike, Melville & Popinet 2016; Wang, Yang & Stern 2016) confirm the power-law dependence N(r) ∝ r−10/3 for larger bubbles in breaking waves experiments and simulations. & Peregrine (2001), we derive a (r, )-plane prediction of when air entrainment occurs in free-surface turbulence (FST). The DNS confirms the key predictions of the scaling model: the gravity- and surface-tension-dominated power-law regimes and slopes; the separation scale r0 = rc (≈1.5 mm for an air–water interface in Earth gravity); and the scaling with 2/3 (over the range we considered). Plotting the DNS data on the –r regime map confirms the critical dissipation for air entrainment, cr ∼ O(10−2 m2 s−3), for an air–water interface and Earth gravity

Scaling for bubble-size distribution of air entrainment in SFST
Direct numerical simulations of FST
Conclusion
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