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Clustering, coalescing and bursting processes in surface bubbles of surfactant water flows

Published online by Cambridge University Press:  14 October 2024

Yasunori Watanabe*
Affiliation:
Faculty of Engineering, Hokkaido University, North 13 West 8, Sapporo 0608628, Japan
Ayumi Saruwatari
Affiliation:
Faculty of Engineering, Hokkaido University, North 13 West 8, Sapporo 0608628, Japan
*
*Corresponding author. E-mail: [email protected]

Abstract

Breaking waves aerate seawater surfaces and form whitecaps in the open ocean. The aerated surface area, or whitecap coverage, has been used to macroscopically parametrize air–sea momentum and gas exchange. However, the microscopic mechanisms of the generation, evolution and attenuation of surface bubbles in whitecaps remain poorly understood. In this study, we examined the size distributions and size-dependent lifetimes of surface bubbles generated by water sheet entry and air injection on a porous plate during the clustering, coalescing and bursting processes, depending on surfactant concentrations and bubble mobility. Mechanisms of coalescence through film thinning of adjacent bubble walls owing to the inter-bubble attraction and Marangoni forces experimentally described the surfactant-dependent bubble growth, finally achieving bubble bursting, which were statistically characterized in a population balance analysis. Lagrangian bubble lifetimes were described by the Weibull distribution, providing that surfactant in seawater extended the probabilistic survival periods of surface bubbles two times longer than those of clean bubbles.

Type
Research Article
Creative Commons
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This is an Open Access article, distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivatives licence (http://creativecommons.org/licenses/by-nc-nd/4.0), which permits non-commercial re-use, distribution, and reproduction in any medium, provided that no alterations are made and the original article is properly cited. The written permission of Cambridge University Press must be obtained prior to any commercial use and/or adaptation of the article.
Copyright
© The Author(s), 2024. Published by Cambridge University Press

Impact Statement

The aggregation of breaking-wave-induced surface bubbles on seawater surfaces contributes to the enhancement of air–sea gas transfer, thereby impacting marine ecosystem management. The transient features of oceanic bubble aggregation – dependent on the polydispersivity of bubble size, bubble mobility and surfactant concentration – must be identified to predict their effects on the ocean environment. In this study, we characterized individual bubble behaviours during the coalescing and bursting processes in simplified experiments modelling plunging jets and divergent surface flows through precision image analysis. We observed active coalescence of non-surfactant bubbles colliding through attraction by inter-bubble forces, while aggregating behaviours were predominant at surfactant concentrations that suppress coalescence owing to the Marangoni forces, which modified mechanisms of the total bubble loss and thus probabilistic bubble lifetimes. We also observed another bursting mechanism for travelling bubbles through surface replacement on the bubble cap, which influenced the decay process of surface bubble aggregations. The findings will contribute as the first step in understanding complex oceanic bubble behaviours in surface flows.

1. Introduction

In the surf zone, air bubbles generated by breaking waves are entrained into bulk seawater and entrapped within breaking-wave-induced vortices and turbulence (Reference Watanabe, Saeki and HoskingWatanabe, Saeki & Hosking 2005; Reference WatanabeWatanabe 2022) (figure 1a), thereby contributing to the dissipation of wave energy (Reference Lamarre and MelvilleLamarre & Melville 1991; Reference Callaghan, Deane and StokesCallaghan, Deane & Stokes 2016) and dissolution of gases into seawater (Reference Niida and WatanabeNiida & Watanabe 2018). When turbulence weakens, buoyant bubbles are released from the vortices and rise towards the sea surface. Bubbles arriving at the surface may aggregate and remain as a foam structure for long periods, enhancing the chemical and biological activities that support marine ecosystems (Reference Schilling and ZessnerSchilling & Zessner 2011). In the open ocean, wind-induced breakers aerate wave faces to create active whitecaps; new foam patches emerge behind the crests through buoyant degassing of entrapped bubble plumes (Reference Deane and StokesDeane & Stokes 2002), which exponentially decay over time (Reference Monahan and MuircheartaighMonahan & Muircheartaigh 1980) (figure 1b). The whitecap has roles in exchanging heat and moisture between air and sea (Reference MarmorinoMarmorino 2005; Reference Watanabe and MoriWatanabe & Mori 2008; Reference Wanninkhof, Asher, Ho, Sweeney and McGillisWanninkhof et al. 2009) and in producing sea spray aerosols through bubble bursting (Reference CallaghanCallaghan 2013; Reference VeronVeron 2015), which is significantly influenced by variations of surfactants covering ocean surfaces (Reference Jähne and HaußeckerJähne & Haußecker 1998). The area covered by this foam has been used in the parametrization of gas transfer velocity (Reference Monahan and LuMonahan & Lu 1990). The extension of the foam area along wave crests, defined as the crest length, has been used as a parameter to estimate wave energy dissipation and flux exchange (Reference MelvilleMelville 1996). Although macroscopic investigations of photographic whitecap data are commonly performed for oceanic parametrization with wind velocity (Reference MonahanMonahan 1971; Reference Callaghan, Deane and Dale StokesCallaghan, Deane & Stokes 2008), the fundamental mechanisms of whitecap evolution through the aggregation, coalescence and bursting of bubbles floating on the sea surface remain poorly understood.

Figure 1. Photographs of aerated water generated by shoaling wave splash in the surf zone, taken at Pecatu, South Bali (a) and patches of surface bubbles drifted behind whitecaps, taken at Mombetsu, Hokkaido (b).

Bubble–bubble interactions in bulk liquid flows have been studied both experimentally (Reference Soto, Maddalena, Fraters, van der Meer and LohseSoto et al. 2018) and theoretically (Reference ChestersChesters 1991; Reference Chan, Klaseboer and ManicaChan, Klaseboer & Manica 2011). When a bubble approaches and collides with a neighbouring bubble, drainage thins the disk-shaped film between the bubbles. If the thinning film is destabilized and ruptured by van der Waals forces, capillary waves generated around the rupture hole rapidly propagate on the coalescing bubble surfaces until the spherical bubble form is recovered (Reference Soto, Maddalena, Fraters, van der Meer and LohseSoto et al. 2018). The bubble may break up under sufficient bulk flow disturbances (Reference HinzeHinze 1955). The mechanisms that underlie the deformation and breakup of a bulk bubble rising in a turbulent flow via wake instability have been examined elsewhere (Reference Ravelet, Colin and RissoRavelet, Colin & Risso 2011). In breaking waves, as surface tension modifies surface forms at the onset of wave breaking (Reference DuncanDuncan 2001), subsequent splashing behaviours, characterizing bubble entrainment through interactions between turbulence and surface, are also dependent on seawater surfactants (Reference Liu and DuncanLiu & Duncan 2006). Reference Deane and StokesDeane & Stokes (2002) found that turbulent breakup of the entrained bubbles results in a distinct bubble size distribution of power-law scaling. The void fraction associated with the bulk bubble entrainment is an essential parameter to estimate energy budget in breaking wave turbulence (Reference Na, Chang and LimNa, Chang & Lim 2019). The presence of wave-induced vortices also influences bubble motion; bubbles initially entrained at shallow-level seawater are transported in depths by a Langmuir type of vortical convection (Reference Czerski, Brooks, Gunn, Pascal, Matei and BlomquistCzerski et al. 2022). In a stage of bubble rise, the bulk vortices modify paths, velocity and drag of buoyant bubbles and enhance aggregation to form bubble clusters through bubble–vorticity interactions (Reference Watanabe, Oyaizu, Satoh and NiidaWatanabe et al. 2021).

When rising bulk bubbles arrive at a free surface and float, their local behaviours are governed by distinctive dynamics. Surface bubbles comprise three types of surfaces: a liquid film covering the top of the bubble (i.e. the bubble cap), a meniscus surface surrounding the cap and a submerged bubble wall (Reference TobaToba 1959). The meniscus forms through a balance of hydrostatic pressure and surface tension on the circular edge of the bubble cap, thereby creating a sloping free surface around the cap (figure 2a). If another bubble is present on the meniscus surface, that bubble must climb the sloping surface because of the tangential component of buoyancy (figure 2c); both bubbles attract each other to the point of aggregation, regardless of whether there is sufficient current to transport them. Reference NicolsonNicolson (1949) developed a mechanical model of bubble aggregation based on the apparent attractive force acting between the bubbles. The aggregation of multiple surface bubbles results in the formation of a bubble cluster or raft (Reference Néel and DeikeNéel & Deike 2021; Reference WatanabeWatanabe 2022).

Figure 2. Schematic illustrations of (a) bubble-cap film thinning through drainage, (b) retraction of the rim bounding the film as the bubble bursts, (c) bubble attraction on the meniscus surface and (d) neck expansion during coalescence.

The coalescence of contacting surface bubbles may progress under a mechanism similar to that of bulk bubbles; when the film separating adjacent bubbles ruptures, various modes of capillary waves propagate on the cap films of the coalescing bubbles (figure 2d), causing oscillatory deformation until a spherical form is recovered (Reference Shaw and DeikeShaw & Deike 2021). While the size distribution of clustering bubbles changes during coalescence, cluster attenuation is also caused by bursting of the surface bubble. Reference Lhuissier and VillermauxLhuissier & Villermaux (2011) described the microscopic bursting mechanism of an isolated stationary surface bubble. The Bénard–Marangoni effect destabilizes the thinning bubble-cap film through gravitational and viscous drainage (figure 2a), resulting in the nucleation of a hole near the edge of the bubble cap. This opening rapidly expands at Taylor–Culick velocity until the cap is eliminated (figure 2b). Reference Néel and DeikeNéel & Deike (2021) experimentally studied changes in a bubble population caused by coalescing and bursting processes in stationary rafts of monodisperse surfactant bubbles that were generated by air ejection from a circular array of submerged needles.

These findings contribute to the broader understanding of the fundamental coalescing and bursting processes of surface bubbles; however, further understandings of bubble–flow interactions, which may modify the processes of clustering, coalescing and bursting, are required for applications to complex oceanic bubble flows. Additionally, bubble dynamics is strongly dependent on the physiochemical properties of seawater (Reference Slauenwhite and JohnsonSlauenwhite & Johnson 1999), which contains numerous surfactants, marine organisms and particulates (Reference Schilling and ZessnerSchilling & Zessner 2011) that exhibit seasonal and regional effects according to annual fluctuations of biological activity (Reference Wurl, Wurl, Miller, Johnson and VagleWurl et al. 2011). Because surfactants are responsible for the formation of sea foam and stabilization of bubbles against coalescence and breakup, the surfactant concentration must be considered when predicting the growth and dissipation of whitecaps in the open ocean and in aerated seawater in the surf-zone foam (Reference Callaghan, Deane, Dale Stokes and WardCallaghan et al. 2012; Reference Callaghan, Deane and Dale StokesCallaghan, Deane & Stokes 2013; Reference Villermaux, Wang and DeikeVillermaux, Wang & Deike 2022) (figure 1). In this study, the mechanisms to induce bubble clustering, colliding, coalescing and bursting are discussed in terms of the experimental parameters of bubble mobility and surfactant concentration; the study objective is to provide fundamental parameters characterizing the transient bubble population, size distribution and bubble lifetime, modified by mobility and organization of surface bubbles, in experiments modelling plunging jets and divergent surface flows, as the first step in understanding complex behaviours of whitecap bubbles in turbulent breaking waves.

The remainder of this paper is organized as follows. Section 2 describes the experimental set-ups, experimental conditions and bulk bubble sizes, as well as image analyses to measure the locations, sizes and travelling velocities of individual bubbles. Section 3 explains behaviours of surface bubbles in coalescing and bursting processes, characterizing the bubble size distributions. Analytical models of the film thinning on adjacent bubble walls, causing coalescence, and the drainage in a bubble-cap film, leading to bubble bursts, are explained in § 4. The regional properties of bubble populations through binary coalescence and their dependency on the surfactant concentration are statistically investigated in § 5. Section 6 discusses contributions of relative frequencies of coalescence and bursting to total bubble loss in population balance analysis. Bubble lifetime probability distributions derived from bubble tracking are examined in § 7. The conclusion is presented in § 8.

2. Experiments

Characteristic size, shape and motion of bubbles involved in breaking waves vary in time and space through breakup, coalescence and convection in anisotropic turbulence evolving in splashing waves (Reference Deane and StokesDeane & Stokes 2002; Reference Watanabe, Saeki and HoskingWatanabe et al. 2005; Reference Czerski, Brooks, Gunn, Pascal, Matei and BlomquistCzerski et al. 2022; Reference Villermaux, Wang and DeikeVillermaux et al. 2022). In order to avoid direct measurements of such complex bubble-laden turbulent flows, simplified model experiments, focusing on major bubble behaviours in wave plunging and degassing, have been commonly performed to find characteristic aspects of the flows in the breaking process. Air entrainment at plunging planar jets supported by a vertical wall has been experimentally investigated to identify the distributions of void fraction (Reference Cumming and ChansonCumming & Chanson 1997a), bubble diffusion in a turbulent shear layer formed under the jets (Reference Cumming and ChansonCumming & Chanson 1997b; Reference Brattberg and ChansonBrattberg & Chanson 1998) and the mechanisms of entrainment and breakup (Reference Cumming and ChansonCumming & Chanson 1999). Reference ChansonChanson (1995) discussed analogies of turbulent bubble flow under planar jets with that developed in turbulent hydraulic jumps and bores. Bubble plumes generated by consecutive bubble ejection from porous plates (Reference Anagbo and BrimacobeAnagbo & Brimacobe 1990; Reference AbadieAbadie et al. 2022) and needles (Reference RissoRisso 2018) have been extensively studied to identify effects of bubble agitation on rise velocity and bubble drag in terms of void fraction. Reference Néel and DeikeNéel & Deike (2021) used needle-generated bubbles as an experimental model of oceanic bubbles aggregating and bursting on surfactant water surfaces, aiming to find fundamental properties of mass transfer between air and sea. These findings obtained in the model experiments have provided additional interpretations for specific aspects of oceanic bubble flows. In this study, we followed the conventional approach introducing model experiments to generate bubbles, which provided characteristic behaviours of surface bubbles responding in the specific flows explained below.

2.1 Experimental set-ups

We performed laboratory experiments using two bubble generation methods: bubble entrainment by planar plunging jets (S1) and air ejection through a circular porous ceramic plate (S2). In experiment S1 (figure 3ac), a circulation system consisting of a head tank ($200\,{\rm mm} \times 115\,{\rm mm}\times 100\,{\rm mm}$), transparent test tank ($380\,{\rm mm}{\,\times\,}190\,{\rm mm}\,{\times}\, 215\,{\rm mm}$) and submerged hydraulic pumps produced a steady sheet of falling water that splashed onto still water in the test tank, causing bubble entrainment; this is the simplest model of a plunging breaker jet. The head tank, which was divided into two chambers by submerged walls, had a 2 mm opening over the bottom end of the tank. Liquid was pumped up from both bottom sides of the test tank, then delivered to chamber 1 and overflowed the submerged wall; this cycle prevented disturbed liquid from flowing into the test tank. In chamber 2, the stabilized liquid surface passed down through an opening along one side wall of the test tank as a planar sheet, creating a bubble plume beneath the impacting still water in the test tank. The surface level in the head tank was maintained at a constant water head difference of 100 mm. Reference Cumming and ChansonCumming & Chanson (1997a) have explained evolution of bubble flows under the planar plunging jets, as schematically illustrated in figure 3(c). When the descending planar jet impinges on the still water surface, the resulting velocity gradient beneath the outer jet surface induces a shear stress, which pulls the water near the surface deeper into the bulk for creating a cusp-like cavity close to the jet surface (Reference Kiger and DuncanKiger & Duncan 2012). The cavity elongated downward by the shear becomes unstable and finally breaks up into bubbles to be transported downward with turbulent diffusion in the momentum shear layer expanding towards depths (Reference Cumming and ChansonCumming & Chanson 1997a). While the bubbles are decomposed into smaller ones by turbulent disturbances during descending transport in the shear layer, the diffused bubbles rise up where downward momentum sufficiently attenuates away from the plunging jet. Surface bubbles were illuminated by a red-light-emitting diode panel ($410\,{\rm mm} \times 230\,{\rm mm}$) through the transparent tank bottom. Backlit top-down-view images of the surface bubbles over a field of view of $90\,{\rm mm} \times 70\,{\rm mm}$ were recorded using a high-speed digital video camera (resolution of $1280\,{\times}\, 1024$ pixels) from above the tank by means of a 45$^{\circ }$ angle mirror; the recording frequency was 250 Hz. We defined a coordinate system with the origin at 20 mm from the wall covered by the liquid sheet on the $x$ axis and the centre of the tank on the transverse $y$ axis. Original 8-bit images of backlit bubbles in the domain of $0\le x\le 90$ mm were acquired at a resolution of 0.088 mm pixel$^{-1}$.

Figure 3. Two experimental set-ups for artificial bubble generation. (ac) Experiment S1: entrainment using planar plunging jets. (df) Experiment S2: air ejection through a circular porous ceramic plate. (c,f) Schematic of typical flow patterns formed in each experiment.

In experiment S2, a circular porous plate (diameter of 50 mm) was placed on one bottom end of the test tank (380 mm length$\,{\times}\, 190$ mm width$\,{\times}\, 215$ mm height; figure 3df). Air was injected from an air pump to the plate at a constant discharge rate of 500 ml s$^{-1}$ to generate air bubbles in a tank filled with liquid. As described for S1, surface bubbles were illuminated by a light-emitting diode panel through the transparent bottom of the test tank, then recorded by a high-speed video camera from above. Backlit images from the outer edge of the ceramic plate (60 mm from the wall, downstream) over a field of view of $110\,{\rm mm} \times 90\,{\rm mm}$ were acquired at a resolution of 0.126 mm pixel$^{-1}$. The buoyant bubbles produced on the porous plate entrain the bulk water upward, resulting in liquid circulation in a tank with horizontal divergent flow near the surface and convergent flow in the bulk (Reference Anagbo and BrimacobeAnagbo & Brimacobe 1990; Reference Niida and WatanabeNiida & Watanabe 2018) (see figure 3f), which induces active bubble transport on the surface flow.

Two different time scales of measurements were considered in this study. A long time measurement at a low recording frequency (1.0 Hz) for 100.0 s was used for statistical analysis for equilibrium state of bubble population (figures 9 and 12 in § 3, and discussions in § 4). Dynamic behaviours of surface bubbles, including bubble tracking, were analysed by high-speed images recorded at 250 Hz for 5.0 s (1250 sampling frames), which are discussed in §§ 5, 6 and 7.

Aliquots of purified water containing the non-ionic surfactant Triton X-100 at concentrations of $C= 0$, 200, 400 and $800\,{\mathrm {\mu }}$g l$^{-1}$ were used in the experiments. Triton X-100, which mimics the effects of natural seawater, has been used to model surfactant enrichment in seawater (Reference Wurl, Wurl, Miller, Johnson and VagleWurl et al. 2011). The surfactant concentrations used in this study (200, 400 and $800\,{\mathrm {\mu }}$g l$^{-1}$) are within the ranges of mean concentrations for oligotrophic, mesotrophic and eutrophic seawater conditions, respectively (Reference Wurl, Wurl, Miller, Johnson and VagleWurl et al. 2011). For each concentration, the surface tension was given by reference to the experimental work of Reference Wu, Dai and MicaleWu, Dai & Micale (1999): $\gamma \approx 71.0$, 70.2 and 67.6 dyn cm$^{-1}$ for $C=200$, 400 and $800\,{\mathrm {\mu }}$g l$^{-1}$, respectively. Reference Néel and DeikeNéel & Deike (2021) studied influences of surface contamination by sodium dodecylsulphate and Triton X-100 on behaviours of surface bubbles. They used surfactant water at concentrations of 0.25–$50\,{\mathrm {\mu }}$M (corresponding to 162–$32\,350\,{\mathrm {\mu }}$g l$^{-1}$) of Triton X-100 in the experiments, covering the current concentration range. The flow set-ups used in S1 and S2 were controlled to produce identical population densities of surface bubbles at $C=0$, allowing comparisons of surfactant-concentration-dependent effects in both bubble populations with the common population of non-surfactant bubbles.

2.2 Sizes of rising bubbles in bulk liquid

We performed preliminary backlit experiments to measure rising bulk bubbles. Backlit bubbles at medium depth, illuminated by a light-emitting diode panel placed on an adjacent side wall, were recorded from another side of the tank (see superposed images in figure 4). The sizes of the backlit bubbles were estimated using edge detection based on an established level-set method (Reference Watanabe, Oyaizu, Satoh and NiidaWatanabe et al. 2021).

Figure 4. Probability densities of circle-equivalent diameters of submerged bubbles for experiments S1 (a) and S2 (b).

Figure 4 shows the probability distributions of circle-equivalent diameters of submerged bubbles, $d_0$, for both experiments. Bubbles generated in S1 had larger diameters in $d_0 < 1$ mm and were mainly distributed in the class $0 < d_0 < 5$ mm for all surfactant concentrations, featuring polydisperse bubbles. The observed mean diameters were $\overline {d_{01}} = 2.12$ mm ($C= 0\,{\mathrm {\mu }}$g l$^{-1}$), 1.97 mm ($C=200\,{\mathrm {\mu }}$g l$^{-1}$), 1.86 mm ($C= 400\,{\mathrm {\mu }}$g l$^{-1}$) and 1.89 mm ($C= 800\,{\mathrm {\mu }}$g l$^{-1}$). In S2, the probability distribution was narrower (1.0–3.5 mm) and nearly symmetric around the mean diameter. The estimated mean diameters, $\overline {d_{02}}$, were 2.28, 2.10, 2.38 and 2.31 mm for surfactant concentrations of 0, 200, 400 and $800\,{\mathrm {\mu }}$g l$^{-1}$, respectively. Thus, mean bulk bubble sizes were similar between experiments S1 and S2, whereas high polydispersivity was observed in experiment S1. It should be noted that, according to Reference Néel and DeikeNéel & Deike (2021), variations of surfactant concentration have no influence on the sizes of needle-generated bubbles. The current bubble sizes for all concentrations also exhibited an identical distribution with minor fluctuations.

2.3 Locations and sizes of surface bubbles

The edge detection technique is commonly used for estimation of the locations and sizes of sprays (e.g. Reference Watanabe and IngramWatanabe & Ingram 2015) and bubbles (e.g. Reference Watanabe, Oyaizu, Satoh and NiidaWatanabe et al. 2021) on backlit images. In this method, the particle size is determined from the area enclosed by a closed particle edge on an image, and the particle position is given as the centre of the closed area. We observed that the planar shapes of the surface bubbles have circular features, which are typically in contact under aggregation (figure 21a in Appendix A). General edge detection methods may provide erroneous detection of aggregated surface bubbles because the ring-shaped backlit shadows of the bubbles are connected to the shadows of adjacent bubbles, thus resulting in unnecessary areas enclosed by outer edges of the connected ring shadows within the aggregate.

The circle Hough transform (CHT) procedure, a circle detection method, is widely used in image analyses. Multiple improvements have been proposed to detect these inherent locations in parameter space (e.g. Reference Yuen, Princen, Illingworth and KittlerYuen et al. 1990). Reference Atherton and KerbysonAtherton & Kerbyson (1999) combined previous CHT techniques and introduced edge orientation (Reference Kimme, Ballard and SklanskyKimme, Ballard & Sklansky 1975), phase coding (Reference Atherton and KerbysonAtherton & Kerbyson 1993) and a Hough transform filter (Reference Kerbyson and AthertonKerbyson 1995). The resulting phase-coded CHT (PCCHT) was adopted in the present study to estimate the locations and radii of the circular bubbles. In this study, a PCCHT, introducing phase coding and a Hough transform filter (Reference Atherton and KerbysonAtherton & Kerbyson 1999), has been used to detect optimal coordinates and radii for all circular bubbles on the images (Appendix A). Since accurate sizes of very small bubbles with radii unresolved by at lease three pixels were unable to be estimated in this method, sufficiently resolved bubbles with diameters larger than 0.75 mm were used in this analysis.

Using the consecutive bubble locations and sizes, we tracked individual bubbles while the bubble velocity was updated on sequential images, which allowed the estimation of each bubble's lifetime (figure 5). The specific tracking procedure is given in Appendix B.

Figure 5. Example of the estimated bubble velocity (a) and horizontal distributions of the mean horizontal bubble velocity (b) and its standard deviation (c). Dotted and solid lines indicate experiments S1 and S2.

Figure 5(b) shows the horizontal distributions of the mean horizontal bubble velocity in both experiments. We found that surface bubbles in experiment S1 had a stationary feature. Accordingly, while we observed progressive behaviours of young bubbles just emerging on the surface near the source region ($x <2$ cm), the horizontal velocity rapidly became attenuated and the bubbles drifted very slowly; this feature was particularly evident in surfactant bubbles (supplementary movie 1 available at https://doi.org/10.1017/flo.2024.19). In experiment S2, the ascending bubble plume caused by submerged air ejection led to induction of divergent bubble flow on the surface; therefore, the surface bubbles were rapidly transported from the source region outward (supplementary movie 1). The bubble velocity decreased during movement in the divergent flow; thus, younger bubbles with higher velocity at locations closer to the source were able to catch up and collide with preceding older bubbles. These differences in bubble behaviour between experiments resulted in distinct features during coalescence, clustering and bursting, which are discussed in the following sections. When coalescence occurred, the centre location of the coalesced bubble might simultaneously move, while the other adjacent bubbles also rapidly changed their positions (supplementary movie 1). The fluctuations in bubble motion were reflected as standard deviations of local bubble velocity, $\sigma _{u_b}$ (figure 5c). The standard deviations gradually decreased with distance $x$ in both experiments as the frequency of coalescence horizontally attenuates (as discussed in § 5).

3. Behaviours of surface bubbles

3.1 Evolution of bubbles generated by water sheet entry

Figure 6 shows backlit images of non-surfactant bubbles during the coalescence process observed in experiment S1 (supplementary movie 1). Surface bubbles, emerged on the still surface near the source region, formed polydisperse clusters primarily composed of large aggregated bubbles surrounded by smaller satellite bubbles (figure 6a); large bubbles after steep meniscus surfaces tend to attract smaller neighbouring bubbles (figure 2c). We also observed successive coalescence after the production of capillary waves from neck extensions that travelled on the cap films (arrows, figures 6 and 2d), which is similar to the coalescence observed in stationary pair bubbles generated by gas injection (Reference Shaw and DeikeShaw & Deike 2021). However, in the aggregated bubble system, when coalescence-induced waves travelling on the film arrive the cap edge, they disturb and rupture the films in contact with adjacent bubbles (figure 6b). These events generated new capillary waves along the neighbouring bubble cap, which then destabilized the films upon arrival. Thus, through successive coalescence, the initial polydisperse bubble cluster (figure 6a) evolved into bidisperse clusters composed of the ballooning primary bubble surrounded by small satellite bubbles (figure 6c). The growing caps of primary bubbles finally ruptured in a process similar to the bursting of an isolated stationary bubble observed by Reference Lhuissier and VillermauxLhuissier & Villermaux (2011). Specifically, a hole in the film bounded by the circular rim was rapidly retracted on the cap film (figure 2b and arrow, figure 7a), resulting in the formation of an unstable rim with ‘fingers’ at regular intervals along the rim axis (figure 7b).

Figure 6. Backlit images of bubble clusters during the coalescing process at $C=0$ in experiment S1 for (a) $t=t_0$, (b) $t=t_0+\Delta t$ and (c) $t=t_0+2\Delta t$, where $\Delta t=8$ ms. Arrows indicate neck expansion of coalescing bubbles.

Figure 7. Backlit images of bubble clusters during the bursting process at $C=0$ in experiment S1 for (a) $t=t_0$, (b) $t=t_0+\Delta t$ and (c) $t=t_0+2\Delta t$, where $\Delta t= 4$ ms. Arrow indicates the boundary of the cap film.

Figure 8 shows typical surfactant bubbles observed at $C= 400\,{\mathrm {\mu }}$g l$^{-1}$ in experiment S1. Since the surfactant prevented coalescence as the inter-bubble force was reduced by the Marangoni effect (§ 4), the emerged polydisperse bulk bubbles remained on the still surface, resulting in the formation of a dense polydisperse bubble raft that covered a large area of the stagnant surface. The bubbles gradually grew through intermittent coalescence to adjacent ones in the rafts until they burst. We also observed that a single bubble burst in the rafts triggered successive bursting of neighbouring bubbles, which might be also caused by capillary waves, generated by the initial bursting, rapidly propagated to the surrounding bubbles and ruptured their cap films (see arrows in figure 8). Figure 9 shows the spatial distributions of the mean bubble population per unit area, $N (d, x)$, as a function of the bubble diameter in experiment S1. The maximal $N$ in $d<2$ mm extended over the $x$ axis in any cases of $C$, indicating small bubbles uniformly distributed in the whole measurement domain. In the non-surfactant case (figure 9a), there was also a broad size distribution of $N$ in $2\,{\rm mm}< d<10\,{\rm mm}$, indicating bubble growth through successive coalescence over the wide size range (figure 6). As $C$ increased, coalescence was inhibited, thereby reducing the maximum bubble diameter and narrowing the size distribution (figure 9b,c). Because the polydisperse bubble raft covered the most surface at $C = 400$ and $800\,{\mathrm {\mu }}$g l$^{-1}$ (figure 8), the size distributions became horizontally uniform.

Figure 8. Backlit images of bubble clusters at $C= 400\,{\mathrm {\mu }}$g l$^{-1}$ in experiment S1 for (a) $t=t_0$, (b) $t=t_0+\Delta t$ and (c) $t=t_0+2\Delta t$, where $\Delta t=4$ ms. Arrow indicates locations of bubbles that successively burst.

Figure 9. Horizontal variations of bubble size distributions in experiment S1.

3.2 Evolution of bubbles generated by air injection on a porous plate

Figure 10 shows non-surfactant bubble clusters evolving through coalescence in experiment S2. As explained in § 2.3, surface bubbles travel horizontally in the divergent bubble flow (figure 5b). When younger bubbles with higher velocity approached older preceding bubbles, because of attraction on the bubble-induced meniscus surfaces, they were rapidly attracted to each other, leading to collision (see also supplementary movie 1). Thus, bubble sizes increased during travel via consecutive coalescence events after collisions through bubble attraction. For example, the original bubbles, A–E in figure 10(a), repeatedly collided and coalesced with approaching younger bubbles, resulting in rapid growth of the primary bubbles in figure 10(be).

Figure 10. Backlit images of bubble clusters in the process of coalescing and bursting at $C= 0$ in experiment S2 for (a) $t=t_0$, (b) $t=t_0+32\Delta t$, (c) $t=t_0+50\Delta t$, (d) $t=t_0+91\Delta t$ and (e) $t=t_0+108\Delta t$, where $\Delta t= 4$ ms. Red letters (A–F) indicate original bubbles before coalescence, for reference.

At a surfactant concentration of $C= 400\,{\mathrm {\mu }}$g l$^{-1}$ in experiment S2 (figure 11), the surfactant suppressed coalescence, which reduced the frequency of collision-induced coalescence events, thereby inhibiting bubble growth through this process. Instead, colliding younger bubbles contacted older bubbles to form patch-like clusters that were transported downstream. These clusters were then disassembled through successive bursting of the component bubbles (arrows, figure 11df).

Figure 11. Backlit images of bubble clusters during the processes of coalescence and aggregation and bursting at $C= 400\,{\mathrm {\mu }}$g l$^{-1}$ in experiment S2 for (a) $t=t_0$, (b) $t=t_0+45\Delta t$, (c) $t=t_0+122\Delta t$, (d) $t=t_0+241\Delta t$, (e) $t=t_0+252\Delta t$ and (f) $t=t_0+289\Delta t$, where $\Delta t= 4$ ms. Arrows in (ac) indicate coalescing bubbles, whereas arrows in (df) indicate past sites of vanished bubbles.

The size growth of the travelling non-surfactant bubbles in the collision–coalescence process was identified over a wide size range of $3\,{\rm mm} < d<8\,{\rm mm}$ (see the region surrounded by the dashed curve in figure 12a). With an increase of the surfactant concentration, as the frequency of coalescence decreases, the maximum size achieved through coalescence was reduced (figure 12b,c). We also found that any sizes of bubbles dissipated and vanished within a certain travel distance (see vertical lines in figure 12), unlike uniform distributions in surfactant bubble rafts observed in experiment S1 (figure 9).

Figure 12. Horizontal variations of bubble size distributions in experiment S2. Bubble size growth owing to coalescence during horizontal travel is indicated in the area surrounded by a dashed curve. A vertical line indicates a critical travel distance at which most bubbles have vanished.

3.3 Mobility effect

The dynamic behaviours of the observed bubbles differed between experiments S1 and S2; quasi-stationary bubbles formed clusters and rafts covering the surface in experiment S1, whereas travelling bubbles coalesced and burst through collisions in experiment S2. To understand the effects of bubble mobility on bursting processes, we performed additional experiments to visualize the surface liquid on bubble caps in experiment S2. Immiscible dry powders (DIAION HP20SS; mean diameter, $100\,{\mathrm {\mu }}$m) were sprinkled on the surface as tracers of surface liquid on the caps of travelling bubbles (figure 13). We observed that the particles floating on the still surface near the travelling bubbles moved over the cap film (arrows, figures 13 and 14a); that is, the liquid in the cap film of the moving bubble was replaced with liquid from the downstream surface. Since the film is steadily renewed before undergoing drainage, film thinning, causing a bubble to burst, may be inhibited. However, if a bubble moves towards the disturbed surface, as the disturbances are transported to the cap through the liquid replacement, the disturbed film may become unstable to be ruptured (figure 14b). The observed successive bursting of bubbles travelling in aggregate, as shown in figure 11(df), may be triggered by this process; specifically, surface disturbance caused by the bursting of one preceding bubble in the aggregation is transported to the cap of the adjacent bubble, causing that bubble to burst. This repeated process eventually leads to overall collapse of the entire aggregation (figure 11f). Further investigations are required to identify details of the mechanisms, including relative acceleration of fluid on the film and dependencies on surfactants.

Figure 13. Successive backlit images demonstrating that floating particles (arrows) passed over the cap films of bubbles travelling from left to right. The time interval of the images in (ac) was $\Delta t= 4$ ms.

Figure 14. Schematic illustrations of the top (a) and side (b) views of a surface bubble moving from left to right. (a) Particles floating on the cap surface translating in the opposite direction to the bubble movement. (b) Film liquid on a moving bubble is replaced by liquid from the downstream surface. After a disturbance on the surface, the cap film liquid is replaced with disturbed surface liquid during bubble travel, leading to rupture of the film.

4. Film thinning

When two bubbles approach each other, the fluid between them is displaced and drained in radial flow normal to the approach direction (figure 15a). Coalescence can occur when the fluid layer between them becomes thinner through drainage than the critical value where rupture takes place (Reference Chesters and HofmanChesters & Hofman 1982). For submerged bubbles, coalescence has been modelled by the relative contact time during collision to the film drainage time (Reference Prince and BlanchPrince & Blanch 1990; Reference ChestersChesters 1991; Reference Sungkorn, Derksen and KhinastSungkorn, Derksen & Khinast 2011).

Figure 15. (a) A circular disk-shaped film on the bubble wall of two colliding surface bubbles. (b) Thinning rates of the film thickness, $h/h_0$, estimated by (4.5) (blue), (4.6) (red) and (4.7) (black) at $h_0=100\,{\mathrm {\mu }}$m and $C=0$: — ($R=1.0$ mm), - - - ($R=2.0$ mm), $\cdots$ ($R=3.0$ mm), – $\cdot$ – ($R=4.0$ mm).

The drainage process has often been explained by the Stefan–Reynolds flat-film model (Reference FriedlanderFriedlander 2000; Reference Chan, Klaseboer and ManicaChan et al. 2011), assuming the thinning-film form of a circular flat disk with radius $a$ (figure 15b). Considering axisymmetric viscous flow in the disk film of thickness $h$ between approaching bubble walls under external force $F$, the solution of the Stokes flow with lubrication approximation, integrated over the disk, is given by

(4.1)\begin{equation} \frac{{\rm d} h}{{\rm d} t} = {-}\frac{2}{3{\rm \pi}}\frac{h^3}{a^4 \rho \nu}F, \end{equation}

where $\rho$ is the density of liquid and $\nu$ is the kinematic viscosity.

As explained in § 3, aggregations of surface bubbles were caused by the apparent attraction which is a tangential component of buoyancy on the meniscus surface slopes formed around the adjacent bubbles (see also figure 2 and supplementary movie 1). When we consider a circular disk-shaped film between the bubble walls of two colliding bubbles of identical radius $R$ (figure 15a), neglecting Hamaker forces, the force acting on two colliding surface bubbles (Reference NicolsonNicolson 1949) is given by

(4.2)\begin{equation} F = {\rm \pi}R \gamma q, \end{equation}

where

(4.3)\begin{equation} q = \frac{\beta^3}{\sqrt{4-\beta^2}}\frac{K_1(2\alpha\sqrt{1-a^2/R^2})}{K_1(\alpha \beta)}-2 \frac{a^2}{R^2}-M(C, a), \end{equation}

where the Morton number $\alpha =R\sqrt {\rho g/\gamma }$ and $M(C, a )$ is the Marangoni force describing surfactant effects on drainage in a film ($M$=0 for non-surfactant bubbles) (Reference LangevinLangevin 2019). Reference Radoëv, Dimitrov and IvanovRadoëv, Dimitrov & Ivanov (1974) solved the Reynolds flat-film model including effects of surfactant concentration and found the Marangoni effect reduced drainage to decelerate the film thinning. In the current work, for simplicity, $M$ was dealt with as an undetermined constant, assuming slower temporal variation of $M$ than the thinning velocity. The first and second terms of the right-hand side of (4.3) indicate contributions of the attraction force and the excess pressure, respectively. The radius of a circular edge of a bubble cap relative to the bubble radius, $\beta =b/R$ (figure 15a), is determined by the mechanical balance between the buoyancy and static pressure on the meniscus:

(4.4)\begin{equation} \beta^2-\frac{2}{3}\alpha^2\left(1 + \sqrt{(1-\beta^2)(1 + \beta^2/2)}-\frac{3}{2} \frac{\beta^3}{\alpha\sqrt{4-\beta^2}}\frac{K_0(\alpha \beta)}{K_1(\alpha\beta)}\right) = 0, \end{equation}

where $K_0$ and $K_1$are the modified Bessel functions of the second kind of order zero and one, respectively. Assuming the thinning velocity is much faster than the moving velocity of bubbles (i.e. constant $F$) and integrating (4.1) with (4.2), the thickness of the thinning film between the attracted bubbles is given by

(4.5) \begin{equation} h = \left(\frac{4}{3}\frac{\gamma R q}{\rho \nu a^4}t + \frac{1}{h_0^2}\right)^{{-}1/2}. \end{equation}

For colliding bubbles in bulk liquid, the bubble contact time relative to the film drainage time has modelled the occurrence of coalescence (Reference Prince and BlanchPrince & Blanch 1990; Reference Sungkorn, Derksen and KhinastSungkorn et al. 2011). Once surface bubbles collide, they never detach as the attraction force keeps acting on them (figures 6, 8, 10 and 11). The contact time thus cannot be a parameter modelling the coalescence rate for surface bubbles. From (4.5), it may be appropriate to use the characteristic drainage time $\tau _c\sim \rho \nu a^4/\gamma R q h_0^2$ as a measure of the time of commencing film rupture leading to coalescence. The film thinning becomes slower (with longer $\tau _c$) as $q$ is reduced by the Marangoni effect (equation (4.3)).

Next we consider drainage in a bubble-cap film. Following Reference Couder, Fort, Gautier and BoudaoudCouder et al. (2005), and Reference Lhuissier and VillermauxLhuissier & Villermaux (2011), considering the viscous flow in a curved thin film of the bubble cap, subjected to gravity, the thickness of the thinning film during gravity drainage can be given as a similarity solution for the lubrication equation system of Poiseuille flow:

(4.6)\begin{equation} h = G(\theta) \left(\frac{g}{3\nu R}t + \frac{1}{h_0^2}\right)^{{-}1/2}, \end{equation}

where $G(\theta )=(4/(3 \sin4/3\,\theta)\int _0 ^\theta \sin ^{1/3}\phi \,{\rm d}\phi )^{1/2}$ and $\theta$ is the polar angle. Here $G(\theta )$ is almost uniform between $G(0)=1$ and $G({\rm \pi} /2)\approx 0.76$. The characteristic time $\tau _b\sim \nu R/g h_0^2$ may be used for the reference time required for film rupture resulting in bursting of an isolated surface bubble (without coalescing process). Reference Lhuissier and VillermauxLhuissier & Villermaux (2011) considered capillary effects on drainage velocity and suggested another thinning law:

(4.7) \begin{equation} h\sim \rho g^{1/3} R^{7/3} \gamma^{{-}1} \left(\frac{\nu}{t}\right)^{2/3}. \end{equation}

Figure 15(b) shows the temporal variations of film thickness given by (4.5), (4.6) and (4.7) at $C=0$. Initial thickness ($h_0$) of $100\,{\mathrm {\mu }}$m was assumed for all cases (Reference Sungkorn, Derksen and KhinastSungkorn et al. 2011). Constant $G=1$ was used for (4.6). Equation (4.5) was solved for the bubbles placed 0.1 % closer to the contact central distance ($2R$); i.e. $a=0.0316R$. Because of active drainage in the bubble-wall film between attracted bubbles, the film thickness, described by (4.5), decreased with much faster velocity than that of a cap film owing to natural gravity drainage, (4.6) and (4.7), indicating that rupture of the bubble-wall film, leading to coalescence, occurred earlier than bursting through slower thinning of the cap film (see figures 6, 10 and 11 and also supplementary movie 1). In surfactant cases, as drainage velocity was decreased by the Marangoni force, resulting from surfactant gradients over the bubble-wall film (as $M > 0$ in (4.3), the inter-bubble force $F$ in (4.2) decreased), the film thinning decelerated, resulting in inhibition of coalescence (see figure 12c). When a raft of surfactant bubbles was formed (figures 8 and 9b,c), as omnidirectional attraction forces worked each other from all contacting bubbles, further reduction of the total inter-bubble force resulted in slower drainage, causing further reduction of the frequency of coalescence.

5. Population through bubble burst and coalescence

In this section, we statistically characterize variations in the bubble population through bubble burst and coalescence following the mechanisms discussed in § 4. The volume of air in bubbles is conserved during coalescence. When the number density of bubbles is discretized in terms of volume classes $v_i\ (i=1, 2, \ldots )$, assuming binary coalescence of monodisperse bubbles in the volume class $v_1$, added volumes of coalesced bubbles are given as $v_2 = 2v_1$, $v_3=v_1+v_2=3v_1$, $v_4=v_1+v_3=2v_2=4v_1$, $v_5=v_1+v_4=v_2+v_3=5v_1$, and so on. Accordingly, the coalesced bubble volumes are simply described by multiples of the initial volume, $v_1$. Reference Néel and DeikeNéel & Deike (2021) found the bubble number density exhibited harmonic variations achieving the maximal peaks at multiples of the mean volume of bulk bubbles through bubble coalescence events in non-surfactant bubble rafts.

Figure 16 shows the bubble density per 0.1 mm$^3$ increment per unit area as a function of the spherical bubble volume. We found oscillatory features of the bubble densities with respect to the bubble volume in any surfactant scenarios. In the non-surfactant experiment S2, because of the inter-bubble attraction force (4.2), bubbles successively collided with each other, leading to successive coalescence owing to rapid film thinning in an early phase of the bubble travel (see also figures 10 and 12 $a$), which resulted in harmonic volume variations at $x= 20$ mm (figure 16a-ii). The harmonic peaks with intervals of 3–4 mm$^3$ correspond to the volume of a spherical bubble in $1.8\,{\rm mm}< d<2.0$ mm, approximately corresponding to the mean diameter of bulk bubbles (§ 2.2). For moderate concentration of $C=400\,{\mathrm {\mu }}$g l$^{-1}$, the harmonic signatures were observed at $x=40$ mm (figure 16b-ii), indicating that coalescence occurred in a later phase than in the non-surfactant case, since the Marangoni force $M$ in (4.3) reduced the total inter-bubble force of (4.2) and decelerated the film thinning. Further reduction of $F$ at the highest surfactant concentration $C=800\,{\mathrm {\mu }}$g l$^{-1}$ significantly suppressed the volume transition through coalescence (figure 16c-ii). In all cases, the bubble densities over volume significantly decreased with distance $x$ (see also figure 12) owing to successive bursting of travelling bubbles (§ 3.3).

Figure 16. Size distribution plots as a function of the bubble volume in experiment S1 (a-i,b-i,c-i) and S2 (a-ii,b-ii,c-ii) for (a-i,a-ii) $C=0\,{\mathrm {\mu }}$g l$^{-1}$, (b-i,b-ii) $400\,{\mathrm {\mu }}$g l$^{-1}$ and (c-i,c-ii) $800\,{\mathrm {\mu }}$g l$^{-1}$.

In experiment S1, since coalescence was significantly inhibited in a raft structure, as explained in § 4, uniform density with minor variations increased over volume without distinct harmonic peaks, indicating that polydisperse coalescence governed in these cases.

6. Frequencies of coalescence and bursting

A Boltzmann-type transport equation has been used to describe the evolution of population of bulk bubbles (Reference Carrica, Drew, Bonetto and LaheyCarrica et al. 1999; Reference Martínez-Bazán, Montañés and LasherasMartínez-Bazán, Montañés & Lasheras 1999; Reference Marchisio and FoxMarchisio & Fox 2013; Reference Ruiz-Rus, Ern, Roig and Martínez-BazánRuiz-Rus et al. 2022):

(6.1)\begin{equation} \frac{\partial n}{\partial t} + \boldsymbol{\nabla}\boldsymbol{\cdot}(n \overline{\boldsymbol{u}}) + \frac{\partial \phi n}{\partial v} = {S}, \end{equation}

where $n (v, {\boldsymbol{x}},t)$ is the number density of bubbles with volume $v$ at location ${x}$ and time $t$, $\overline{\boldsymbol{u}} (v, {\boldsymbol{x}}, t)$ is the mean horizontal velocity of bubbles of volume $v$, $\phi$ is the rate of change of the volume $v$ of a bubble due to thermal effects (condensation, evaporation and dissolution) and ${S}(v, {\boldsymbol{x}},t)$ is the source term.

When taking into account production source, coalescence and bursting, assuming one-dimensional bubble flow and ignoring thermal effects, (6.1) is reduced as

(6.2) \begin{equation} \frac{\partial n}{\partial t} + \frac{\partial}{\partial x} n \bar{u} = {Q_{c}} + {Q_m} + {Q_b} + {S_p} , \end{equation}

where ${Q_{c}} (v, {x},t)$ and ${Q_{m}}(v, {x},t)$ are the birth and death rates of bubbles due to coalescence, respectively, ${Q_b}(v, {x},t)$ is the death rate of bubbles due to bursting and ${S_p}(v, {x},t)$ indicates the source associated with bubble emergence on a surface. We may also define frequencies of coalescence, $q_m (v)$, and bursting, $q_b (v)$, by $Q_m=q_m n$ and $Q_b=q_b n$, respectively (Reference Ruiz-Rus, Ern, Roig and Martínez-BazánRuiz-Rus et al. 2022). Rates $Q_c$, $Q_m$ and $Q_b$ can be directly estimated in the current temporal analysis through bubble tracking on the basis of sequential locations and sizes throughout lifetimes of individual bubbles (Appendix B).

Figure 17 shows $Q_c$, $Q_m$ and $Q_b$ and their sum $Q_s=Q_c+Q_m+Q_b$ against the bubble volume at three different locations $x= 20$, 40 and 60 mm. As the source of bubbles is sufficiently away in $x\ge 20$ mm (i.e. $S_p \approx 0$), ignoring the first term of the left-hand side of (6.2) at a steady state, the total sink $Q_s$ balances with the bubble density transported from upstream $\partial n\bar {u}/\partial x$. In the non-surfactant case of experiment S1, the relative death rate due to bursting with respect to the total sink, $Q_b/ Q_s$, took values in 0.13–0.28; that is, the major cause of depopulation in this case was not bursting but coalescence. While the coalescence rates decreased by reduction of the inter-bubble force in the rafts (§ 4), the observed intermittent bursts, induced by cap-film thinning, triggered successive bursting of surrounding bubbles (figure 8). Rate $Q_b$ thus relatively increased in the rafts: $Q_b/Q_s\sim 0.72$–0.80 ($x=40$ mm), $Q_b/Q_s>0.95$ ($x=60$ mm) for $C=400\,{\mathrm {\mu }}$g l$^{-1}$; and $Q_b/Q_s>0.87$ ($x=40$ mm), $Q_b/Q_s>0.80$ ($x=60$ mm) for $C=800\,{\mathrm {\mu }}$g l$^{-1}$. Therefore the bursting process is more important for predicting the total bubble loss in the surfactant scenarios. In experiment S2, the rates of bubble loss due to both coalescence and bursting increased more than ten times compared with those observed in S1, especially in the small-volume range $v<5$ mm$^3$, causing significant depopulation during horizontal travel of bubbles (see also figure 16). Rate $Q_m$ took the largest negative values in an early stage of bubble travel ($x=20$ mm) for any surfactant concentration, which decreased with surfactant concentration as the inter-bubble force decreased by the Marangoni effect. In contrast, frequencies of bursting, $Q_b$, increased at any locations with surfactant concentration (e.g. maximum $Q_b/Q_s< 0.1$ for $C=0$, while $Q_b/Q_s$ exceeds 0.95 for $C=800\,{\mathrm {\mu }}$g l$^{-1}$). According to Reference Shaw and DeikeShaw & Deike (2021), when two expanding surface bubbles coalesce, the liquid from the meniscus between the parent bubble caps is brought up in a bulge on the top surface of the film and eventually spreads out over the newly formed bubble cap, suggesting that the liquid mass in the bulge on the new cap recovers the thickness of the cap film. In this case, the cap film thinning might be suppressed through successive coalescence, which possibly resulted in the observed opposite trends of frequencies of bubble bursts and coalescence with respect to surfactant concentration. Further research on changes in film thickness through coalescence is necessary for validation.

Figure 17. Rates of birth $Q_c$ and death $Q_m$ of bubbles due to coalescence and rate of bursting $Q_b$ as a function of the bubble volume in experiment S1 (a-i,b-i,c-i) and S2 (a-ii,b-ii,c-ii) for (a-i,a-ii) $C= 0\,{\mathrm {\mu }}g$ l$^{-1}$, (b-i,b-ii) $400\,{\mathrm {\mu }}g$ l$^{-1}$ and (c-i,c-ii) $800\,{\mathrm {\mu }}$g l$^{-1}$.

Reference Néel and DeikeNéel & Deike (2021) assumed the exponential decay of a raft composed of $\hat {n}$ surfactant bubbles:

(6.3)\begin{equation} \hat{n} = \hat{n_0} \exp({-t/\hat{\tau_r}}), \end{equation}

where $\hat {n_0}$ is the initial bubble population in a raft and $\hat {\tau _r}$ is the raft decay time. The rates of coalescence ($\hat {Q_m}$) and bursting ($\hat {Q_b}$) were defined in terms of the global frequencies of coalescence, $\hat {q_m}$, and bursting, $\hat {q_b}$, by

(6.4a,b)\begin{equation} {\hat{Q_m}} = \hat{q_m} \hat{n},\quad {\hat{Q_b}} = \hat{q_b}\hat{n}. \end{equation}

The exponential decay time was then approximated as

(6.5)\begin{equation} \frac{1}{\hat{\tau_r}}\equiv\hat{q_r} = \hat{q_m} + \hat{q_b}, \end{equation}

where $\hat {q_r}$ is the global frequency of total raft decay. It should be noted that $\hat {q_m}$ and $\hat {q_b}$ are constant in each raft, regardless of bubble size. Therefore, the raft decay time $\hat {\tau _r}$ does not coincide with lifetimes of individual bubbles from birth to death. In this study, mean frequencies of coalescence and bursting over the size and space domains, which may be comparable to $\hat {q_m}$ and $\hat {q_b}$, are defined in terms of the measured $Q_m$ and $Q_b$:

(6.6a,b)\begin{equation} \left.\begin{gathered} \tilde{q_m} = \frac{\displaystyle\int_0^\infty\int_0^{\infty}n q_m \,{\rm d} v\,{\rm d} x}{\displaystyle\int_0^\infty \int_0^{\infty}n \,{\rm d} v\,{\rm d} x} = \frac{\displaystyle\int_0^\infty\int_0^{\infty}Q_m \,{\rm d} v\,{\rm d} x}{\displaystyle \int_0^\infty\int_0^{\infty}n \,{\rm d} v\,{\rm d} x},\\ \tilde{q_b} = \frac{\displaystyle\int_0^\infty\int_0^{\infty}n q_b \,{\rm d} v\,{\rm d} x}{\displaystyle \int_0^\infty\int_0^{\infty}n \,{\rm d} v\,{\rm d} x} = \frac{\displaystyle\int_0^\infty \int_0^{\infty}Q_b \,{\rm d} v\,{\rm d} x}{\displaystyle\int_0^\infty\int_0^{\infty}n \,{\rm d} v\,{\rm d} x}. \end{gathered}\right\} \end{equation}

The corresponding decay time is thus given by following (6.5):

(6.7)\begin{equation} \frac{1}{\tilde{\tau_r}}\equiv\tilde{q_r} = \tilde{q_m} + \tilde{q_b}.\end{equation}

Figure 18 compares the estimated $\tilde {q_m}$, $\tilde {q_b}$, $\tilde {q_r}$ and $\tilde {\tau _r}$ with $\hat {q_m}$, $\hat {q_b}$, $\hat {q_r}$ and $\hat {\tau _r}$ given in Reference Néel and DeikeNéel & Deike (2021). While all the frequencies, $\tilde {q_m}$, $\tilde {q_b}$ and $\tilde {q_r}$, in experiment S1 were smaller than those in S2, overall features of decreasing $\tilde {q_m}$ and unchanging $\tilde {q_b}$ with increasing $C$ were consistent with those of Néel and Deike. We note that there is an analogy of stationary feature of the surface bubbles observed in the current experiment S1 and the previous one by Néel and Deike. The current mean decay time $\tilde {\tau _r}$ for experiment S1 was also comparable to $\hat {\tau _r}$, suggesting that an analogous mechanism (through thinning cap film due to drainage) might trigger the bursting process for stationary bubbles in both the experiments. Time $\tilde {\tau _r}$ of experiment S2, where different organizations of bubble aggregations were observed, indicates shorter decay time than that reported by Néel and Deike. It should be noted that characteristic time scales for coalescence and bursting (§ 4), governed by cap-film thinning due to local inter-bubble forces and Marangoni effects in rafts, highly depend on bubble sizes, as observed in figure 17, which cannot be described by the macroscopic decay time (6.7). Statistical properties of the size-dependent bubble life are discussed in the next section.

Figure 18. Current estimates of mean frequencies of coalescence and bursting, defined by (6.6a,b), and global decay time, (6.7), compared with the previous ones, (6.5), by Reference Néel and DeikeNéel & Deike (2021) (ND): (a) frequencies in experiment S1, (b) frequencies in experiment S2 and (c) decay time.

7. Lagrangian bubble lifetime

In this section, we discuss the Lagrangian lifetimes of individual bubbles, which are measured by bubble tracking (Appendix B). Figure 19 shows scatter plots of the measured bubble lifetime, $T_l$, against the bubble diameter at bursting, $d_b$. As we consider here lifetimes of bursting bubbles owing to ruptures of cap films, the lifetimes ended by coalescence are excluded in the analysis. We found that $T_l$ has weak correlations with $d_b$ in both the experiments. As discussed in § 4, the cap-film thinning through gravity drainage is characterized by the time $\tau _b$ that is proportional to the bubble size. Therefore, a linear relationship between $T_l$ and $d_b$ was assumed and fitted to the lifetime plots by the method of least squares (see lines in figure 19). The optimal rates of the regression slopes and the root-mean-square deviations are given in table 1. In experiment S1, we observed dispersion of $T_l$ with respect to $d_b$, which might result from successive bursts, as observed in figure 8, vanishing adjacent bubbles with arbitrary sizes. In experiment S2, we found better approximations of the lifetimes by linear regression with less deviations than those in experiment S1. Long-life bubbles ($T_l >1.0$ s) grown through coalescence ($d_b>4$ mm) were also observed for moderate surfactant concentration (200 and $400\,{\mathrm {\mu }}$g l$^{-1}$), which may be interpreted in terms of inhibition of bubble-cap thinning owing to film renewal through coalescence, as discussed in the previous section. Since the frequency of coalescence decreased by the predominant Marangoni effect in the highest concentration, both the lifetime and bursting diameter significantly decreased.

Figure 19. Scatter plots of bubble lifetime $T_l$ as a function of the diameter of the bursting bubble $d_b$ in experiments S1 (a) and S2 (b).

Table 1. Optimal proportional constants fitted with a linear equation of $d_b$ and the root-mean-square deviation from the linear approximation.

The size-dependent bubble lifetimes, shown in figure 19, indicate that coalescence, causing bubble growth, significantly affects the bursting process ending the lives of individual bubbles, which depends on local inter-bubble forces, organization of clusters and rafts and bubble mobility. In terms of prediction of total bubble attenuation via these local processes, it is also important to understand probabilistic features of the lifetime distributions. We consider here probabilities of ($a$) bubble lifetimes ended only by bursting and ($b$) lifetimes ended by bursting or coalescence.

The Weibull distribution was previously used to describe lifetime probability for an isolated stationary bubble by Reference Lhuissier and VillermauxLhuissier & Villermaux (2011):

(7.1)\begin{equation} f(T_l) = \frac{m}{\tau_0}\left(\frac{T_l}{\tau_0}\right)^{m-1}\exp({-(T_l/\tau_0)^m}), \end{equation}

where $\tau _0$ is the characteristic time and $m$ is the scale parameter. It is known that (7.1) can describe characteristics of different types of distributions with the value of $m$; i.e. an exponential distribution with $m=1$ and a Rayleigh distribution with $m=2$. Reference Zheng, Klemas and HsuZheng, Klemas & Hsu (1983) proposed a Rayleigh distribution of lifetimes of stationary surface bubbles generated by air injection through a capillary tube. Reference Lhuissier and VillermauxLhuissier & Villermaux (2011) suggested $m=4/3$ through reanalysis of the experimental results by Reference Zheng, Klemas and HsuZheng et al. (1983). While the previous studies used the Weibull lifetime probability for an isolated stationary bubble, the effects of bubble aggregation and mobility on the bubble lifetimes were examined through comparisons with optimal Weibull parameters of the measured bubble lifetimes estimated by fitting the distribution (7.1).

Figure 20 shows the Weibull distributions fitted to the experimental bubble lifetimes ended by bursting. The lifetime distributions in experiment S1 have a longer tail than those in S2 for any surfactant concentration, which may be interpreted by shorter bubble lives ended by cascade bursts of travelling bubbles observed in S2 (§ 3.3). As discussed in § 6, a possible mechanism of cap-film recovery through intermittent coalescence, reducing the frequency of bursting for moderate surfactant concentration, may result in a slightly wider distribution at $C = 400\,{\mathrm {\mu }}$g l$^{-1}$ in experiment S2. The optimal parameters $\tau _0$ and $m$ for the cases of both (a) bubble loss by bursting and (b) total bubble loss are specifically given in table 2. The characteristic time $\tau _0$ in any cases of experiment S1 were larger than those in S2, which was consistent with the relative values of macroscopic decay time $\tilde {\tau _r}$ (figure 18). The values of $\tau _0$ for (b) were smaller than those for (a) in all cases, suggesting that frequent coalescence of short-life bubbles predominated the total bubble loss. We also found the shape parameter $m$ took values close to 1 in (b), indicating that an exponential distribution well approximated the probabilistic lifetimes of total bubble loss. We note that the linear relation of the lifetime and bursting diameter, $T_l\propto d_b$, observed in figure 19, may be able to specify the probability of occurrence of the bursting diameter, as well as the bursting frequency against the bubble volume (figure 17).

Figure 20. Probability densities of bubble lifetimes in experiments S1 (a) and S2 (b). Solid lines indicate Weibull distributions (7.1), with optimal parameters given in table 1.

Table 2. Parameters of a Weibull distribution, and reliable lifetimes.

The Weibull reliable life for a specified reliability $L$ is defined by

(7.2)\begin{equation} \tau_L = \tau_0(-\ln(L))^{1/m}.\end{equation}

If $L=0.5$, (7.2) indicates the median lifetime (half of the bubbles can survive by $\tau _{0.5}$). The estimated $\tau _{0.5}$ and $\tau _{0.1}$ are provided in table 2. Considering mesotrophic seawater, corresponding to $C = 400\,{\mathrm {\mu }}$g l$^{-1}$, both $\tau _{0.5}$ and $\tau _{0.1}$ increase 1.3–1.5 times in (a) and 1.9–2.2 times in (b) compared with non-surfactant cases. Accordingly, surfactant in seawater contributes to suppress the dissipation of bubbles and increase bubble lifetime about twice as long as that for clean water.

The Weibull parameters $\tau _0$ and $m$ should be generalized according to bubble mobility in a future study. The additional effects of turbulence on the parameters should also be determined to predict sea-surface coverage by any surface bubbles that arise from breaking waves.

8. Conclusions

In this study, we experimentally examined the physical properties of clustering, coalescing and bursting surface bubbles generated by water sheet entry (experiment S1) and an air-injected porous plate (experiment S2) based on precise measurements of backlit images. The non-ionic surfactant Triton-X100, which mimics the effects of natural seawater, was used in our experiments to model surfactant enrichment in seawater. The PCCHT method was used to identify the locations and diameters of circular forms representing the surface bubbles, which were then used to quantify the bubble size distributions and track individual bubbles to estimate bubble lifetime.

In the non-surfactant S1 experiment, the largest primary bubble in quasi-stationary, polydisperse surface bubbles attracted and aggregated with nearby smaller bubbles on the meniscus surface, resulting in the formation of bubble clusters where primary bubbles rapidly grew through coalescence with smaller satellite bubbles. The bubble cap of the fully developed primary bubble then ruptured in a process similar to the bursting of a stationary isolated bubble (Reference Lhuissier and VillermauxLhuissier & Villermaux 2011). In this case, as the frequency of coalescence was much higher than the bursting frequency, total bubble loss was governed by the coalescence process. As surfactant concentration increased, coalescence was suppressed by the Marangoni effect preventing film thinning on bubble walls, resulting in the formation of a bubble raft exhibiting polydisperse distribution spread over the liquid surface. Since bubbles in the raft received omnidirectional inter-bubble forces from neighbouring bubbles, the total force is significantly reduced and thus the frequency of coalescence further decreased. The rates of bubble loss due to bursting in the rafts became predominant, since intermittent bursts emitted capillary waves and disturbed surrounding bubbles, causing successive bursting in the rafts.

In experiment S2, bubbles were transported in a divergent bubble flow, where younger bubbles successively approached older bubbles. When the bubbles came close, attraction force acting on them accelerated younger bubbles towards preceding ones, causing collision. As bubble-wall films of collided bubbles rapidly thinned through drainage by inter-bubble attraction, non-surfactant bubbles successively coalesced with colliding bubbles, resulting in the rapid growth of primary bubbles. Since inter-bubble forces of surfactant bubbles were reduced by the Marangoni force, frequencies of coalescence decreased with surfactant concentration, and instead, patch-like bubble clusters were organized. We detected another potential mechanism for the bursting of travelling bubbles, which constituted cap-film liquid renewal with ambient surface liquid. If disturbances occur on ambient surfaces, the cap film of the travelling bubble is replaced with the disturbed surface liquid, which may destabilize the film. This process might cause successive bubble bursting during bubble drift, resulting in significant depopulation with travel distance. The rates of bubble loss due to both coalescence and bursting were recorded as more than ten times higher than those in experiment S1, resulting in shorter bubble lifetimes than in S1.

Finally, we estimated the Lagrangian bubble lifetime via bubble tracking. We found that the lifetimes had linear correlations with the sizes of bursting bubbles in experiment S2, which was supported by a theoretical time scale of cap-film thinning through drainage. The observed successive bursting of surfactant bubbles in rafts in experiment S1 caused dispersion of their lifetimes from the linear regression. Probability densities of the lifetimes ended by surfactant bubble bursting in experiment S1 have longer tails than those in experiment S2, which may indicate uncertainty associated with successive bursting triggered by intermittent bursts in the rafts. The lifetimes ended by both coalescence and bursting were well approximated by an exponential distribution in both the experiments, while optimal scale parameters of the Weibull distribution of the lifetimes ended only by bursting took values similar to those previously estimated by Reference Lhuissier and VillermauxLhuissier & Villermaux (2011) and Reference Zheng, Klemas and HsuZheng et al. (1983). Considering the linear correlation between the lifetime and bursting diameter, the lifetime distributions may provide probabilities of occurrence of bursting diameters, and bursting frequencies against bursting sizes. The analysis of the Weibull reliable life led to the conclusion that surfactants in mesotrophic seawater increase bubble lifetime about twice as long as that for clean water.

Through all the analyses of surface bubbles generated for different experimental set-ups and surfactant concentrations, we found that bubble growth and dissipation highly depend on a distinct coalescence process via modification of inter-bubble forces and distinct bursting process including uncertain successive bursting in rafts as well as cap-film replacement, resulting in different behaviours of submerged bubbles in bulk liquid that have been revealed by many previous studies. The current findings provided fundamental parameters characterizing the evolution of surface bubbles, sensitively modified by mobility and organization of surface bubbles, which will be useful for considering suitable parameters required to understand realistic oceanic bubbles in future studies.

All findings obtained in this study relate to a limited range of bubble size, $d>0.75$ mm. Further analysis for smaller bubbles remains to be performed. We also note that the current experiments modelling plunging jets and bubble plumes in a small tank had inherent flows limited by walls, which are different from what is observed in oceans. Further extensions of research are required for applications to whitecap bubbles.

Supplementary movie is available at https://doi.org/10.1017/flo.2024.19.

Acknowledgements

We gratefully acknowledge the experimental support of T. Nonaka who was a graduate student of Hokkaido University.

Funding statement

This research was supported by a JSPS Grant-in-Aid for Scientific Research (23H00191, 22K04324).

Declaration of interests

The authors declare no conflict of interest.

Author contributions

Y.W. created the research plan, designed experiments, performed experiments and wrote the manuscript. Y.W. and A.S. analysed experimental data.

Data availability statement

Original image data are provided in the supplementary movie.

Ethical standards

The research meets all ethical guidelines, including adherence to the legal requirements of the study country.

Appendix A. Phase-coded circle Hough transform

In CHT, the centre coordinate ($a$, $b$) and radius $r$ of a circle are related to positions along its edge ($x$, $y$), which forms a circle under the constraint $(x-a)^2+(y-b)^2=r^2$. This equation gives the set of parameters ($a$, $b$, $r$) along the circular edge in the ($a$, $b$, $r$) parameter space; thus, only a single location satisfies the constraint over the whole circular edge (figure 21b,c), which defines the location and radius of the circle edge on the image (figure 21d). Multiple improvements have been proposed to detect these inherent locations in the parameter space (e.g. Reference Yuen, Princen, Illingworth and KittlerYuen et al. 1990). Reference Atherton and KerbysonAtherton & Kerbyson (1999) combined previous CHT techniques and introduced edge orientation (Reference Kimme, Ballard and SklanskyKimme et al. 1975), phase coding (Reference Atherton and KerbysonAtherton & Kerbyson 1993) and a Hough transform filter (Reference Kerbyson and AthertonKerbyson 1995). The resulting PCCHT transforms original images (figure 21a) into the parameter space (figure 21b,c), thereby providing optimal coordinates and radii for all circular bubbles on the images (figure 21d). As mentioned in § 2.3, in backlit measurement, as shadows of surface bubbles connect with those of adjacent bubbles in a raft, a boundary of each bubble cannot be defined by common edge detection techniques. Figure 22 compares the bubble edges identified by some common techniques provided by the Image Processing Toolbox of Matlab. We found that both the Sobel and Canny methods provided outer edges enveloping the raft containing bubbles with common shadows of adjacent ones (figure 22b,c). As there were many edges, including inner boundaries surrounded by shadow rings and around the voids among bubbles, it may be difficult to define sizes of individual component bubbles. We found the current technique identifying a circular form of bubble shadows consistently estimates the radii and centre locations of circular bubbles in the rafts (figure 22d).

Figure 21. The PCCHT procedure used to determine the locations and sizes of circular bubbles. (a) Original backlit images of surface bubbles. (b) Number of responses in centre coordinate space. Bubble centres are positioned at coordinates with response peaks. (c) Bubble radii determined using the centre coordinate values shown in (b). (d) Circles indicating the estimated radii and centre coordinates, superimposed on (a).

Figure 22. (a) Original backlit image, (b) edges detected by the Sobel method, (c) edges detected by the Canny method, (d) current estimation of circular edges by the PCCHT method and (e) definition of overlap length.

We detected circular bubbles partially overlapped in a packed raft where bubbles might be squeezed. In this case, the interface between the adjacent bubbles may be located along a line segment connecting the intersections of the circular bubbles (a chord of minor segment of a circle; see figure 22e). We defined an error length as the height of the circular segment of a circular bubble. For instance, as the simplest case, if we consider two overlapping circular bubbles of radius $r_1$ and $r_2$ located with distance $D$ as shown in figure 22(e), the overlap length $\epsilon$ can be estimated as $\epsilon =(r_1+r_2-D)/2$. We estimated the overlap lengths $\epsilon$ over all the detected bubbles to evaluate errors arising from the current measurements. Figure 23 shows the mean overlap length $\epsilon$ and relative overlap length $\epsilon / d$ for all experimental cases. While there were minor variations against surfactant concentration, both maximum errors of 0.003 mm in experiment S1 and 0.006 mm in S2 were negligibly smaller than the minimum pixel width (0.08 mm), indicating that overlapping errors did not affect the current bubble size estimations. The relative overlap lengths took maximum values less than 0.04 % in experiment S1 and 0.1 % in S2, which might give negligible influence on the statistics given in §§ 57.

Figure 23. Mean overlap length $\epsilon$ (solid line) and relative overlap length $\epsilon /d$ (dotted line) in experiment S1 (a) and S2 (b).

As the current analysis assumed two-dimensional distributions of bubbles floating on a liquid surface, when a bubble is slightly displaced downward, a smaller size of the bubble could be recorded on an image. Assuming a pinhole image projection, as the optical distance from the centre of projection to the focal plane at a still water surface was about 30 cm in the current camera system, when a bubble displaced 1 mm downward, the size of the bubble was recorded as 0.997 times smaller than that on the surface. In this case, the error caused by vertical displacement of the mean diameter of bulk bubbles (2 mm) was 0.006 mm, which was negligibly smaller than the minimum pixel width. If we consider an extreme case of a bubble displaced 10 mm downward (although we could not observe such large displacement throughout the experiments governed by the monolayer formation of bubble aggregations), the estimated error of 0.064 mm for the mean diameter of bulk bubbles was still smaller than the minimum pixel width. While we found that vertical displacement did not affect the accuracy of the current analysis, three-dimensional analysis may be required for measuring more complex bubble flows such as bubbles on wavy surfaces.

Appendix B. Bubble tracking

In previous experiments of bubble columns, imaging analyses have been used for measuring bubble velocity (Reference Hassan and CanaanHassan & Canaan 1991; Reference Rodriguez-Rodriguez, Martínez-Bazán and MontañésRodriguez-Rodriguez, Martínez-Bazán & Montañés 2003; Reference Zaruba, Krepper, Prasser and SchleicherZaruba et al. 2005; Reference Zhou and NiuZhou & Niu 2020) and morphological properties (Reference de Langlard, Al-Saddik, Charton, Debayle and Lamadiede Langlard et al. 2018; Reference Laupsien, Le Men, Cockx and LinéLaupsien et al. 2019) of bulk bubbles. Reference Hassan and CanaanHassan & Canaan (1991) applied conventional particle tracking velocimetry to bubbly flows, based on statistical selections of bubble trajectories with the minimum variance of length and angle of travel between successive frames. Reference Rodriguez-Rodriguez, Martínez-Bazán and MontañésRodriguez-Rodriguez et al. (2003) developed a tracking technique introducing the so-called pseudo-distance defined by location and projection area of bubbles. In this method, bubble breakup was defined when multiple daughter bubbles were associated with a mother bubble through forward and backward tracking, and coalescence occurred when multiple mother bubbles were associated with one daughter in the frames adjacent to each other. In addition, a two-dimensional orthogonal projection of bubbles moving in three-dimensional space resulted in bubble overlaps on images especially in high void fraction, causing termination of bubble tracking and erroneous estimation of bubble size. The overlap problem has been considered in recent analyses (Reference de Langlard, Al-Saddik, Charton, Debayle and Lamadiede Langlard et al. 2018; Reference Zhou and NiuZhou & Niu 2020; Reference Chen, Huang, Hu, Yin and WangChen et al. 2022). Reference Gao, Deane, Liu and ShenGao et al. (2021) proposed a technique for Lagrangian tracking of bubbles entrained by computed breaking waves in three-dimensional space, which determined optimal network links of bubbles to minimize the pseudo-distance errors with constraints of bubble positions, velocity and volume between adjacent time instants. This technique detected five evolution behaviours of formation, extinction, continuity, binary fragmentation and binary coalescence. In the current experiments of surface bubbles floating on aliquid surface without any bubble overlap, as the observed motions of bubbles were two-dimensional (see supplementary movie 1), the number of candidate links of bubbles between adjacent frames was much smaller than that for submerged bubbles three-dimensionally dispersed in breaking waves. In addition, while strong shear and turbulence highly deformed bubble surfaces leading to fragmentation in breaking waves, a similar breakup process could not observed in the current experiments. Therefore, we introduced a simpler method of two-dimensional bubble tracking, which was similar to the algorithm by Reference Rodriguez-Rodriguez, Martínez-Bazán and MontañésRodriguez-Rodriguez et al. (2003), taking into account bubble emergence, bursting, continuity and binary coalescence, under constraints of bubble position and size between adjacent video frames. The bubble tracking was performed as follows:

  1. (1) Detect positions, $\boldsymbol {x}_i^j$, and diameters, $d_i^j$, of all bubbles numbered $i = 1, \ldots, n (j)$ on successive images with frame numbers $j = 1, \ldots, N$ using the PCCHT procedure, where $n (j)$ and $N$ are the bubble population on the $j$th image and the total number of video frames, respectively.

  2. (2) Assuming that the bubble velocity $\boldsymbol {u}_i^j$ at bubble location $\boldsymbol {x}_i^j$ and time $t = j \Delta t$ is known, approximate the translational position at the next frame as $\boldsymbol {x}_c = \boldsymbol {x}_i^{j} + \boldsymbol {u}_i^j \Delta t$, where $\Delta t$ is the time increment of the image frames. Search for the candidate bubble on image $j+1$ with the nearest location to $\boldsymbol {x}_c$ (see figure 24).

  3. (3) If the diameter of the candidate bubble, $d_c$, is consistent with the diameter of the previous bubble, $d_i^j$, with a size criterion of $\mid 1-d_i^j/d_c\mid <0.5$, then the candidate is linked with the bubble path (see figure 24). Determine the bubble location at $j+1$ of the link, $\boldsymbol {x}_i^{j+1}$. Estimate the distance error $\delta =\mid \boldsymbol {x}_i^{j+1}-\boldsymbol {x}_c \mid$ for validation (figure 25).

  4. (4) If both candidate positions, $\boldsymbol {x}_c$, of two neighbouring bubbles are close to $\boldsymbol {x}_i^{j+1}$, fulfilling the distance criterion $\delta < d_i$, and the size constraint for the larger bubble,$\mid 1-d_i^j/d_c\mid <0.5$, is satisfied, the two bubbles are considered to coalesce (see case of bubbles 2 and 4 in figure 24), which corresponds to the pseudo-distance approach by Reference Rodriguez-Rodriguez, Martínez-Bazán and MontañésRodriguez-Rodriguez et al. (2003). The daughter bubble inherits longer lifetime of either parent bubble (generally a larger one through coalescence), while the lifetime of the other parent is terminated upon coalescence.

  5. (5) Update the bubble velocity as $\boldsymbol {u}_i^{j+1}=(\boldsymbol {x}_i^{j+1}-\boldsymbol {x}_i^{j})/\Delta t$ (figure 5a).

  6. (6) If no candidate is within the distance criterion ($\delta < d_i$), then terminate tracking under the assumption that the bubble bursts. Determine the bubble lifetime according to the total number of images obtained during its movement (see case of bubble 1 in figure 24).

Figure 24. (a) Schematic diagram of bubble behaviours in successive time instants and (b) corresponding network links of bubbles: bubble 1 bursting at $t=t_0+3\Delta t$, bubbles 2 and 6 coalescing at $t=t_0+3\Delta t$, bubble 3 continuing translational motion, bubble 4 reaching an edge of field of view (FOV) and bubble 5 immediately vanishing after emergence of surface. The red arrow in (b) indicates the network link used for estimating the lifetime ended by bursting, and the blue arrow is the link used for estimating the lifetime ended by coalescence. The cases of bubbles 4 and 5 (indicated by the black links) were excluded from the analysis.

Figure 25. The mean distance errors in experiment S1 (a) and S2 (b).

This method, assuming circular bubbles, cannot be used for highly deformed bubbles, which are often observed during coalescence. In such instances, because the bubble location cannot be determined, the trajectory is temporarily terminated. However, because the coalesced bubble rapidly recovers its circular shape, detection may resume after a time lag, typically within several frames. In this computation, a coalesced daughter bubble with substantial deformation was observed within a short time (0.08 s) after track termination and was linked with the terminated trajectory upon detection.

Lifetimes ended both by bursting and by coalescence are considered in § 7. We note that many surface bubbles vanished in a short duration after their appearance on the surface in both the experiments. Such immediate bursting has been considered as an identical process of coalescence of approaching bubbles in bulk (Reference Kirkpatrick and LockettKirkpatrick & Lockett 1974; Reference Chesters and HofmanChesters & Hofman 1982); that is, the immediate bursting depends on rise velocity of a bubble arriving at the surface. While it is interesting to study the immediate bursting at the surface, affected by vertical acceleration, its mechanism is different from that for surface bubbles exhibiting two-dimensional motion on a liquid surface without vertical movement, considered in this work (§ 4). Therefore, we excluded the bubble lifetime less than 16 ms ended by the immediate bursting from the current analysis focusing on behaviours of floating bubbles. Once a bubble reached an edge of field of view or appeared from outside of field of view, tracking data for the bubble were excluded from the analysis because the lifetime of the bubble was undetermined (see case of bubble 4 in figure 24).

Figure 25 shows the mean distance errors over all tracking data during the whole video frames. While the errors for non-surfactant bubbles that deformed at successive coalescence in experiment S1 (figure 6) were relatively large, the maximum error of 1.2 mm achieved at $d=9.5$ mm was smaller than the criterion $d$, indicating that bubbles were appropriately associated between adjacent video frames in the current bubble tracking.

References

Abadie, T., et al. 2022 Oxygen transfer of microbubble clouds in aqueous solutions–application to wastewater. Chem. Engng Sci. 257, 117693.CrossRefGoogle Scholar
Anagbo, P.E. & Brimacobe, J.K. 1990 Plume characteristics and liquid circulation in gas injection through a porous plug. Metall. Trans. B 21, 637648.CrossRefGoogle Scholar
Atherton, T.J. & Kerbyson, D.J. 1993 Using phase to represent radius in the coherent circle hough transform. In IEE Colloquium on Hough Transforms, pp. 5/1–5/4. IET.CrossRefGoogle Scholar
Atherton, T.J. & Kerbyson, D.J. 1999 Size invariant circle detection. Image Vis. Comput. 17 (11), 795803.CrossRefGoogle Scholar
Brattberg, T. & Chanson, H. 1998 Air entrapment and air bubble dispersion at two-dimensional plunging water jets. Chem. Engng Sci. 53 (24), 41134127.CrossRefGoogle Scholar
Callaghan, A.H. 2013 An improved whitecap timescale for sea spray aerosol production flux modeling using the discrete whitecap method. J. Geophys. Res. 118 (17), 999710010.CrossRefGoogle Scholar
Callaghan, A.H., Deane, G.B. & Dale Stokes, M. 2008 Observed physical and environmental causes of scatter in whitecap coverage values in a fetch-limited coastal zone. J. Geophys. Res. 113 (C5), C05022.CrossRefGoogle Scholar
Callaghan, A.H., Deane, G.B. & Dale Stokes, M. 2013 Two regimes of laboratory whitecap foam decay: bubble-plume controlled and surfactant stabilized. J. Phys. Oceanogr. 43 (6), 11141126.CrossRefGoogle Scholar
Callaghan, A.H., Deane, G.B., Dale Stokes, M. & Ward, B. 2012 Observed variation in the decay time of oceanic whitecap foam. J. Geophys. Res. 117 (C9), C09015.CrossRefGoogle Scholar
Callaghan, A.H., Deane, G.B. & Stokes, M.D. 2016 Laboratory air-entraining breaking waves: imaging visible foam signatures to estimate energy dissipation. Geophys. Res. Lett. 43 (21), 11320–11328.CrossRefGoogle Scholar
Carrica, P.M., Drew, D., Bonetto, F. & Lahey, R.T. 1999 A polydisperse model for bubbly two-phase flow around a surface ship. Intl J. Multiphase Flow 25 (2), 257305.CrossRefGoogle Scholar
Chan, D.Y.C., Klaseboer, E. & Manica, R. 2011 Film drainage and coalescence between deformable drops and bubbles. Soft Matt. 7 (6), 22352264.CrossRefGoogle Scholar
Chanson, H. 1995 Air entrainment in two-dimensional turbulent shear flows with partially developed inflow conditions. Intl J. Multiphase Flow 21 (6), 11071121.CrossRefGoogle Scholar
Chen, W., Huang, G., Hu, Y., Yin, J. & Wang, D. 2022 Experimental study on continuous spectrum bubble generator with a new overlapping bubbles image processing technique. Chem. Engng Sci. 254, 117613.CrossRefGoogle Scholar
Chesters, A.K. 1991 Modelling of coalescence processes in fluid-liquid dispersions: a review of current understanding. Chem. Engng Res. Des. 69 (A4), 259270.Google Scholar
Chesters, A.K. & Hofman, G. 1982 Bubble coalescence in pure liquids. Appl. Sci. Res. 38 (1), 353361.CrossRefGoogle Scholar
Couder, Y., Fort, E., Gautier, C.-H. & Boudaoud, A. 2005 From bouncing to floating: noncoalescence of drops on a bath. Phys. Rev. Lett. 94, 177801.CrossRefGoogle ScholarPubMed
Cumming, P.D. & Chanson, H. 1997 a Air entrainment in the developing flow region of plunging jets. Part 1. Theoretical development. J. Fluids Engng 119, 597602.CrossRefGoogle Scholar
Cumming, P.D. & Chanson, H. 1997 b Air entrainment in the developing flow region of plunging jets. Part 2. Experimental. J. Fluids Engng 119, 603608.CrossRefGoogle Scholar
Cumming, P.D. & Chanson, H. 1999 An experimental study of individual air bubble entraiment at a planar plunging jet. Chem. Engng Res. Des. 77 (Part A), 159164.CrossRefGoogle Scholar
Czerski, H., Brooks, I.M., Gunn, S., Pascal, R., Matei, A. & Blomquist, B. 2022 Ocean bubbles under high wind conditions. Part 1. Bubble distribution and development. Ocean Sci. 18 (3), 565586.CrossRefGoogle Scholar
Deane, G.B. & Stokes, M.D. 2002 Scale dependence of bubble creation mechanisms in breaking waves. Nature 418 (6900), 839844.CrossRefGoogle Scholar
Duncan, J.H. 2001 Spilling breaker. Annu. Rev. Fluid Mech. 33 (1), 519547.CrossRefGoogle Scholar
Friedlander, S.K. 2000 Smoke, Dust, and Haze, Vol. 198. Oxford University Press.Google Scholar
Gao, Q., Deane, G.B., Liu, H. & Shen, L. 2021 A robust and accurate technique for lagrangian tracking of bubbles and detecting fragmentation and coalescence. Intl J. Multiphase Flow 135, 103523.CrossRefGoogle Scholar
Hassan, Y.A. & Canaan, R.E. 1991 Full-field bubbly flow velocity measurements using a multiframe particle tracking technique. Exp. Fluids 12–12 (1–2), 4960.CrossRefGoogle Scholar
Hinze, J.O. 1955 Fundamentals of the hydrodynamic mechanism of splitting in dispersion processes. AIChE J. 1 (3), 289295.CrossRefGoogle Scholar
Jähne, B. & Haußecker, H. 1998 Air-water gas exchange. Annu. Rev. Fluid Mech. 30 (1), 443468.CrossRefGoogle Scholar
Kerbyson, D.J. & Atherton, T.J. 1995 Circle detection using Hough transform filters, 5th Intl Conf. on Image Processing and its Applications, pp. 370–374. IET.CrossRefGoogle Scholar
Kiger, K.T. & Duncan, J.H. 2012 Air-entrainment mechanisms in plunging jets and breaking waves. Annu. Rev. Fluid Mech. 44 (1), 563596.CrossRefGoogle Scholar
Kimme, C., Ballard, D. & Sklansky, J. 1975 Finding circles by an array of accumulators. In Proc. ACM 18, pp. 120–122. Association for Computing Machinery.CrossRefGoogle Scholar
Kirkpatrick, R.D. & Lockett, M.J. 1974 The influence of approach velocity on bubble coalescence. Chem. Engng Sci. 29 (12), 23632373.CrossRefGoogle Scholar
Lamarre, E. & Melville, W.K. 1991 Air entrainment and dissipation in breaking waves. Nature 351 (6326), 469472.CrossRefGoogle Scholar
Langevin, D. 2019 Coalescence in foams and emulsions: similarities and differences. Curr. Opin. Colloid Interface Sci. 44, 2331.CrossRefGoogle Scholar
de Langlard, M., Al-Saddik, H., Charton, S., Debayle, J. & Lamadie, F. 2018 An efficiency improved recognition algorithm for highly overlapping ellipses: application to dense bubbly flows. Pattern Recognit. Lett. 101, 8895.CrossRefGoogle Scholar
Laupsien, D., Le Men, C., Cockx, A. & Liné, A. 2019 Image processing for bubble morphology characteristics in diluted bubble swarms. Phys. Fluids 31 (5), 053306.CrossRefGoogle Scholar
Lhuissier, H. & Villermaux, E. 2011 Bursting bubble aerosols. J. Fluid Mech. 696, 544.CrossRefGoogle Scholar
Liu, X. & Duncan, J.H. 2006 An experimental study of surfactant effects on spilling breakers. J. Fluid Mech. 567, 433.CrossRefGoogle Scholar
Marchisio, D.L. & Fox, R.O. 2013 Computational Models for Polydisperse Particulate and Multiphase Systems. Cambridge University Press.CrossRefGoogle Scholar
Marmorino, G.O. 2005 Bright and dark ocean whitecaps observed in the infrared. Geophys. Res. Lett. 32 (11), L11604.CrossRefGoogle Scholar
Martínez-Bazán, C., Montañés, J.L. & Lasheras, J.C. 1999 On the breakup of an air bubble injected into a fully developed turbulent flow. Part 1. Breakup frequency. J. Fluid Mech. 401, 157182.CrossRefGoogle Scholar
Melville, W.K. 1996 The role of surface-wave breaking in air-sea interaction. Annu. Rev. Fluid Mech. 28 (1), 279321.CrossRefGoogle Scholar
Monahan, E.C. 1971 Oceanic whitecaps. J. Phys. Oceanogr. 1 (2), 139144.2.0.CO;2>CrossRefGoogle Scholar
Monahan, E.C. & Lu, M. 1990 Acoustically relevant bubble assemblages and their dependence on meteorological parameters. IEEE J. Ocean. Engng 15 (4), 340349.CrossRefGoogle Scholar
Monahan, E.C. & Muircheartaigh, L. 1980 Optimal power-law description of oceanic whitecap coverage dependence on wind speed. J. Phys. Oceanogr. 10 (12), 20942099.2.0.CO;2>CrossRefGoogle Scholar
Na, B., Chang, K.-A. & Lim, H.-J. 2019 Flow kinematics and air entrainment under laboratory spilling breaking waves. J. Fluid Mech. 882, A15.Google Scholar
Néel, B. & Deike, L. 2021 Collective bursting of free-surface bubbles, and the role of surface contamination. J. Fluid Mech. 917, A46.CrossRefGoogle Scholar
Nicolson, M.M. 1949 The interaction between floating particles. Math. Proc. Camb. Phil. Soc. 45 (2), 288295.CrossRefGoogle Scholar
Niida, Y. & Watanabe, Y. 2018 Oxygen transfer from bubble-plumes. Phys. Fluids 30, 107104.CrossRefGoogle Scholar
Prince, M.J. & Blanch, H.W. 1990 Bubble coalescence and break-up in air-sparged bubble columns. AIChE J. 36 (10), 14851499.CrossRefGoogle Scholar
Radoëv, B.P., Dimitrov, D.S. & Ivanov, I.B. 1974 Hydrodynamics of thin liquid films effect of the surfactant on the rate of thinning. Colloid Polym. Sci. 252 (1), 5055.CrossRefGoogle Scholar
Ravelet, F., Colin, C. & Risso, F. 2011 On the dynamics and breakup of a bubble rising in a turbulent flow. Phys. Fluids 23 (10), 103301.CrossRefGoogle Scholar
Risso, F. 2018 Agitation, mixing, and transfers induced by bubbles. Annu. Rev. Fluid Mech. 50 (1), 2548.CrossRefGoogle Scholar
Rodriguez-Rodriguez, J., Martínez-Bazán, C. & Montañés, J.L. 2003 A novel particle tracking and break-up detection algorithm: application to the turbulent break-up of bubbles. Meas. Sci. Technol. 14 (8), 13281340.CrossRefGoogle Scholar
Ruiz-Rus, J., Ern, P., Roig, V. & Martínez-Bazán, C. 2022 Coalescence of bubbles in a high Reynolds number confined swarm. J. Fluid Mech. 944, A13.CrossRefGoogle Scholar
Schilling, K. & Zessner, M. 2011 Foam in the aquatic environment. Water Res. 45 (15), 43554366.CrossRefGoogle ScholarPubMed
Shaw, D.B. & Deike, L. 2021 Surface bubble coalescence. J. Fluid Mech. 915, A105.CrossRefGoogle Scholar
Slauenwhite, D.E. & Johnson, B.D. 1999 Bubble shattering: differences in bubble formation in fresh water and seawater. J. Geophys. Res. 104 (C2), 32653275.CrossRefGoogle Scholar
Soto, Á.M., Maddalena, T., Fraters, A., van der Meer, D. & Lohse, D. 2018 Coalescence of diffusively growing gas bubbles. J. Fluid Mech. 846, 143165.CrossRefGoogle Scholar
Sungkorn, R., Derksen, J.J. & Khinast, J.G. 2011 Euler-lagrange modeling of a gas-liquid stirred reactor with consideration of bubble breakage and coalescence. AIChE J. 58 (5), 13561370.CrossRefGoogle Scholar
Toba, Y. 1959 Drop production by bursting of air bubbles on the sea surface (II) theoretical study on the shape of floating bubbles. J. Oceanogr. Soc. Japan 15 (3), 121130.CrossRefGoogle Scholar
Veron, F. 2015 Ocean spray. Annu. Rev. Fluid Mech. 47 (1), 507538.CrossRefGoogle Scholar
Villermaux, E., Wang, X. & Deike, L. 2022 Bubbles spray aerosols: certitudes and mysteries. PNAS Nexus 1 (5), pgac261.CrossRefGoogle ScholarPubMed
Wanninkhof, R., Asher, W.E., Ho, D.T., Sweeney, C. & McGillis, W.R. 2009 Advances in quantifying air-sea gas exchange and environmental forcing. Annu. Rev. Mar. Sci. 1 (1), 213244.CrossRefGoogle ScholarPubMed
Watanabe, Y. 2022 Dynamics of Water Surface Flows and Waves. CRC Press.CrossRefGoogle Scholar
Watanabe, Y. & Ingram, D.M. 2015 Transverse instabilities of ascending planar jets formed by wave impacts on vertical walls. Proc. R. Soc. A 471, 20150397.CrossRefGoogle Scholar
Watanabe, Y. & Mori, N. 2008 Infrared measurements of surface renewal and subsurface vortices in nearshore breaking waves. J. Geophys. Res. 113 (C7), C07015.CrossRefGoogle Scholar
Watanabe, Y., Oyaizu, H., Satoh, H. & Niida, Y. 2021 Bubble drag in electrolytically generated microbubble swarms with bubble-vortex interactions. Intl J. Multiphase Flow 136, 103541.CrossRefGoogle Scholar
Watanabe, Y., Saeki, H. & Hosking, R.J. 2005 Three-dimensional vortex structures breaking waves. J. Fluid Mech. 545, 218328.CrossRefGoogle Scholar
Wu, N., Dai, J. & Micale, F.J. 1999 Dynamic surface tension measurement with a dynamic wilhelmy plate technique. J. Colloid Interface Sci. 215 (2), 258269.CrossRefGoogle Scholar
Wurl, O., Wurl, E., Miller, L., Johnson, K. & Vagle, S. 2011 Formation and global distribution of sea-surface microlayers. Biogeosciences 8 (1), 121135.CrossRefGoogle Scholar
Yuen, H.K., Princen, J., Illingworth, J. & Kittler, J. 1990 Comparative study of hough transform methods for circle finding. Image Vis. Comput. 8 (1), 7177.CrossRefGoogle Scholar
Zaruba, A., Krepper, E., Prasser, H.-M. & Schleicher, E. 2005 Measurement of bubble velocity profiles and turbulent diffusion coefficients of the gaseous phase in rectangular bubble column using image processing. Exp. Therm. Fluid Sci. 29 (7), 851860.CrossRefGoogle Scholar
Zheng, Q.A., Klemas, V. & Hsu, Y.-H.L. 1983 Laboratory measurement of water surface bubble life time. J. Geophys. Res. 88 (C1), 701.CrossRefGoogle Scholar
Zhou, H. & Niu, X. 2020 An image processing algorithm for the measurement of multiphase bubbly flow using predictor-corrector method. Intl J. Multiphase Flow 128, 103277.CrossRefGoogle Scholar
Figure 0

Figure 1. Photographs of aerated water generated by shoaling wave splash in the surf zone, taken at Pecatu, South Bali (a) and patches of surface bubbles drifted behind whitecaps, taken at Mombetsu, Hokkaido (b).

Figure 1

Figure 2. Schematic illustrations of (a) bubble-cap film thinning through drainage, (b) retraction of the rim bounding the film as the bubble bursts, (c) bubble attraction on the meniscus surface and (d) neck expansion during coalescence.

Figure 2

Figure 3. Two experimental set-ups for artificial bubble generation. (ac) Experiment S1: entrainment using planar plunging jets. (df) Experiment S2: air ejection through a circular porous ceramic plate. (c,f) Schematic of typical flow patterns formed in each experiment.

Figure 3

Figure 4. Probability densities of circle-equivalent diameters of submerged bubbles for experiments S1 (a) and S2 (b).

Figure 4

Figure 5. Example of the estimated bubble velocity (a) and horizontal distributions of the mean horizontal bubble velocity (b) and its standard deviation (c). Dotted and solid lines indicate experiments S1 and S2.

Figure 5

Figure 6. Backlit images of bubble clusters during the coalescing process at $C=0$ in experiment S1 for (a) $t=t_0$, (b) $t=t_0+\Delta t$ and (c) $t=t_0+2\Delta t$, where $\Delta t=8$ ms. Arrows indicate neck expansion of coalescing bubbles.

Figure 6

Figure 7. Backlit images of bubble clusters during the bursting process at $C=0$ in experiment S1 for (a) $t=t_0$, (b) $t=t_0+\Delta t$ and (c) $t=t_0+2\Delta t$, where $\Delta t= 4$ ms. Arrow indicates the boundary of the cap film.

Figure 7

Figure 8. Backlit images of bubble clusters at $C= 400\,{\mathrm {\mu }}$g l$^{-1}$ in experiment S1 for (a) $t=t_0$, (b) $t=t_0+\Delta t$ and (c) $t=t_0+2\Delta t$, where $\Delta t=4$ ms. Arrow indicates locations of bubbles that successively burst.

Figure 8

Figure 9. Horizontal variations of bubble size distributions in experiment S1.

Figure 9

Figure 10. Backlit images of bubble clusters in the process of coalescing and bursting at $C= 0$ in experiment S2 for (a) $t=t_0$, (b) $t=t_0+32\Delta t$, (c) $t=t_0+50\Delta t$, (d) $t=t_0+91\Delta t$ and (e) $t=t_0+108\Delta t$, where $\Delta t= 4$ ms. Red letters (A–F) indicate original bubbles before coalescence, for reference.

Figure 10

Figure 11. Backlit images of bubble clusters during the processes of coalescence and aggregation and bursting at $C= 400\,{\mathrm {\mu }}$g l$^{-1}$ in experiment S2 for (a) $t=t_0$, (b) $t=t_0+45\Delta t$, (c) $t=t_0+122\Delta t$, (d) $t=t_0+241\Delta t$, (e) $t=t_0+252\Delta t$ and (f) $t=t_0+289\Delta t$, where $\Delta t= 4$ ms. Arrows in (ac) indicate coalescing bubbles, whereas arrows in (df) indicate past sites of vanished bubbles.

Figure 11

Figure 12. Horizontal variations of bubble size distributions in experiment S2. Bubble size growth owing to coalescence during horizontal travel is indicated in the area surrounded by a dashed curve. A vertical line indicates a critical travel distance at which most bubbles have vanished.

Figure 12

Figure 13. Successive backlit images demonstrating that floating particles (arrows) passed over the cap films of bubbles travelling from left to right. The time interval of the images in (ac) was $\Delta t= 4$ ms.

Figure 13

Figure 14. Schematic illustrations of the top (a) and side (b) views of a surface bubble moving from left to right. (a) Particles floating on the cap surface translating in the opposite direction to the bubble movement. (b) Film liquid on a moving bubble is replaced by liquid from the downstream surface. After a disturbance on the surface, the cap film liquid is replaced with disturbed surface liquid during bubble travel, leading to rupture of the film.

Figure 14

Figure 15. (a) A circular disk-shaped film on the bubble wall of two colliding surface bubbles. (b) Thinning rates of the film thickness, $h/h_0$, estimated by (4.5) (blue), (4.6) (red) and (4.7) (black) at $h_0=100\,{\mathrm {\mu }}$m and $C=0$: — ($R=1.0$ mm), - - - ($R=2.0$ mm), $\cdots$ ($R=3.0$ mm), – $\cdot$ – ($R=4.0$ mm).

Figure 15

Figure 16. Size distribution plots as a function of the bubble volume in experiment S1 (a-i,b-i,c-i) and S2 (a-ii,b-ii,c-ii) for (a-i,a-ii) $C=0\,{\mathrm {\mu }}$g l$^{-1}$, (b-i,b-ii) $400\,{\mathrm {\mu }}$g l$^{-1}$ and (c-i,c-ii) $800\,{\mathrm {\mu }}$g l$^{-1}$.

Figure 16

Figure 17. Rates of birth $Q_c$ and death $Q_m$ of bubbles due to coalescence and rate of bursting $Q_b$ as a function of the bubble volume in experiment S1 (a-i,b-i,c-i) and S2 (a-ii,b-ii,c-ii) for (a-i,a-ii) $C= 0\,{\mathrm {\mu }}g$ l$^{-1}$, (b-i,b-ii) $400\,{\mathrm {\mu }}g$ l$^{-1}$ and (c-i,c-ii) $800\,{\mathrm {\mu }}$g l$^{-1}$.

Figure 17

Figure 18. Current estimates of mean frequencies of coalescence and bursting, defined by (6.6a,b), and global decay time, (6.7), compared with the previous ones, (6.5), by Néel & Deike (2021) (ND): (a) frequencies in experiment S1, (b) frequencies in experiment S2 and (c) decay time.

Figure 18

Figure 19. Scatter plots of bubble lifetime $T_l$ as a function of the diameter of the bursting bubble $d_b$ in experiments S1 (a) and S2 (b).

Figure 19

Table 1. Optimal proportional constants fitted with a linear equation of $d_b$ and the root-mean-square deviation from the linear approximation.

Figure 20

Figure 20. Probability densities of bubble lifetimes in experiments S1 (a) and S2 (b). Solid lines indicate Weibull distributions (7.1), with optimal parameters given in table 1.

Figure 21

Table 2. Parameters of a Weibull distribution, and reliable lifetimes.

Figure 22

Figure 21. The PCCHT procedure used to determine the locations and sizes of circular bubbles. (a) Original backlit images of surface bubbles. (b) Number of responses in centre coordinate space. Bubble centres are positioned at coordinates with response peaks. (c) Bubble radii determined using the centre coordinate values shown in (b). (d) Circles indicating the estimated radii and centre coordinates, superimposed on (a).

Figure 23

Figure 22. (a) Original backlit image, (b) edges detected by the Sobel method, (c) edges detected by the Canny method, (d) current estimation of circular edges by the PCCHT method and (e) definition of overlap length.

Figure 24

Figure 23. Mean overlap length $\epsilon$ (solid line) and relative overlap length $\epsilon /d$ (dotted line) in experiment S1 (a) and S2 (b).

Figure 25

Figure 24. (a) Schematic diagram of bubble behaviours in successive time instants and (b) corresponding network links of bubbles: bubble 1 bursting at $t=t_0+3\Delta t$, bubbles 2 and 6 coalescing at $t=t_0+3\Delta t$, bubble 3 continuing translational motion, bubble 4 reaching an edge of field of view (FOV) and bubble 5 immediately vanishing after emergence of surface. The red arrow in (b) indicates the network link used for estimating the lifetime ended by bursting, and the blue arrow is the link used for estimating the lifetime ended by coalescence. The cases of bubbles 4 and 5 (indicated by the black links) were excluded from the analysis.

Figure 26

Figure 25. The mean distance errors in experiment S1 (a) and S2 (b).

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