2017
DOI: 10.1021/acs.langmuir.7b02280
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Toroidal Droplets: Growth Rates, Dispersion Relations, and Behavior in the Thick-Torus Limit

Abstract: Toroidal droplets in a viscous liquid are unstable and transform into single or multiple spherical droplets. For thin tori, this can happen via the Rayleigh-Plateau instability causing the breakup of cylindrical jets. In contrast, for thick tori, this can happpen via the shrinking of the "hole". In this work, we use the thin-torus limit to directly measure the growth rate associated with capillary disturbances. In the case of toroidal droplets inside a much more viscous liquid, we even obtain the full dispersi… Show more

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Cited by 3 publications
(5 citation statements)
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“…These observations (Figure b–d) are contrary to the periodicity and symmetry expected for a Rayleigh-type instability as manifested in both freestanding and supported toroidally shaped liquid rings, ,, where morphologies are quite sensitive to the radius of the toroid and the fluid flows creates a necklace of linked swells and necks. Freestanding toroidal rings have comparable major and minor diameters (of a few mm) and circular cross-section.…”
Section: Resultsmentioning
confidence: 57%
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“…These observations (Figure b–d) are contrary to the periodicity and symmetry expected for a Rayleigh-type instability as manifested in both freestanding and supported toroidally shaped liquid rings, ,, where morphologies are quite sensitive to the radius of the toroid and the fluid flows creates a necklace of linked swells and necks. Freestanding toroidal rings have comparable major and minor diameters (of a few mm) and circular cross-section.…”
Section: Resultsmentioning
confidence: 57%
“…The observations of aperiodicity and the sequential appearance of mesas, their outward motion as well as their coalescence-assisted growth, and the fact that away from mesas, the ridge maintains its shape indicate that the formation of mesas cannot be attributed to the breakdown of the nanoridge through a capillary-driven Rayleigh-type instability, often cited in the stratification literature ,, as the mechanistic basis of the nanoridge-to-mesa instability. Thus, the quantitative characterization of the formation and evolution of mesas rules out hydrodynamic instabilities due to capillarity or viscous dissipation effects , ,, and strongly suggests a thickness-dependent phase transition. The topological instabilities underlying mesa formation and the emergence of thinner, darker domains are quite analogous, even though in the latter case a metastable branch corresponding to a lower thickness gets picked.…”
Section: Resultsmentioning
confidence: 97%
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“…3B, we show that this result holds over a broad range of flow rates Q and nozzle speeds U0. The order of magnitude of the path wavelength L ∼ A must be similar to that of the natural mode of the instability (30). In this range, it is possible to fully program the instability.…”
Section: Resultsmentioning
confidence: 99%
“…The maintenance of fine droplet structures under conditions such as atomization is primarily characterized by a high Laplace number. [52][53][54] It indicates that the influence of surface tension forces is relatively strong compared to the fluid's momentum, affecting the behavior and dynamics of fluid interfaces, as in the case of the smectic A surface.…”
Section: Surface Tension and Smectic Morphologiesmentioning
confidence: 99%