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Updated: Dec 9, 2025

Magnetically Induced Rotating Rayleigh-Taylor Instability
Published on: March 3, 2017
Stability of a directional Marangoni flow.
Corentin Tregouet1, Arnaud Saint-Jalmes1
1Univ Rennes, CNRS, IPR (Institut de Physique de Rennes), UMR 6251, F-35000, Rennes, France. corentin.tregouet@univ-rennes1.fr.
Confined Marangoni flows form inertial surface jets, which destabilize into meanders. This study analytically predicts jet velocity profiles and meander wavelengths, validated by experiments.
Area of Science:
- Fluid dynamics
- Surface phenomena
- Surfactant behavior
Background:
- Marangoni flows, driven by surface-tension gradients, are crucial in phenomena like foam dynamics and microswimmer propulsion.
- These flows typically occur over finite surface distances, with secondary flows observable on larger scales.
Purpose of the Study:
- To investigate the behavior of Marangoni flows when laterally confined.
- To characterize the resulting inertial surface jet and its subsequent destabilization.
- To provide an analytical framework for understanding confined Marangoni spreading.
Main Methods:
- Experimental observation of Marangoni flows in a laterally confined system.
- Analytical prediction of the surface jet's velocity profile.
- Quantitative comparison of theoretical predictions with experimental measurements of meander wavelengths.
Main Results:
- Lateral confinement transforms Marangoni flow into an inertial surface jet.
- The velocity profile of this jet was accurately predicted analytically and matched experimental data.
- The straight jet was observed to destabilize into meanders, with critical wavelengths quantitatively agreeing with theory.
Conclusions:
- The study provides a comprehensive understanding of 2D confined Marangoni spreading.
- It highlights the significant role of inertial effects in confined Marangoni flows.
- This work serves as a foundation for further research into Marangoni flow dynamics under confinement.
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