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Interact Session

Interact: Interesting Assorted Problems Involving Geophysical Flows

10:31 am – 12:31 pm, Sunday November 23 Session C04 George R. Brown Convention Center, 310A
Chair:
Pascale Garaud, University of California, Santa Cruz
Topics:

Direct numerical simulation of gravity-capillary waves breaking with surfactant

10:36 am – 10:37 am
Presenter: Rui Yang (Princeton University)
Authors: Zehua Liu (Princeton University), Palas Kumar Farsoiya (Department of Chemical Engineering, Indian Institute of Technology Roorkee, Roorkee, Uttarakhand 247667, India), Stephane Popinet (Sorbonne Université and CNRS, Institut Jean Le Rond d'Alembert UMR 7190, F-75005 Paris, France), Luc Deike (Department of Mechanical and Aerospace Engineering, High Meadows Environmental Institute, Princeton University)

Surfactant at fluid interfaces plays a crucial role in fluid dynamics by modifying surface tension. This study investigates its effect on waves by integrating an insoluble surfactant transport equation at the interface and incorporating Marangoni forces into an incompressible two-phase Navier–Stokes framework, using the Basilisk solver. Surface tension is modeled via a nonlinear equation of state, following previous experimental observations. We conduct simulations of two-dimensional gravity-capillary waves and analyze the impacts of control parameters on surface roughness, wave regime transitions, and energy budget. Our results reveal a non-monotonic relationship between surfactant concentration and wave roughness: roughness initially decreases and then increases with surfactant concentration as parasitic capillary waves are either suppressed or enhanced, while the energy budget displays the opposite trend. The presence of surfactants also induces earlier transitions between wave regimes. We further quantify the non-monotonic behavior in roughness and energy by the effective Marangoni number based on surface tension gradient, while transitions between wave regimes are governed by the effective Bond number.

Funding acknowledgement

This work is supported by the National Science Foundation under grant 2318816 to LD (Physical Oceanography program) and the NASA Ocean Vector Winds Science Team, grant 80NSSC23K0983 to LD.

PRESENTATIONS (18)