The nonlinear evolution of an isolated, finite-amplitude wave at the interface between two immiscible fluids of different density is simulated by means of a discrete vortex method. In contrast to a periodic disturbance, that evolves into the familiar train of Kelvin-Helmholtz (KH) linear rolls, the single-wave scenario possess unique features that are not yet well understood. The aim of the present contribution is to provide an in-depth description of the nonlinear wave evolution, and to highlight the different features that distinguish the nonlinear case from the classical KH model. The two-phase interface is represented by a discrete vortex sheet, whose dynamics is simulated by a point vortex method that accounts for density stratification, surface tension and gravity. It is found that the different topology of streamlines occurring in the two cases determine a nonlinear wave speed that is different from the one predicted by classical KH theory. The instability onset threshold, as well as other flowfield properties also change accordingly.
Nonlinear evolution of an isolated disturbance at two-phase flow interface / Coppola, Gennaro; Capuano, Francesco; DE LUCA, Luigi. - In: BULLETIN OF THE AMERICAN PHYSICAL SOCIETY. - ISSN 0003-0503. - (2015).
Nonlinear evolution of an isolated disturbance at two-phase flow interface
COPPOLA, GENNARO;CAPUANO, FRANCESCO;DE LUCA, LUIGI
2015
Abstract
The nonlinear evolution of an isolated, finite-amplitude wave at the interface between two immiscible fluids of different density is simulated by means of a discrete vortex method. In contrast to a periodic disturbance, that evolves into the familiar train of Kelvin-Helmholtz (KH) linear rolls, the single-wave scenario possess unique features that are not yet well understood. The aim of the present contribution is to provide an in-depth description of the nonlinear wave evolution, and to highlight the different features that distinguish the nonlinear case from the classical KH model. The two-phase interface is represented by a discrete vortex sheet, whose dynamics is simulated by a point vortex method that accounts for density stratification, surface tension and gravity. It is found that the different topology of streamlines occurring in the two cases determine a nonlinear wave speed that is different from the one predicted by classical KH theory. The instability onset threshold, as well as other flowfield properties also change accordingly.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.