Abstract

In this article, we investigate the effect of surface tension in the Rayleigh–Taylor (RT) problem of stratified incompressible viscoelastic fluids. We prove that there exists an unstable solution to the linearized stratified RT problem with a largest growth rate Λ under the instability condition (i.e., the surface tension coefficient ϑ is less than a threshold vartheta _{c}). Moreover, for this instability condition, the largest growth rate varLambda _{vartheta } decreases from a positive constant to 0, when ϑ increases from 0 to vartheta _{c}, which mathematically verifies that the internal surface tension can constrain the growth of the RT instability during the linear stage.

Highlights

  • It is well known that the equilibrium state of the heavier fluid on top of the lighter one under the gravity is unstable to sustain a small disturbance

  • In 1953, Bellman–Pennington [2] first analyzed the inhibition of RT instability by surface tension, where the study was based on a linearized two-dimensional (2D) motion equation of stratified incompressible inviscid fluids defined on the domain T1 × (–h, h+) (i.e., μ = 0 in the corresponding 2D case of (1.13))

  • 3 Main results In this paper, we investigate the effect of surface tension on the linear RT instability by the linearized motion (1.13)

Read more

Summary

Introduction

It is well known that the equilibrium state of the heavier fluid on top of the lighter one under the gravity is unstable to sustain a small disturbance. In 1953, Bellman–Pennington [2] first analyzed the inhibition of RT instability by surface tension, where the study was based on a linearized two-dimensional (2D) motion equation of stratified incompressible inviscid fluids defined on the domain T1 × (–h–, h+) (i.e., μ = 0 in the corresponding 2D case of (1.13)). They precisely proved that there exists a threshold gtρuL21 of surface tension coefficient for linear stability and instability of RT problem. As documented in [14, 18], the results of nonlinear RT instability in inhomogeneous fluid (without interface), by the classical bootstrap instability method, were obtained for inviscid and viscous cases

Simplified notations
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.