Inviscid instability of two-fluid free surface flow down an incline

The inviscid temporal stability analysis of two-fluid parallel shear flow with a free surface, down an incline, is studied. The velocity profiles are chosen as piecewise-linear with two limbs. The analysis reveals the existence of unstable inviscid modes, arising due to wave interaction between the...

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Main Authors: Ghosh, Sukhendu, Usha, Ranganathan, Govindarajan, Rama, Tammisola, Outi
Format: Article
Published: Springer 2016
Online Access:https://eprints.nottingham.ac.uk/33266/
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author Ghosh, Sukhendu
Usha, Ranganathan
Govindarajan, Rama
Tammisola, Outi
author_facet Ghosh, Sukhendu
Usha, Ranganathan
Govindarajan, Rama
Tammisola, Outi
author_sort Ghosh, Sukhendu
building Nottingham Research Data Repository
collection Online Access
description The inviscid temporal stability analysis of two-fluid parallel shear flow with a free surface, down an incline, is studied. The velocity profiles are chosen as piecewise-linear with two limbs. The analysis reveals the existence of unstable inviscid modes, arising due to wave interaction between the free surface and the shear jump interface. Surface tension decreases the maximum growth rate of the dominant disturbance. Interestingly, in some limits, surface tension destabilises extremely short waves in this flow. This can happen because of the interaction with the shear-jump interface. This flow may be compared with a corresponding viscous two-fluid flow. Though viscosity modifies the stability properties of the flow system both qualitatively and quantitatively, there is qualitative agreement between the viscous and inviscid stability analysis when the less viscous fluid is closer to the free surface.
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spelling nottingham-332662020-05-04T17:57:02Z https://eprints.nottingham.ac.uk/33266/ Inviscid instability of two-fluid free surface flow down an incline Ghosh, Sukhendu Usha, Ranganathan Govindarajan, Rama Tammisola, Outi The inviscid temporal stability analysis of two-fluid parallel shear flow with a free surface, down an incline, is studied. The velocity profiles are chosen as piecewise-linear with two limbs. The analysis reveals the existence of unstable inviscid modes, arising due to wave interaction between the free surface and the shear jump interface. Surface tension decreases the maximum growth rate of the dominant disturbance. Interestingly, in some limits, surface tension destabilises extremely short waves in this flow. This can happen because of the interaction with the shear-jump interface. This flow may be compared with a corresponding viscous two-fluid flow. Though viscosity modifies the stability properties of the flow system both qualitatively and quantitatively, there is qualitative agreement between the viscous and inviscid stability analysis when the less viscous fluid is closer to the free surface. Springer 2016-06-10 Article PeerReviewed Ghosh, Sukhendu, Usha, Ranganathan, Govindarajan, Rama and Tammisola, Outi (2016) Inviscid instability of two-fluid free surface flow down an incline. Meccanica . ISSN 1572-9648 (In Press)
spellingShingle Ghosh, Sukhendu
Usha, Ranganathan
Govindarajan, Rama
Tammisola, Outi
Inviscid instability of two-fluid free surface flow down an incline
title Inviscid instability of two-fluid free surface flow down an incline
title_full Inviscid instability of two-fluid free surface flow down an incline
title_fullStr Inviscid instability of two-fluid free surface flow down an incline
title_full_unstemmed Inviscid instability of two-fluid free surface flow down an incline
title_short Inviscid instability of two-fluid free surface flow down an incline
title_sort inviscid instability of two-fluid free surface flow down an incline
url https://eprints.nottingham.ac.uk/33266/