Closure relations effects on the prediction of the stratified two-phase flow stability via the two-fluid model. (December 2017)

• Record Type: Journal Article
• Authors: Kushnir, R.; Segal, V.; Ullmann, A.; Brauner, N.
• Is Part Of: International journal of multiphase flow. Volume 97(2017)
• Page Start: 78
• Page End: 93
• Publication Date: 2017-12
• Subjects: Two-fluid model -- Stratified flow -- Closure relations -- Stability -- Sheltering -- Multiple solutions; Multiphase flow -- Periodicals; Écoulement polyphasique -- Périodiques; Multiphase flow; Periodicals; 620.1064
• DOI: 10.1016/j.ijmultiphaseflow.2017.07.010
• Languages: English
• ISSNs: 0301-9322

Abstract

Highlights: Stability analysis of stratified flow via the Two-Fluid (TF) model is revisited. The required closure relations are critically examined and new ones are suggested. The TF model is able to reproduce the exact long wave neutral stability curves. The role of the 'sheltering force' due to wave induced shear stresses is quantified. A simple closure relation for the 'sheltering' term in the TF model is provided. Abstract: The possibility of predicting the exact long wave linear stability boundary via the two-fluid (TF) model for horizontal and inclined stratified two-phase flow is examined. The application of the TF model requires the introduction of empirical closure relations for the velocity profile shape factors and for the wave induced wall and interfacial shear stresses. The latter are recognized as the problematic closure laws. In order to explore the closure relations effects and to suggest the necessary modifications that can improve the stability predictions of the TF model, the results are compared with the exact long wave solution of the Orr–Sommerfeld equations for the two-plate geometry. It is demonstrated that with the shape factors corrections and the inclusion of wave induced stresses effects, the TF model is able to fully reproduce the exact long wave neutral stability curves. The wave induced shear stresses in phase with the wave slope, which give rise to the so called "sheltering force", were found to have a remarkable destabilizing effect in many cases of horizontal and inclined flows. In such cases, the sheltering effects must be included in the TF model, otherwise the region of smooth stratified flow would be significantly over predicted. Based on the results of the exact analysis, a simple closure relation for the sheltering term in the TF model is provided.