4.5 Article

Interfacial instability in turbulent flow over a liquid film in a channel

期刊

INTERNATIONAL JOURNAL OF MULTIPHASE FLOW
卷 37, 期 7, 页码 812-830

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ijmultiphaseflow.2011.02.010

关键词

Interfacial instability; Turbulence; Two-phase flow

资金

  1. EPSRC [EP/E021468/1, EP/F009194/1] Funding Source: UKRI
  2. Engineering and Physical Sciences Research Council [EP/E021468/1, EP/F009194/1] Funding Source: researchfish

向作者/读者索取更多资源

We revisit the stability of a deformable interface that separates a fully-developed turbulent gas flow from a thin layer of laminar liquid. Although this problem has received considerable attention previously, a model that requires no fitting parameters and that uses a base-state profile that has been validated against experiments is, as yet, unavailable. Furthermore, the significance of wave-induced perturbations in turbulent stresses remains unclear. To address these outstanding issues, we investigate this problem and introduce a turbulent base-state velocity that requires specification of a flow rate or a pressure drop only; no adjustable parameters are necessary. This base state is validated extensively against available experimental data as well as the results of direct numerical simulations. In addition, the effect of perturbations in the turbulent stress distributions is investigated, and demonstrated to be small for cases wherein the liquid layer is thin. The detailed modelling of the liquid layer also elicits two unstable modes, 'interfacial' and 'internal', with the former being the more dominant of the two. We show that it is possible for interfacial roughness to reduce the growth rate of the interfacial mode in relation to that of the internal one, promoting the latter, to the status of most dangerous mode. Additionally, we introduce an approximate measure to distinguish between 'slow' and 'fast' waves, the latter being the case for 'critical-layer'-induced instabilities; we demonstrate that for the parameter ranges studied, the large majority of the waves are 'slow'. Finally, comparisons of our linear stability predictions are made with experimental data in terms of critical parameters for onset of wave-formation, wave speeds and wavelengths; these yield agreement within the bounds of experimental error. (c) 2011 Elsevier Ltd. All rights reserved.

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