TY - JOUR
T1 - Absolute linear instability in laminar and turbulent gas-liquid two-layer channel flow
AU - Náraigh, L. Ó
AU - Spelt, P. D.M.
AU - Shaw, S. J.
PY - 2013/1/10
Y1 - 2013/1/10
N2 - We study two-phase stratified flow where the bottom layer is a thin laminar liquid and the upper layer is a fully developed gas flow. The gas flow can be laminar or turbulent. To determine the boundary between convective and absolute instability, we use Orr-Sommerfeld stability theory, and a combination of linear modal analysis and ray analysis. For turbulent gas flow, and for the density ratio r= 1000, we find large regions of parameter space that produce absolute instability. These parameter regimes involve viscosity ratios of direct relevance to oil and gas flows. If, instead, the gas layer is laminar, absolute instability persists for the density ratio r= 1000, although the convective/absolute stability boundary occurs at a viscosity ratio that is an order of magnitude smaller than in the turbulent case. Two further unstable temporal modes exist in both the laminar and the turbulent cases, one of which can exclude absolute instability. We compare our results with an experimentally determined flow-regime map, and discuss the potential application of the present method to nonlinear analyses.
AB - We study two-phase stratified flow where the bottom layer is a thin laminar liquid and the upper layer is a fully developed gas flow. The gas flow can be laminar or turbulent. To determine the boundary between convective and absolute instability, we use Orr-Sommerfeld stability theory, and a combination of linear modal analysis and ray analysis. For turbulent gas flow, and for the density ratio r= 1000, we find large regions of parameter space that produce absolute instability. These parameter regimes involve viscosity ratios of direct relevance to oil and gas flows. If, instead, the gas layer is laminar, absolute instability persists for the density ratio r= 1000, although the convective/absolute stability boundary occurs at a viscosity ratio that is an order of magnitude smaller than in the turbulent case. Two further unstable temporal modes exist in both the laminar and the turbulent cases, one of which can exclude absolute instability. We compare our results with an experimentally determined flow-regime map, and discuss the potential application of the present method to nonlinear analyses.
KW - absolute/convective instability
KW - instability
KW - interfacial flows (free surface)
UR - http://www.scopus.com/inward/record.url?scp=84871882883&partnerID=8YFLogxK
U2 - 10.1017/jfm.2012.452
DO - 10.1017/jfm.2012.452
M3 - Article
AN - SCOPUS:84871882883
SN - 0022-1120
VL - 714
SP - 58
EP - 94
JO - Journal of Fluid Mechanics
JF - Journal of Fluid Mechanics
ER -