On the stability of thermally driven shear flow of an Oldroyd-B fluid heated from below

DOI10.1016/S0377-0257(02)00143-XzbMath1022.76017OpenAlexW2049775600MaRDI QIDQ1811691

Yanyan Li

Publication date: 17 June 2003

Published in: Journal of Non-Newtonian Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/s0377-0257(02)00143-x

zbMATH Keywords

convectionOldroyd-B fluideigenvalue problemlinear stability analysisinclined temperature gradienthorizontal temperature gradientlateral heatingChebyshev Tau-QZ methodhorizontal Rayleigh numbershallow horizontal layervertical Rayleigh number

Mathematics Subject Classification ID

Viscoelastic fluids (76A10) Convection in hydrodynamic stability (76E06)

Related Items (3)

Linear and nonlinear stability analyses of thermal convection for Oldroyd-B fluids in porous media heated from below ⋮ Linear and weakly nonlinear analysis of a ferrofluid layer for an LTNE model with variable gravity and internal heat source ⋮ Bio‐thermal convection caused by combined effects of swimming of oxytactic bacteria and inclined temperature gradient in a shallow fluid layer

This page was built for publication: On the stability of thermally driven shear flow of an Oldroyd-B fluid heated from below