The influence of fluid elasticity on the onset and stability of axisym
metric Taylor vortices is examined for the Taylor-Couette flow of an O
ldroyd-B fluid. A truncated Fourier representation of the how field an
d stress leads to a six-dimensional dynamical system that generalizes
the three-dimensional system for a Newtonian fluid. The coherence of t
he model is established through comparison with existing linear stabil
ity analyses and finite-element calculations of the nonlinear dynamics
of the transition to time-periodic (finite-amplitude) flow. The stabi
lity picture and flow are drastically altered by the presence of the n
onlinear (upper convective) terms in the constitutive equation. It is
found that the critical Reynolds number Re-c at the onset of Taylor vo
rtices decreases with increasing fluid elasticity or normal stress eff
ects, and; is strongly influenced by fluid retardation. For weakly ela
stic flows, there is an exchange of stability at Re=Re-c through a sup
ercritical bifurcation, similar to the one predicted by the Newtonian
model. As the elasticity number exceeds a critical value, a subcritica
l bifurcation emerges at Re, similar to the one predicted by the Landa
u-Ginzburg equation. More importantly, it is shown that, if fluid elas
ticity is adequately accounted for, any small but nonvanishing amount
of fluid elasticity can lead to the onset of chaos usually observed in
experiments on the Taylor-Couette flow of supposedly Newtonian fluids
. This is in sharp contrast to the Newtonian model, which does not pre
dict the destabilization of the Taylor vortices, and therefore cannot
account for the onset of periodic and chaotic motion. (C) 1995 America
n Institute of Physics.