THE CENTER FOR NONLINEAR STUDIES | ||
PROGRAM |
||
Tuesday May 23, 2000 1:00pm-2:00pm |
Lecture I: Turbulent Heat Transport in Fluids Heated from
Below One
of the central issues in turbulent convection of a fluid heated from below
has been the global heat transport, as expressed by the Nusselt number
A number of theoretical models have predicted powerlaw relations between N
and
the Rayleigh number R.
New
high precision measurements will be discussed which show that simple
powerlaws are not adequate for this purpose. On the other hand, a model
recently proposed by Grossmann and Lohse (GL) and based on the
decomposition of the kinetic and the thermal dissipation into boundary-layer
and bulk contributions gives an excellent fit to the R-dependence.
Unfortunately, the Prandtl-number dependence, which is given as well by
the GL model, does not agree with experiment.
|
|
Tuesday May 23, 2000
|
Lecture II: Pattern Formation near Onset of Rayleigh-Benard Convection: Some Simple Unexplained Results. Although
much is known about pattern formation in nonlinear dissipative systems,
there are several seemingly simple experimentally observed phenomena which
either remain unexplained, or on which experiment and theory disagree.
This is so even near the threshold of pattern formation where weakly
nonlinear theories should be applicable. This talk will discuss a number
of studies of pattern formation under carefully controlled conditions near
the onset of convection in a shallow horizontal layer of a fluid heated
from below (Rayleigh-Benard convection). Issues to be addressed will
include wavenumber selection near onset, the effect of a Coriolis force on
pattern formation, and convection with rotation at small Prandtl numbers. |
|
Wednesday May 24, 2000 10:00am-11:00am |
Lecture III: Critical Phenomena near Bifurcations in Systems far from
Equilibrium In
spatially-extended nonlinear dissipative systems far from equilibrium,
bifurcations are usually discussed in terms of deterministic equations for
the macroscopic variables which neglect the "microscopic"
degrees of freedom. An example is the use of the NavierStokes equation for
Rayleigh-Benard convection (RBC). There is then a sharp bifurcation point R=Rc
at which an exchange of stability occurs between the spatially-uniform
state and the state with spatial variation.
|
|
Refreshments Will Be Served Following Each Lecture |
||