Abstract :
This paper answers some recent questions posed by heat propagation
mechanisms in near-supercritical pure fluids under normal gravity conditions.
The role of microgravity experiments in the discovery of a fourth temperature
equilibration mode in hypercompressible fluids, called the piston effect, is
described, as well as its basic mechanisms that are responsible for temperature
equilibration on a much shorter time scale than heat diffusion. The question
whether this mechanism still exists on the ground is then approached. The
results of the numerical calculations which answer this question and the basic
references are preseInted. It is emphasized, in particular, that, although the
piston effect has been demonstrated by microgravity experiments, this effect
appears to be the temperature equilibrating mechanism on ground, also leading
to the striking evidence of a quasi-isothermal convection. Recent modeling in
connection with experiments that suggested that the piston effect could be killed
by convection shows, on the contrary, that a cooling piston effect, triggered by
thermal plumes, prevents the bulk increase in temperature.
Keywords :
Finite volume methods , Convection , supercritical fluids. , hypercompressible fluids , Numerical Hydrodynamics , piston effect