Ab. Cortesi et al., Numerical investigation of the entrainment and mixing processes in neutraland stably-stratified mixing layers, PHYS FLUIDS, 11(1), 1999, pp. 162-185
The direct numerical simulation (DNS) of a temporally-growing mixing layer
has been carried out, for a variety of initial conditions at various Richar
dson and Prandtl numbers, by means of a pseudo-spectral technique; the main
objective being to elucidate how the entrainment and mixing processes in m
ixing-layer turbulence are altered under the combined influence of stable s
tratification and thermal conductivity. Stratification is seen to significa
ntly modify the way by which entrainment and mixing occur by introducing hi
ghly-localized, convective instabilities, which in turn cause a substantial
ly different three-dimensionalization of the flow compared to the unstratif
ied situation. Fluid which was able to cross the braid region mainly undist
urbed (unmixed) in the unstratified case, pumped by the action of rib pairs
and giving rise to well-formed mushroom structures, is not available with
stratified how. This is because of the large number of ribs which efficient
ly mix the fluid crossing the braid region. More efficient entrainment and
mixing has been noticed for high PrandtI number computations, where vortici
ty is significantly reinforced by the baroclinic torque. In liquid sodium,
however, for which the Prandtl number is very low, the generation of vortic
ity is very effectively suppressed by the large thermal conduction, since o
nly small temperature gradients, and thus negligible baroclinic vorticity r
einforcement, are then available to counterbalance the effects of buoyancy.
This is then reflected in less efficient entrainment and mixing. The influ
ence of the stratification and the thermal conductivity can also be clearly
identified from the calculated entrainment coefficients and turbulent Pran
dtl numbers, which were seen to accurately match experimental data. The tur
bulent Prandtl number increases rapidly with increasing stratification in l
iquid sodium, whereas for air and water the stratification effect is less s
ignificant. A general law for the entrainment coefficient as a function of
the Richardson and Prandtl numbers is proposed, and critically assessed aga
inst experimental data. (C) 1999 American Institute of Physics. [S1070-6631
(99)01201-5].