It is then possible to add the effects of that non-trivial local dynamic
to turbulent mixing. We select the model of Sect. 5.
In order to study the influence of the turbulence, we again do a comparison
between a turbulent and a Gaussian velocity field (Fig. 13
for one example). Note that A, B (chemical species),
U (internal energy) and R (proportional to the total
density) are advected as described by Eq. (11) extended
to 4 variables.
![]() |
Figure 13:
Density of component ![]() |
![]() |
Figure 14:
Density of components ![]() ![]() |
We can observe that, as in the previous case (Sect. 4.3), structures appear naturally at all scales in the turbulent case and not with a Gaussian velocity field. Appendix D shows the variations of A on a much larger time scale. Different initial conditions give indistinguishable results, suggesting that steady state is reached. However, we cannot exclude that some long time drift may still exist which our computation is unable to uncover.
Turbulent structures are not the same for the different components
(A, B, R) neither in position nor in size, as
can be seen in Fig. 14, which is an horizontal
cut of Fig. 13. In order to study more precisely
these effects, we plot the probability density function of A(Fig. 15) which should be compared to Fig 8.
![]() |
Figure 15:
Probability density function of ![]() |
Note that the presence of a non-uniform velocity field leads to a single-peaked broad distribution. Turbulence leads to a broader distribution and extended wings. Thus the probability to find some regions at far from equilibrium values is enhanced.
We also plotted the density of
as a function of size (see Fig. 16) using the same
procedure as for Fig. 9. The slope is
(instead of
for the total density, cf. Sect. 4.3).
The evolution through scales is therefore significantly different
for one particular component and for the total density.
Copyright ESO 2002