Direct numerical simulations of passive scalars with Pr>1 advected by turbulent flow
Direct numerical simulations of passive scalars, with Prandtl numbers Pr=3, 5, and 7, advected by turbulence at three low Reynolds numbers were performed. The energy spectra are self-similar under the Kolmogorov scaling and exhibit behaviour consistent with many other investigations: a short inertia...
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Veröffentlicht in: | Journal of fluid mechanics 1997-07, Vol.343, p.111-130 |
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Sprache: | eng |
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Zusammenfassung: | Direct numerical simulations of passive scalars, with Prandtl numbers
Pr=3, 5, and
7, advected by turbulence at three low Reynolds numbers were performed.
The energy
spectra are self-similar under the Kolmogorov scaling and
exhibit behaviour consistent
with many other investigations: a short inertial range for the
highest Reynolds number
and the universal exponential form of the spectrum for all Reynolds numbers
in the
dissipation range. In all cases the passive scalar spectra
collapse to a single self-similar curve under the Batchelor scaling and
exhibit the k−1 range followed by an
exponential fall-off. We attribute the applicability of the Batchelor scaling
to our
low-Reynolds-number flows to the universality of the energy dissipation
spectra. The
Batchelor range is observed for wavenumbers in general agreement with experimental
observations but smaller than predicted by the classical estimates. The
discrepancy
is caused by the fact that the velocity scales responsible for the generation
of the
Batchelor range are in the vicinity of the wavenumber of the maximum energy
dissipation, which is one order of magnitude less than the Kolmogorov wavenumber
used in the classical theory. Two different functional forms of
passive scalar spectra
proposed by Batchelor and Kraichnan were fitted to the simulation results
and it was
found that the Kraichnan model agrees very well with the data while the
Batchelor
formula displays systematic deviations from the data.
Implications of these differences
for the experimental procedures to measure the energy and passive scalar
dissipation
rates in oceanographic flows are discussed. |
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ISSN: | 0022-1120 1469-7645 |
DOI: | 10.1017/S0022112097005727 |