Environmental Engineering Reference
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Fig. 6 Variation of average
fl
flame length with increase in Reynolds number
Fig. 7 Comparison of turbulent kinetic energy spectra at x/h = 4 for Re = 18,000 and 33,000
shows the turbulent kinetic energy (TKE) spectra for these cases. It is clearly seen
that TKE is higher in large scales for Re = 33,000 when compared to 18000. Also,
there is a sharp decrease in TKE in small scales for Re = 33,000 relative to 18,000.
This reveals that the large scales are being formed at the expense of small scales at
Re = 33,000, bringing out evidence for the ARS to churn these large-scale struc-
tures. The ARS reorganises the
field into large-scale coherent structures and
prevents their decay into small scales, as observed in experiments.
fl
ow
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