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The computation of turbulent natural convection flows - Turbulence ...

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299<br />

active sides, y-z, there are recirculation cells similar to those discussed in the<br />

previous section.<br />

Figures 7.89,7.94,7.95,7.96 and 7.97 show the temperature distributions within<br />

a number <strong>of</strong> longitudinal planes. <strong>The</strong>se comparisons reveal that the imple-<br />

mentation <strong>of</strong> <strong>turbulent</strong> viscosity limit does not make significant changes to the<br />

temperature pr<strong>of</strong>iles. <strong>The</strong>re are only slight changes near the top and bottom <strong>of</strong><br />

the cavity. Figures 7.90, 7.98, 7.99 present the corresponding longitudinal ve-<br />

locity distributions within longitudinal, x-y, planes and Figures 7.102 and 7.103<br />

the distribution <strong>of</strong> the longitudinal and normal velocities within the mid-plane<br />

plane parallel to the thermally active sides, x-z plane at Y=0.5. <strong>The</strong> compar-<br />

isons show that introduction <strong>of</strong> the viscosity limiter, in addition to enabling<br />

the k-ε-AWF to return unstable flow conditions, leads to some improvements<br />

in the predicted time-averaged velocity field, but there still large deviations be-<br />

tween the predicted and measured flow fields. Figures 7.92, 7.93, 7.100, 7.101,<br />

7.104 and 7.105 show the corresponding comparisons for the corresponding<br />

rms velocity pr<strong>of</strong>iles. Improvements in the predicted rms are evident, most<br />

notably near the end walls, where the predicted levels are now significantly<br />

higher than those <strong>of</strong> k-ε-AWF predictions without the viscosity limiter, and<br />

close to the measured values. <strong>The</strong>se predictive improvements are most likely<br />

to result from the fact that the predicted rms velocities now include both the<br />

modelled component from the solution <strong>of</strong> the transport equation for k, which<br />

represents the contribution <strong>of</strong> the small-scale motion, and the resolved compo-<br />

nent, obtained by post processing the instantaneous velocity and which rep-<br />

resents the contribution <strong>of</strong> the large-scale unsteady motion. This is consistent<br />

with the fact that the largest improvements in the predicted rms velocity field<br />

is observed near the two end walls, where the predicted flow is most unsta-<br />

ble. Finally in Figure 7.106, the time-averaged longitudinal distributions <strong>of</strong><br />

the Nusselt number at four spanwise locations, Z=0.5, 0.625, 0.75, 0.865, pre-<br />

dicted by the k-ε-AWF, are compared to the measured data. At all spanwise<br />

locations, the low Nu levels near the bottom end wall are under estimated, the<br />

higher levels near the top end wall are well predicted, but the predicted longi-<br />

tudinal variation in local Nusselt number from the bottom to the top end wall<br />

is non-monotonic. <strong>The</strong> local Nusselt number rises from zero at the bottom end

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