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

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stable test case, the computed three-dimensional structures are weaker. In con-<br />

trast to the experimental evidence, the time-dependent three-dimensional k-ε-<br />

AWF simulations returned a mainly stable and largely two-dimensional flow<br />

field. With the introduction <strong>of</strong> the RSM model, on the other hand, the time-<br />

dependent RANS are able to reproduce the three-dimensional flow features,<br />

though not to the same degree as the experimental data. <strong>The</strong> Nu variation pre-<br />

dicted by the RSM is in reasonable agreement with the measurements in terms<br />

<strong>of</strong> the Nu levels and variations, while the EVM returned the correct levels for<br />

the Nusselt number, but not the correct variation.<br />

<strong>The</strong> horizontal annular penetration case involves a horizontal annular pas-<br />

sage, closed at one end, with the inner core maintained at a lower temperature.<br />

<strong>The</strong> inner core cools the fluid around it, which makes it heavier. <strong>The</strong> heavier<br />

fluid drops out <strong>of</strong> the penetration, from the open end, and new warm fluid<br />

enters to take its place. In the lower Ra case, the time-dependent simulation<br />

showed that downward flow which separates from the cold tube was not uni-<br />

form all along the tube and over most <strong>of</strong> the penetration there were strong<br />

oscillations. In the higher Ra case, the contours <strong>of</strong> the instantaneous vertical<br />

velocity, in common with those at the lower Rayleigh number, showed flow<br />

oscillations within the penetration, but with smaller amplitude.<br />

26

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