UFR 2-10 Evaluation

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Evaluation

A detailed comparison of the LES with the test case experiment is provided in Palau-Salvador et al (2010) and here only the main findings are reproduced. Fig. 5 shows contours of the mean streamwise velocity together with streamlines in the centre plane for both the shorter and the longer cylinder. Near the cylinder walls, LDV measurements could not be carried out so that there is a blanked out region in the experimental part of the figure. Overall, the contours of velocity and the streamlines show good agreement between LES and experiments, even though the length of recirculation behind the cylinder is slightly overpredicted for the long cylinder case. The core of the recirculation is located much closer to the cylinder in the long cylinder case and could not be resolved in the experiment. A more direct quantitative comparison of results is provided below in terms of profiles in Figures 8 – 10. Fig. 6 compares contours of the streamwise and vertical fluctuations in the longitudinal centre plane for both cases. The main features are again predicted quite well, at least qualitatively (for quantitative comparison see Figs. 8 and 9) and this includes the differences between the two cases and between streamwise and vertical fluctuations.


Figure 5. Time-average streamlines and contours of mean velocity components <u> in the centre plane y/D=0, from Palau-Salvador et al (2010)


Fig. 7 provides contours of streamwise velocity and steamlines in two wall-parallel planes, one near the mid-height of the cylinder (z/h = 0.6) and the other near the free-end (z/h = 0.8). Unfortunately, measurements closer to the ground plate are not available. Near mid-height, the streamlines show the typical picture of the flow around a circular cylinder. As could be imagined from the shape of the reverse flow region in Fig. 5, the separation bubble length reduces significantly with distance from the ground and at z/h = 0.6 it is already considerably smaller than the reattachment length. Near the free-end (z/h = 0.8) a fairly clear bubble still exists for the long cylinder case, but the bubble length is reduced even more. The effects of the free-end are clearly present already and they are much stronger for the short cylinder case. Here the end effects distort the bubble in the horizontal plane and make it much smaller. All these features are predicted by the LES in fairly good agreement with the experiments.

To allow better quantitative comparison between LES and measurements, several profiles are presented in Figs. 8 to 10. Fig. 8 shows profiles of mean and fluctuating streamwise and vertical velocities along the lines at z = 0.2h and z = 0.6h on the centre plane for both cylinder cases. The velocity profiles show that the deceleration in front of the cylinder, then behind the cylinder the reverse flow region and the recovery of the velocity and the wake. On the whole the agreement between LES and measurements is again good, in particular with respect to the differences in reverse flow between the two heights considered and the two cylinders. At z/h = 0.6, a strong upflow is present near the wall of the short cylinder which is well predicted. For the long cylinder this upflow is weaker and as mentioned already could not be resolved in the measurements. It follows a strong downwash which reaches its maximum at x/D ≈ 2 and subsequently reduces further downstream. All this, and also the behaviour of the streamwise and vertical fluctuations are quite well predicted by the LES. Fig. 9 compares vertical distributions of the same quantities in the centre plane at x/D = 1. Over the entire height from the ground plate to the free stream the agreement is generally quite good with only local deviations and the differences between the two cases are overall well predicted. Profiles along the lateral direction y of means streamwise and lateral velocities and corresponding turbulent fluctuations at about mid-height (z/h = 0.6) and the downstream distance of x/D = 1.5 are shown in Fig. 10. Again, the behaviour of mean and fluctuating velocities is quite well simulated by the LES.


UFR2-10 figure 6a.png
Figure 6. Root mean square of the streamwise (u′) and vertical (w′) fluctuations in the centre plane y/D=0, from Palau-Salvador et al (2010)





Contributed by: Guillermo Palau-Salvador, Wolfgang Rodi, — Universidad Politecnica de Valencia, Karlsruhe Institute of Technology


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