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FLOW AROUND A CYLINDER - istiarto

FLOW AROUND A CYLINDER - istiarto

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– 5.19 –<br />

Fig. 5.9 Definition sketch of the coordinate system and the vorticity, ��.<br />

5.5.3 Results of the simulation and comparison to the experimental data<br />

The evaluation of the results of the numerical simulation (see Chapter 4) is made for the<br />

velocity fields and the water surface. Herewith they are compared to the experimental<br />

data (see Chapter 2). Detailed comparison of the 3D velocity profiles in the planes where<br />

the experimental data are available is first presented (Fig. 5.10). The velocity fields,<br />

resulted from the simulation and the measurement, are then presented by vector plots<br />

(Fig. 5.11) and contour plots (Fig. 5.12) in three selected planes, � = 0°, 90°, and 180°, to<br />

show the general pattern of the flow. Next, the prediction of the flow pattern at the<br />

bottom corner of the cylinder is highlighted by contour plots of the computed and the<br />

measured vorticity fields (Fig. 5.13), obtainable from the corresponding 2D velocity<br />

components in those three planes. Finally, an evaluation is made on the computed water<br />

surface profile along the longitudinal section of the symmetry plane and along the<br />

cylinder circumference (Fig. 5.14).�<br />

Vertical distribution of the 3D velocity components<br />

The comparison between the computed and the measured vertical distributions of the 3D<br />

velocity components are done for some selected profiles. Shown in Fig. 5.10 are 20<br />

distributions of the 3D velocity components, u(z), v(z), and w(z), in the planes where<br />

measurements data are available, � = 0°, 45°, 90°, 157.5°, and 180°. Four stations at<br />

r D p � 1.5, 1, 0.75, and 0.55, being considered representative ones, are selected from<br />

each plane. It can be seen from the comparison in Fig. 5.10 that the computed velocity<br />

distributions are in a good agreement with the measured ones, notably in the upstream<br />

region, � = 0°, 45°, and 90°. The agreement, however, is less evident in the wake region,

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