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– 2.58 –<br />
As the flow advances to the downstream passing the scour hole, the intensity of the<br />
turbulence gets stronger. The increase of the turbulence level is notably noticeable from<br />
the plane � = 90° to � = 135°. This increase continues, but with diminishing rate, in the<br />
plane � = 180°. In this downstream plane, the turbulence demonstrates its peak intensity.<br />
It is interesting to observe that, in this plane, the three components of the intensity,<br />
u �� u ��,<br />
v �� v �� and w ��w<br />
��,<br />
indicate a tendency of being isotropic. Observing the intensity<br />
of the turbulence in each plane, one can notice that, approaching the cylinder, the<br />
turbulence inside the scour hole intensifies. In the upper layer, on the other hand, the<br />
turbulence level remains more or less constant.<br />
Approaching the cylinder, in all planes except in the plane � = 180°, the turbulence<br />
intensifies within the scour hole, z < 0, but remains more or less unchanged outside the<br />
scour hole, z > 0. Downstream of the cylinder, in the plane � = 180°, the turbulence gets<br />
its strongest intensities.�<br />
The Reynolds shear-stresses inside the scour hole gets increasingly stronger as the flow<br />
moves towards downstream from the plane � = 0° to � = 135°. In the plane � = 135°, the<br />
stresses are about 3 times higher than those in the plane � = 0°. In the upper layers, z > 0,<br />
the profiles of the Reynolds stresses exhibit a nearly linear distribution. Underneath,<br />
z ≤ 0, the profiles of the Reynolds stresses turn towards a strong peak. In all planes, the<br />
�u �� w �� is always dominant compared to the �v �� w ��.<br />
Downstream of the cylinder,<br />
� = 180°, the vertical distributions of the Reynolds stresses do not show any conclusive<br />
trend.�<br />
References<br />
Cellino, M. (1998). Experimental study of suspension flow in open channels., Doctoral<br />
Dissertation, No. 1824, EPFL, Lausanne, Switzerland.<br />
Graf, W. H., and Altinakar, M. S. (1996). Hydraulique Fluviale, Tome 2., P.P.U.R.,<br />
Lausanne, Switzerland.<br />
Graf, W. H., and Altinakar, M. S. (1998). Fluvial Hydraulics., John Wiley & Sons, Ltd.,<br />
Chichester, England.<br />
Hurther, D., Lemmin, U., and Arditi, M. (1996). ―Using an annular curved array<br />
transducer for bistatic ADVP application.‖ Rapport Annuel, Laboratoire de<br />
recherches hydrauliques, EPFL, 1996, B.201.1-B.201.19.<br />
Kironoto, B. A., and Graf, W. H. (1994). ―Turbulence characteristics in rough uniform<br />
open-channel flow.‖ Proc. Instn. Civ. Engrs. Wat., Marit. & Energy, 106, 333-344.<br />
Lhermitte, R., and Lemmin, U. (1994). ―Open-channel flow and turbulence measurement<br />
by high-resolution Doppler sonar.‖ J. Atm. Ocean. Tech., 11, 1295-1308.<br />
Nezu, I., and Nakagawa, H. (1993). Turbulence in open-channel flows., A.A. Balkema,<br />
Rotterdam, NL.