pdf, 12 MiB - Infoscience - EPFL
pdf, 12 MiB - Infoscience - EPFL
pdf, 12 MiB - Infoscience - EPFL
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
Analysis of the sediment transport<br />
The higher discharges (Figure 6.17 center and bottom) show an almost constant transport rate<br />
(a slightly decreasing tendency can be figured out for the case without macro-roughness). This is<br />
mainly due to the circumstance that the tests were performed as a series with increasing discharge.<br />
The bed was only levelled after the first test (Q = 150 l/s). The next tests continued with the bed<br />
topography of the previous test. Since the discharges were high enough to provoke bed changes<br />
this was no problem, but as far as the sediment transport is concerned, the bed was already<br />
armored; therefore the sediments introduced at the inlet were transported over the armoring layer<br />
to the outlet.<br />
In the presence of macro-roughness, a natural river, subject to a constant sediment transport rate<br />
will compensate the reduced transport capacity in the bend by steepening the slope in the bend:<br />
Upstream the bend, the water depth increases locally. Therefore the transport capacity is reduced<br />
and sediments accumulate in the inlet reach. The overall channel slope increases, till it is sufficient<br />
to pass the bedload across the bend. The increased slope leads to higher velocities in the exit<br />
reach, inducing some additional erosion after the curve.<br />
This phenomenon was observed during the preliminary tests, for which the sediment transport<br />
rate was kept constant (Figure 6.18 and Appendix 3.3.3). For a discharge of 170 l/s respectively<br />
210 l/s the overall bed slope increased by about 40%, respectively 50% from the initial value<br />
(0.50%).<br />
Difference to initial bed level [mm]<br />
100<br />
0<br />
-100<br />
-200<br />
-300<br />
-400<br />
Comparison of the bed levels with and without macro-roughness - Q = 2<strong>12</strong>.5 l/s<br />
Q=2<strong>12</strong>.5 l/s without mr, avg<br />
Q=2<strong>12</strong>.5 l/s with mr, avg<br />
Q=2<strong>12</strong>.5 l/s, Difference, avg<br />
Bend<br />
-500<br />
-100<br />
0 5 10 15 20 25<br />
Distance to the inlet [m]<br />
Figure 6.18: Changes of the average bed level for the preliminary tests (with and without ribs) at a constant sediment<br />
transport rate<br />
500<br />
400<br />
300<br />
200<br />
100<br />
0<br />
Difference between without / with mr<br />
[mm]<br />
<strong>EPFL</strong> Ph.D thesis 2632 - Daniel S. Hersberger November 9, 2002 / page 133