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Traitement et analyse de séries chronologiques continues de ...

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Annexes<br />

a<br />

b<br />

c<br />

1500<br />

TSS (kg)<br />

COD (kg)<br />

d<br />

Event loads (kg)<br />

1000<br />

500<br />

0<br />

1 2 3 4 5 6 7 8 9 1011 12 1314 1516 17 1819 2021 22 2324 25 2627 2829 30 3132 33<br />

Event number<br />

Figure 2. Example of results for the Chassieu catchment: (a) validation graphical user interface for water level<br />

and turbidity time series from 1 - 20 January 2008, (b) Turbidity-TSS and (c) Turbidity-COD correlation<br />

functions, (d) TSS (in black) and COD (in white) event loads in 2005 with 95 % confi<strong>de</strong>nce intervals.<br />

In 2005, 33 storm events have been monitored in Chassieu. For each event, TSS and COD event loads<br />

have been calculated, with their 95 % confi<strong>de</strong>nce intervals. The results are shown in Figure 2d: black<br />

and white thick bars represent respectively the TSS and COD loads for the 33 events. Each thick bar is<br />

compl<strong>et</strong>ed with a vertical thin bar segment representing the 95 % confi<strong>de</strong>nce interval of the event load.<br />

The variability of the event loads is very significant, with values ranging typically from a few to 400-<br />

500 kg of TSS or COD per event. The event number 25 shows extremely high loads compared to all<br />

the other ones. A further analysis of these 33 events loads (results not shown here) has indicated that<br />

there was no correlation b<strong>et</strong>ween events loads and basic event characteristics like rainfall duration,<br />

intensity, antece<strong>de</strong>nt dry weather period or rainfall r<strong>et</strong>urn period.

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