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Appendix P Drainage, Flooding, Stormwater Management Part 5

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<strong>Flooding</strong>, <strong>Drainage</strong> and <strong>Stormwater</strong> <strong>Management</strong><br />

Sanctuary Villages<br />

Details of XP-RAFTS developed model catchment data are summarised in <strong>Appendix</strong> B.<br />

Node locations used in the XP-RAFTS developed model are identical to those for the<br />

existing model and are shown in Figure 3.<br />

The percentage of impervious area for the development site has been adopted as 60%.<br />

This value has been adopted to represent the relative contribution of various land types<br />

including; road reserves, commercial, residential and parkland. This assumption is valid<br />

for a regional level study but a more detailed breakdown of land use will be considered at<br />

the local strategy level.<br />

3.2.3 Developed peak discharges<br />

Predicted developed flow rates within Congewai Creek at Millfield Bridge for the 1, 5, 10,<br />

20, 50 and 100 year ARI storm events are summarised in Table 3-4. Also shown are<br />

existing peak flow rates at this location and the percentage change in flow resulting from<br />

development. Runoff hydrographs for the critical duration storm that produced the largest<br />

peak flow estimate are provided in <strong>Appendix</strong> E for developed conditions. The critical<br />

storm duration that produced the peak flow rate at node CON.15 was the 720 minute<br />

storm for the 1 year ARI event and 2160 minute storm for all other events.<br />

Table 3-4: Developed peak flow estimates within Congewai Creek at Millfield Bridge (Node<br />

CON.15)<br />

ARI<br />

Existing Peak Flow<br />

Rate (m 3 /s)<br />

Developed Peak<br />

Flow Rate (m 3 /s)<br />

Percentage Change<br />

1 Year 62 62 0%<br />

5 Year 221 221 0%<br />

10 Year 296 295 -0.3%<br />

20 Year 392 391 -0.2%<br />

50 Year 571 571 0%<br />

100 Year 762 761 -0.1%<br />

Table 3-4 illustrates that the proposed development results in a negligible change in the<br />

critical duration peak flow rate at Millfield Bridge for the 1, 5, 10, 20, 50 and 100 year ARI<br />

storm events.<br />

Examination of Figure 3 shows the proposed development area to be located near the<br />

outlet of the analysed catchment, which extends as far as Millfield Bridge. The<br />

introduction of impervious surfaces at this location increases the rate of runoff from the<br />

lower portions of the catchment allowing runoff to enter Congewai Creek before the<br />

overall catchment flood peak. This is further supported by examination of the developed<br />

runoff hydrograph for the 1 year critical duration storm event contained within <strong>Appendix</strong><br />

E, which shows a small spike on the rising limb of the hydrograph when compared to the<br />

existing runoff hydrograph at this location.<br />

A comparison of existing and developed peak flow rates for the 1, 10 and 100 ARI storm<br />

events run for a range of storm durations is shown in Figure 5. Examination of Figure 5<br />

reveals negligible change in peak flow rate for the 10 and 100 year ARI storm events at<br />

Millfield Bridge for all storm durations. However, there is a minor increase in peak flow<br />

rate for the shorter duration 1 year ARI storm events. This increase in flow rate will<br />

require detention storage to reduce the potential for scour of existing drainage lines.<br />

PARSONS BRINCKERHOFF 2122870A-PR0116 Page 13

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