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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 />

Existing peak discharges at Millfield Bridge for the 5 and 20 year ARI storm events are<br />

generally in close agreement with estimates documented in the Wollombi Valley Flood<br />

Study prepared by Patterson Britton and <strong>Part</strong>ners (April 2004). The predicted 100 year<br />

discharge is 17% larger than that documented by PBP. This may be due to variations in<br />

the height-storage-discharge relationship adopted by both Consultants.<br />

A summary of existing peak discharges, peak storage and peak water level at Ellalong<br />

Lagoon (node QUO.7) for the 1, 5, 10, 20, 50 and 100 year ARI storm event is provided<br />

in Table 3-3, and will be used as a baseline comparison for evaluating the impacts of the<br />

development on existing flow rates, as well as for estimating the 100 year ARI flood levels<br />

within the study area.<br />

Table 3-3:<br />

ARI<br />

Existing peak discharge, peak storage and peak water level in Ellalong Lagoon<br />

Existing Peak<br />

Discharge (m 3 /s)<br />

Critical Storm<br />

Duration (min)<br />

Peak Storage<br />

(ML)<br />

Peak Water Level<br />

(m AHD)<br />

1 Year 16 720 473 111.23<br />

5 Year 64 2160 1,560 112.35<br />

10 Year 80 2160 1,560 112.84<br />

20 Year 141 2160 2,820 113.34<br />

50 Year 231 2160 3,030 113.51<br />

100 Year 305 2160 3,160 113.62<br />

3.2 Developed hydrology<br />

3.2.1 Potential hydrological impacts of development<br />

Urban development typically results in an increase in the impervious surfaces within a<br />

catchment and engineering works to collect and convey runoff. Without appropriate<br />

management, several potential impacts result from development. These could include:<br />

<br />

<br />

<br />

increased frequency of runoff events;<br />

increased runoff volume, peak flow and velocity; and<br />

decreased groundwater base flows and lowering of the watertable.<br />

These impacts may in turn lead to:<br />

<br />

<br />

<br />

<br />

inundation of downstream property and infrastructure;<br />

change in existing channel form and sediment transport;<br />

damage to riparian and aquatic vegetation; and<br />

damage to existing aquatic ecosystems and natural wetlands.<br />

3.2.2 Model parameters<br />

The effect of urbanisation, of the proposed development site, was modelled using XP-<br />

RAFTS and involved the inclusion of impervious areas within the existing model. The<br />

model was then used to estimate developed peak flow rates at Millfield Bridge (node<br />

CON.15).<br />

PARSONS BRINCKERHOFF 2122870A-PR0116 Page 12

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