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The proposal footprint is located above the Sydney basin-central area porous rock<br />

aquifer unit. This is the most extensive <strong>of</strong> Sydney’s aquifer units; however its<br />

associated groundwater quality is ‘poor-to-very-poor’ (State <strong>of</strong> the Catchment,<br />

Groundwater the Sydney Metropolitan Region 2010, DECCW).<br />

The proposal footprint is not located on land designated for groundwater<br />

management or underlain by a vulnerable aquifer. It is also located outside <strong>of</strong> the<br />

heavily contaminated Botany Bay sand beds.<br />

The available published information on localised groundwater depth is limited to a<br />

few bore records around Barangaroo and the periphery <strong>of</strong> the <strong>city</strong> <strong>centre</strong>. These<br />

records confirm the presence <strong>of</strong> a water bearing zone at shallow depths <strong>of</strong> between<br />

one and six metres. The wider literature also confirms that groundwater depths can<br />

vary from just below the surface to approximately 10 metres 4 . Coastal inundation also<br />

occurs east <strong>of</strong> the proposal footprint, <strong>of</strong>ten requiring dewatering during construction.<br />

In conclusion, the geology and soil characteristics <strong>of</strong> the proposal footprint (refer to<br />

section 6.8.2) are capable <strong>of</strong> bearing groundwater. They are also capable <strong>of</strong> being<br />

hydraulically connected allowing groundwater to transfer between the geological<br />

horizons and the upper soil layers (referred to as an unconfined groundwater). That<br />

said, certain <strong>of</strong> the soils are characteristically impervious or semi-pervious (refer to<br />

section 6.8.2) and would not readily support groundwater flow. They may however<br />

support locally perched waters at or close to the surface or limited flows across their<br />

extents. Closer to Sydney Harbour there is likely to be an interface between the<br />

groundwater and coastal waters. As a result, the groundwater is likely to be slightly<br />

brackish as a result <strong>of</strong> saline intrusion. The extent <strong>of</strong> saline intrusion and brackish<br />

concentrations will depend on the localised groundwater pressure and chemistry<br />

along with the geology <strong>of</strong> the area.<br />

6.7.3 Potential impacts<br />

Water quality and hydrology impacts during construction<br />

Accidental spillage<br />

Some <strong>of</strong> the proposed construction works detailed in section 3.3 would have a limited<br />

risk <strong>of</strong> resulting in accidental chemical, oil and fuel spillages during construction. This<br />

risk would exist:<br />

At any work site as a result <strong>of</strong> general working activities<br />

<br />

<br />

Along haulage routes through accidents or poorly maintained vehicles<br />

At the construction compounds/laydown areas as a result <strong>of</strong> poor materials<br />

handling, poor materials storage or poor equipment maintenance practices.<br />

The corresponding activities within the proposal footprint that would be at greater risk<br />

<strong>of</strong> accidental spillage include:<br />

Removing spoil and waste from site to one <strong>of</strong> the construction compounds or<br />

temporary laydown areas (ie haulage)<br />

Delivering materials to site or one <strong>of</strong> the construction compounds or temporary<br />

laydown areas (ie haulage)<br />

Loading and unloading at the work sites and construction compounds or<br />

laydown areas<br />

Major ground excavation work, including drainage modifications and utility<br />

adjustments.<br />

4<br />

Russell. G, Green. R, Rumpf. C, Managing Groundwater Impacts <strong>of</strong> Construction in Sydney NSW,<br />

2010.<br />

Sydney City Centre Capa<strong>city</strong> Improvement 368<br />

Review <strong>of</strong> Environmental Factors

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