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CoorongIntroduction

The Coorong is part of a wetland region at the lower end of the River Murray catchment. It is connected to the Lower Lakes and Murray Mouth. This region is a nationally significant wetland and is recognised as being of international importance under the Ramsar Convention. The Coorong is a 2-3 km wide lagoon system that follows the coast south for at least 100 km from the river mouth. The Coorong National Park was declared in 1966 to conserve the distinctive landscape, coastal dune system, lagoons, wetlands and coastal vegetation, and the great variety of birds, animals and fish that live in, or visit, the area.

The Coorong is best characterised as ahypersaline estuary, and is influenced by relatively freshwater from the River Murray and local inflows from the Upper South East, as well as by seawater entering through the Murray Mouth and through the sand dunes of the Younghusband Peninsula. The main problem for the Coorong is reduced freshwater flows from the River Murray. Nutrient concentrations are frequently elevated and there is often a large amount of algae, as indicated by the chlorophyll (a) concentrations. The CSIRO have established a research program to explore the complexities of the Murray lakes, estuary and Coorong and provide information to help predict environmental, social and economic effects of different management strategies and policy decisions. >> More

>> Map showing the Coorong monitoring sites (417KB PDF)

>> Information on the Coorong natural attractions (courtesy of the Department of Environment and Heritage, SA)

>> More on the Lower Lakes and the Coorong

>> More photos of the Coorong

Water quality assessment

The Department for Environment and Heritage, SA coordinates quarterly water quality sampling and analyses in the Coorong at 12 locations along its length (see map (417KB PDF)). The indicators that are measured are nutrients (nitrogen and phosphorus), turbidity, chlorophyll (a), and salinity. The concentrations of these indicators are used to classify the water quality as being in good, moderate or poor condition, according to the needs of aquatic ecosystem protection as an environmental value. >> More

Water quality classification for April to September 2006

Indicator
Classification
Good
Good
Poor
Good
Poor
Poor
Chlorophyll (a)
Poor

Notes NA = no data available this period

The water quality monitoring results for this period were generally consistent with previous seasonal results for this site.

The Coorong has an almost constant algal bloom as indicated by the very high chlorophyll (a) levels. The nutrients that support the algae are also very high, although the majority of the nutrients are bound up in the algae that are suspended in the water.

Nutrients can be elevated by fertilisers or animal wastes being washed off farms during storms, although because inflows to the Coorong are minimal, the majority of nutrients taken up by algae are probably being recycled from the sediments.

The high turbidity levels are probably caused by the algae in the water and resuspended sediment particles.

The Coorong also has very high salinity levels due to evaporation and the lack of freshwater inputs from the River Murray. This hyper-saline condition probably reduces animal diversity which would normally keep the algae under control.

There is a distinct north-south gradient in the Coorong water quality characteristics. The salinity is at its lowest near the Lower Lakes and increases to its maximum at its most southerly point. Conversely, the nutrients, chlorophyll (a) and turbidity all increase in concentration in a southerly direction. These spatial variations in the Coorong are seen in the data that can be downloaded for the different monitoring sites (417KB PDF).

>> Archived results

Download water chemistry graphs

Download raw chemistry data

What is being done to improve the condition of the Coorong

There are few pollution pressures directly acting on the Coorong which need to be regulated or managed. Rather, the recovery of the Coorong depends largely on the restoration of the River Murray, Lower Lakes and Murray Mouth region.

To this end, the Department for Water, Land and Biodiversity Conservation and the Murray-Darling Basin Commission are managing the Murray-Darling Basin Initiative. >> More

In addition, the Upper South East Dryland Salinity and Flood Management Program is involved in assessing the ecology of the Coorong and drainage waters that flow to the Coorong via Salt Creek, which enters the Southern Lagoon. >> More

This page was last modified 29-07-2008
 

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