Australian Natural Resources Atlas

Natural Resource Topics

Australian Catchment, River and Estuary Assessment 2002

National Land and Water Resources Audit, 2002
ISBN 0 642 37125 3

Assessment findings

Figure 56: Condition of Australia's estuaries. Fifty percent are near-pristine, 22% are largely unmodified, 19% are modifed and 9% are extensively modified.
Table 23. Condition of Australia's estuaries by process type.
Table 23: Condition of Australia's estuaries by process type.
Class Subclass Near-pristine Largely unmodified Modified Extensively modified Total
Wave estuary 28 41 62 25 156
strandplain 36 13 10 1 60
other 40 30 22 17 109
Tide estuary 57 25 9 4 95
tidal flat/creek               210 43 16 15 284
other 40 17 23 9 89
River wave–dominated delta 28 24 30 12 94
tide–dominated delta 36 16 11 9 72
Not classified 9 1 3 0 13
Total 484 210 186 92 972

Tidal flats and creeks

Most of Australia's estuaries are tide-dominated systems with tidal flats and creeks particularly dominant (29%). Tidal flats are low gradient accumulations of fine sediment or mud, often dissected by numerous tidal channels. Tidal flats occur in regions that have a high tidal influence and are most extensive in macrotidal regions (e.g. Northern Territory, north-west Western Australia) and along muddy low-gradient coastlines (e.g. Gulf of Carpentaria).

Tidal flats drain out at low tide and have mangrove-lined channels with expanses of saltmarsh located further landward, between intertidal and supratidal levels.

Tidal creeks are small tidal channels cut into coastal flats. They are often associated with tidal flats, draining and filling the flats during each tidal cycle. The banks of tidal creeks are generally above the high tide limit. An example of a typical tidal flat system is Moonlight Creek located on the south coast of the Gulf of Carpentaria.

Tidal flats and creeks are well mixed and often naturally turbid. Tidal flows usually have enough velocity to re-suspend fine sediments (mud). Seventy-four percent of Australia's tidal flats and creeks are in near-pristine condition. Most of the tidal flats and creeks have small coastal catchment areas, often in undisturbed condition.

Figure 57: Condition of tidal flats/creeks (284 estuaries assessed).

Note:
Legend Near-pristine
Legend Largely unmodified
Legend Modified
Legend Extensively modified

True estuaries

From a geomorphic perspective an 'estuary' is a discrete type of coastal waterway. They are defined as the 'seaward limit of a drowned valley, which receives sediment from both river and marine sources and is influenced by wave, tide and river processes'. Of the coastal waterways assessed, 26% were classified as 'true' estuaries in a geomorphic sense (16% are wave-dominated estuaries and 10% are tide-dominated estuaries).

Wave-dominated estuaries are characterised by a sandy barrier parallel to the shoreline at the mouth with a low energy central basin landward. Built by wave action, the bar often constricts the entrance of wave-dominated estuaries. Wave dominated estuaries have a high tendency to trap sediment and are generally partially mixed. This type of system tends to be seasonally stratified with naturally low turbidity (except during high winds or flood events). Nutrients recycled from the sediments in the central basin may make systems susceptible to algal blooms. An example of a typical wave-dominated estuary is Lake Illawarra in New South Wales. Wave-dominated estuaries are also known as barrier estuaries, coastal lakes or lagoons.

Geomorphic formations such as the barrier, and flood and ebb tide delta, coupled with the longshore drift and accumulation of marine sediment, reduce the opportunity for ocean exchange and flushing of wave-dominated estuaries. In Australia, wave-dominated estuaries are popular for recreational and residential development. Sediments and nutrients from the catchment generally accumulate in the estuary, making wave-dominated estuaries susceptible to problems associated with poor flushing and increased nutrient levels.

The natural susceptibility of wave-dominated estuaries to development pressures is reflected in the high proportion of modified wave-dominated estuaries. A common management response to water quality problems and navigation difficulties is to artificially open the entrance. Artificial opening is achieved either permanently with training walls (e.g. Wallis Lake New South Wales, Lakes Entrance Victoria) or by bulldozing the beach berm (e.g. many of the smaller New South Wales and Victorian wave-dominated estuaries). This can have serious ecological consequences (e.g. immature black swans can become stranded in wetlands and unable to travel to open water, such as at Smith's Lake and Lake Cathie - Lake Innes, New South Wales). Artificial opening strategies are the subject of many community debates. Certainly strategies need to recognise a range of management objectives and values including waterbird breeding, fisheries, navigation needs, water quality, flooding risk and likelihood of rapid re-closure from seasonal wave conditions.

Figure 58: Condition of true estuaries (156 wave-dominated estuaries assessed; 95 tide-dominated estuaries assessed).

Note:
Legend Near-pristine
Legend Largely unmodified
Legend Modified
Legend Extensively modified

Tide-dominated estuaries are typically funnel-shaped, and contain elongated sand bodies known as tidal sand banks in the main tidal channel(s). These elongated sand banks are generally orientated parallel to the direction of tidal flows. Tide-dominated estuaries trap coarse sediment as part of the development of the tidal sand banks and fine sediment on the margins in the form of intertidal flats, mangroves and salt marshes. Driven by higher velocity tidal flows than their wave-dominated counterparts, tide-dominated estuaries generally have naturally high turbidity and are well mixed throughout the year. An example of a typical tide-dominated estuary is Adelaide River in the Northern Territory.

Tide-dominated estuaries are generally highly turbid due to strong tidal currents. The relatively unconstricted entrance and strong tidal currents enhance flushing, relieving them from some of the impacts of nutrients and sediments. These systems act as a conduit for sediments and nutrients from the catchment to the near-shore marine zone. This underlies the importance of improved catchment management to reduce sediment and nutrient loads in the river basins with these types of estuaries (e.g. Fitzroy River adjoining the Great Barrier Reef).

Deltas

Seventeen percent of Australia's estuaries are deltas (10% wave-dominated, 7% tide-dominated). Deltas are broadly defined as coastal accumulations of river-derived sediment that generally protrudes into the near-shore environment. Deltas are generally net exporters of sediment due to the high river influence.

Wave-dominated deltas have bow-shaped shorelines, poor flushing generally low turbidity and experience partial mixing and salt wedges. Tide-dominated deltas are generally turbid and well mixed.

Sediment delivered to the coast in regions of high wave energy (e.g. New South Wales ) may be transported along the shoreline and the wave-dominated delta may not protrude (e.g. Brunswick River, New South Wales). An example of a typical wave-dominated delta is Nassau River (Queensland); an example of a typical tide-dominated delta is McArthur River (Northern Territory).

Both tide and wave-dominated deltas contribute substantial amounts of sediments and nutrients to the near-shore environment. Along the New South Wales coast, sediments and nutrients escaping deltas are transported along the coast by wave and ocean currents. Along the Queensland coast progradation of deltas into the near-shore environment may be extensive (e.g. Burdekin River).

Figure 59: Condition of deltas (94 wave-dominated estuaries assessed; 72 tide-dominated estuaries assessed).

Note:
Legend Near-pristine
Legend Largely unmodified
Legend Modified
Legend Extensively modified

Jerusalem Creek: a wave-dominated strandplain in near-pristine condition.

Jerusalem Creek: a wave-dominated strandplain in near-pristine condition.

Photo: Department of Land and Water Conservation, New South Wales.

Strandplains, coastal lakes and lagoons

Six percent of Australia's estuaries are drainage points for strandplains. Strandplains are sand bodies that run parallel to the shore and contain beaches, swales and dunes. They are found along prograded linear coasts. Strandplains are not associated with embayments, but are dune systems inter-filling between headlands.

Strandplains are usually associated with small to negligible river input and drain the immediate area of dunes and swales. Wetland and coastal heath systems are often extensive, with creeks usually only intermittently open to the ocean. An example of a strandplain is Jerusalem Creek, New South Wales.

Figure 60. Condition of strandplains, coastal lakes and lagoons (60 estuaries assessed).

Note:
Legend Near-pristine
Legend Largely unmodified
Legend Modified
Legend Extensively modified

Estuaries of Australia's capital cities

The diversity of estuary types distributed around Australia is indicated by the estuaries associated with Australia's capital cities

Table 24. Estuaries of Australia's capital cities.
  Port Estuary class/subclass Condition
Darwin Darwin Harbour tide/other largely unmodified
Brisbane Brisbane River river/tide-dominated delta extensively modified
Sydney Port Jackson tide/other extensively modified
Melbourne Yarra River river/tide-dominated delta extensively modified
Hobart Derwent River tide/other extensively modified
Adelaide Port River Barker Inlet tide/tidal flat/creek extensively modified
Perth Swan River wave/estuary extensively modified

Application of the results

Excess nutrients in estuaries cause algal blooms.

Excess nutrients in estuaries cause algal blooms.

Photo: Rochelle Lawson.

A more detailed study of Australia's modified estuaries enhances our understanding of their condition and the pressures they face. The assessment provides an on-line framework to encourage others to contribute information and knowledge, on what is and is not known, for the estuaries where they live and work. This information will enhance our collective understanding of estuarine management issues and the appropriateness of different management strategies for preventing further degradation and improving estuarine condition.

Limitations of the assessment

The assessment provides an excellent overview of the condition of Australian estuaries with some limitations:

Key pressures on estuaries: common challenges facing Australia's modified estuaries

Photo: Department of Natural Resources and Environment, Victoria.

Photo: Department of Natural Resources and Environment, Victoria.

Case study: Gippsland Lakes

Illustrating the complex nature of estuary management

Introduction

In 1995 the funding and responsibility for 12 local ports in Victoria was transferred from the Port of Melbourne Authority to the Department of Natural Resources Environment. In 1996 the Department of Natural Resources and Environment outsourced the management of these ports and appointed local port managers. In the case of the five Gippsland Regional Ports the manager is the Gippsland Ports Committee of Management.

The Port of Gippsland Lakes encompasses one of Australia's largest estuaries stretching from Sale in the west to Lakes Entrance in the east. The port is the largest of the Gippsland Ports and covers the lower reaches of the Latrobe, Nicholson, Mitchell and Tambo rivers as well as Lakes Wellington, Victoria and King.

Photo: Department of Natural Resources and Environment, Victoria.

Photo: Department of Natural Resources and Environment, Victoria.

The Gippsland Lakes are home to one of Victoria's largest fishing fleets (in terms of vessel numbers [about 65] and landed catch value) and an increasingly popular tourist and recreational boating destination due to its sheltered waters.

Access to the ocean is via Lakes Entrance. This man-made entrance was opened in 1899 and has provided an important contribution to the region's history and economy since that time.

Two of the major issues for the Gippsland Lakes are the silting of the channels and entrance (which requires ongoing dredging to maintain ocean access and navigable internal channels) and the increased demand for land based recreation and tourism facilities (which are sometimes incompatible with, and are placing pressure on the port areas).

Estuary use and value

The Port of Gippsland Lakes is used by both commercial fishermen, who use the entrance to access the ocean, and recreational boaters, who take advantage of the sheltered waters within the lake system for fishing and cruising.

Photo: Department of Natural Resources and Environment, Victoria.

Photo: Department of Natural Resources and Environment, Victoria.

The main commercial fishing port is located at Lakes Entrance and provides catch discharge and processing facilities as well as maintenance facilities (e.g. slipways) and moorings. There are also boating facilities located at Paynesville, including marinas, a boat yard and associated services.

To meet the needs of the port users the estuary primarily has to provide a safe, navigable entrance to the open sea and navigable internal channels.

Benefits and estimates of monetary value

The commercial fishing industry is the major user of the Lakes Entrance channel with approximately 13 000 crossings annually.

The Lakes Entrance Fisherman's Co-operative supplies 35-40% of Melbourne's fish product and is a key employer in the region.

Overall Lakes Entrance channel users, including commercial fishermen and recreational boaters account for:

Photo: Department of Natural Resources and Environment, Victoria.

Photo: Department of Natural Resources and Environment, Victoria.

Management issues

The major management issue at Lakes Entrance is the siltation of the entrance and immediate internal channels. The action of normal coastal processes is to form a sand bar across the entrance to the lakes. The water flows within the estuary caused by having an opening to the sea leads to siltation of the internal channels. To maintain safe navigability ongoing dredging of both the entrance and internal channels is required. To alleviate the problem and maximise the efficiency of dredging the internal channels a new sand transfer system has been installed at a cost of approximately $1.5 m. This system pumps the dredge spoil through a series of pumps and pipes back to the open ocean environment. The system has resulted in a reduction of the net inflow of sand into the estuary.

Photo: Department of Natural Resources and Environment, Victoria.

Photo: Department of Natural Resources and Environment, Victoria.

Other management issues include dealing with the sewage discharged from boats (both commercial and recreational) and containing the contaminants (both airborne and water-borne) that are generated during boat servicing/repair.

One final issue facing the Port Manager is that of balancing the requirements of an industrial port with those of a burgeoning tourist industry. The increasing demand for shore based tourism and recreational facilities places pressure on the areas in which port activities have traditionally taken place.

Conclusion

The issues in the Gippsland Lakes are similar though on a different scale to those experienced in all estuaries that contain port facilities. They highlight the need for a balanced approach between natural resource management and development.

 

Case Study: South-east Queensland regional water quality management strategy

Illustrating the complex nature of estuary management

South-east Queensland's coastal regions and waterways, including Moreton Bay, are complex ecosystems that support healthy populations of dugongs and turtles, migratory wading birds and major recreational and commercial fisheries. Population increases in south-east Queensland have the potential to seriously impact on the ecological and economic health of its waterways and catchments. Nutrients (particularly nitrogen), fine sediments and, to a lesser extent, pesticides and heavy metals have already been identified as causes of significant environmental problems within these systems.

In response to these threats, government, industry and community stakeholders are working to implement a regional water quality management strategy.

The strategy forms part of the South East Queensland Regional Framework for Growth Management 1998 and is a joint Commonwealth, State and local Government initiative covering the south-east Queensland region, including coastal waters, estuaries and freshwater streams from Noosa to the Gold Coast and west to the Great Dividing Range. It covers 15 major catchments with a combined catchment area of approximately 22 352 km2 and includes 19 local government areas.

This collaborative approach has been a key characteristic of the strategy. Based on strong local political leadership and advocacy, it has allowed the development of an effective, 'whole of community' organisational approach to action plans that protect and enhance water quality and ecological/economic sustainability.

The vision

South-east Queensland's catchments and waterways will, by 2020, be healthy living ecosystems supporting the livelihoods and lifestyles of people in south-east Queensland and will be managed through collaboration between community, government and industry.

Strengths of the strategy

The major strengths of the strategy are:

Figure 61: Extent of the South East Queensland Regional Water Quality Management Strategy.

Major achievements to date

Important achievements of the strategy to date include:

Key lessons

Conclusion

The strategy is an example of a successful regional planning process. Its success is due to:

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