Great Artesian Basin

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Great Artesian Basin in Australia
Lightning Ridge bathing thermes supplied by artesian bore water
Hot water bore hole into the Great Artesian Basin in Thargomindah

The Great Artesian Basin, located within Australia, is the largest and deepest artesian basin in the world, stretching over 1,700,000 square kilometres (660,000 sq mi), with measured temperatures ranging from 30–100 °C (86–212 °F). The basin provides the only reliable source of fresh water through much of inland Australia.[1]

The Basin underlies 23% of the continent, including the states and territories of Queensland (most of), the Northern Territory (the south-east corner of), South Australia (the north-east part of), and New South Wales (northern part of). The basin is 3,000 metres (9,800 ft) deep in places and is estimated to contain 64,900 cubic kilometres (15,600 cu mi) of groundwater.[2] The Great Artesian Basin Coordinating Committee (GABCC)[3] coordinates activity between the various levels of government and community organisations.

Physiography[edit]

This area is one of the distinct physiographic provinces of the larger East Australian Basins division, and includes the smaller Wilcannia Threshold physiographic section.

Geology[edit]

The water of the GAB is held in a sandstone layer laid down by continental erosion of higher ground during the Triassic, Jurassic, and early Cretaceous periods. During a time when much

of what is now inland Australia was below sea level, the sandstone 

was then covered by a layer of marine sedimentary rock shortly afterward, which formed a confining layer, thus trapping water in the sandstone aquifer. The eastern edge of the basin was [[Tectonic uplift|uplifted]] when the Great Dividing Range formed. The other side was created from the landforms of the [[Central Eastern Lowlands]] and the Great Western Plateau to the west.

Most recharge water enters the rock formations from relatively high ground near the eastern edge of the basin (in Queensland and New South Wales) and very gradually flows toward the south and west.[4] A much smaller amount enters along the western margin in arid central Australia, flowing to the south and east. Because the sandstones are permeable, water gradually makes its way through the pores between the sand grains, flowing at a rate of one to five metres per year.

Discharge water eventually exits through a number of [[spring (hydrosphere)|springs]] and seeps, mostly in the southern part of the basin. The age of the groundwater determined by carbon-14 and chlorine-36 measurements combined with hydraulic modelling

ranges from several thousand years for the recharge areas in the north 

to nearly 2 million years in the south-western discharge zones.[5]

Water source[edit]

Prior to European occupation, waters of the GAB discharged through mound

springs, many in arid South Australia. These springs supported a 

variety of endemic invertebrates (molluscs, for example), and supported extensive Aboriginal communities and trade routes.[6] After the arrival of Europeans, they enabled early exploration and faster communications between southeastern

Australia and Europe via the [[Australian Overland Telegraph 

Line]].[6] The Great Artesian Basin became an important water supply for cattle stations, irrigation, and livestock and domestic usage, and is a vital life line for rural Australia.[7] To tap it, water wells are drilled down to a suitable rock layer, where the pressure of the water forces it up, mostly without pumping.

The discovery and use of water held underground in the Great Artesian Basin opened up thousands of square miles of country away from rivers in

inland New South Wales, Queensland, and South Australia, previously 

unavailable for pastoral activities. European discovery of the basin dates from 1878 when a shallow bore near [[Bourke, New South Wales|Bourke]] produced flowing water.[[Category:Articles with unsourced statements from September 2010]][citation needed] There were similar discoveries in 1886 at Back Creek east of Barcaldine, and in 1887 near [[Cunnamulla, Queensland|Cunnamulla]].[7][8]

In essence, water extraction from the GAB is a mining operation, with recharge much less than current extraction rates. In 1915, there were 1,500 bores providing 2,000 megalitres (1,600 acre·ft) of water per day, but today the total output has dropped to 1,500 megalitres (1,200 acre·ft) per day.[2] This included just under 2000 freely flowing bores and more than 9000 that required mechanical power to bring water to the surface. Many bores are unregulated or abandoned, resulting in considerable water wastage. These problems have existed for many decades, and in January 2007 the Australian Commonwealth Government announced additional funding in an attempt to bring them under control. However, many of the mound springs referred to

above have dried up due to a drop in water pressure, probably resulting
in extinction of several invertebrate species.[9][10]

In addition, the basin has provided water via a 1.2 km (0.75 mi) deep bore for a geothermal power station at Birdsville. The heated water is 98°C (208°F) and provides 25% of the town's needs. [[Ergon (Australia)|Ergon Energy]] is expanding the 80 kW plant to completely meet Birdsville's electricity requirements.{{Citation needed|date=March 2007}}

Whole of Basin management[edit]

As the Great Artesian Basin underlies parts of Queensland, New South Wales, South Australia and the Northern Territory, which each operate under different legislative frameworks, policies and resource management approaches, a coordinated "whole-of-Basin" approach to the management of this important natural resource is required. The Great Artesian Basin Coordinating Committee (GABCC) provides advice from community organisations and agencies to State, Territory and Australian Government Ministers on efficient, effective and sustainable whole-of-Basin resource management and to coordinate activity between stakeholders.

Membership of the Committee comprises all State, Territory, and Australian Government agencies with responsibilities for management of parts of the Great Artesian Basin, community representatives nominated by agencies; and sector representatives. The primary role of the Committee is to provide advice to State, Territory and Australian Government Ministers on efficient, effective, and sustainable whole-of-Basin resource management and to coordinate activity between stakeholders.

The GABCC website provides up-to-date information and links to other sites that discuss the Basin can be accessed from there.[3]

Current scientific thinking[edit]

A comprehensive background to the Great Artesian Basin, including an overview of the nature of the Basin, the extraction of water and the impacts of that extraction, can be found in the Great Artesian Basin Resource Study, developed by the GABCC to support the Great Artesian Basin Strategic Management Plan.

== Potential depletion and pollution due to coal seam gas extraction == In 2011, ABC TV Four Corners revealed that significant concerns were being expressed about depletion and chemical damage to the Basin as a result of coal seam gas extraction. In one incident, reported in the program, the [[Queensland Gas Company]] (QGC) fracked its Myrtle 3 well connecting the Springbok aquifer to the coal seam below (the Walloon Coal Measures) in 2009. A local farmer was concerned that the process may have released 130 litres (29 imp gal; 34 US gal) of a potentially toxic chemical into the Basin. QGC admitted the incident, but "did not alert authorities or nearby water users about the problem until thirteen months after the incident."[11] The safety data sheet QGC had submitted for the hydraulic fracturing chemical was derived from the United States, incomplete and ten years out of date.[11] Over thirty chemicals may be used in the process of hydraulic fracturing and their long-term impact on aquifers and the agriculture and people supported by

them is unknown.[12]

See also[edit]

References[edit]

  1. ^ Spanevello, M. D. (November 2001). The phylogeny of prokaryotes associated with Australia's Great Artesian Basin (PDF) (Ph.D.). Griffith University. Retrieved 26 July 2009. 
  2. ^ a b {{cite web|url=http://www.derm.qld.gov.au/factsheets/pdf/water/w68.pdf |title=Underground water factsheets: Great Artesian Basin |accessdate=30 September 2010 |publisher=Department of Environment and Resource Management}}
  3. ^ a b GABCC website
  4. ^ http://www.gabcc.org.au/tools/getFile.aspx?tbl=tblContentItem&id=96 page 40[dead link]
  5. ^ Mudd, G.M. (March 2000). "Mound springs of the Great Artesian Basin in South Australia:a case study from Olympic Dam". Environmental Geology (Springer Berlin / Heidelberg) 39 (5). doi:10.1007/s002540050452. 
  6. ^ a b Harris, Colin (2002). [http://www.icomos.org/australia/Tracks/02%20Harris,%20Mound%20Springs.doc Culture and geography: South Australia’s mound springs as trade and communication routes], Historic Environment, 16 (2), 8-11. ISSN 0726-6715.
  7. ^ a b [[Environmental Protection Agency (Queensland)]] (2002). Heritage Trails of the Queensland Outback. State of Queensland. p. 9. ISBN 0-7345-1040-3. 
  8. ^ Nicol, Sally (2005). "The Great Artesian Basin: past, present and future". Water management. The State of Queensland (Department of Natural Resources and Water). Archived from the original on 15 March 2007. Retrieved 2 March 2007. 
  9. ^ Ponder, Winston. [http://www.austmus.gov.au/factsheets/mound_springs.htm Mound Springs in Arid Australia], Australian Museum.
  10. ^ [http://www.environment.nsw.gov.au/determinations/ArtesianSpringsEcologicalCommunityEndComListing.htm Artesian springs ecological community - endangered ecological community listing - final determination], NSW Scientific Committee, Minister for the Climate Change and the Environment, New South Wales Government. Gazetted 15 June 2001. Page updated 12 February 2008.
  11. ^ a b "Farmers count cost of coal seam gas rush". ABC News (Australia). 21 February 2011. Retrieved 21 May 2011. 
  12. ^ Tozer, Joel; Cubby, Ben (19 October 2010). "List reveals toxic chemicals used in coal seam mining". The Sydney Morning Herald. Retrieved 21 February 2011. 

External links[edit]