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RB 77/00132 Hydrogeology of the Paragum Depression, Monarto SA.
Cable tool and rotary drilling of 8 holes has enabled the geological sequence and general hydrology to be determined in the area to appraise its potential as a disposal site for stormwater runoff from urbanised Monarto.-
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Published: 01 Jan 1977
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RB 92/00015 Regional hydrogeology of the Loxton-Noora area, Murray Basin, South Australia.
The Loxton-Noora area is underlain by 3 aquifer systems - the Pliocene Sands water table aquifer, the confined Murray Group limestone and the deepest, the confined Renmark Group aquifer. Both confined aquifers contain groundwater of 20-25 000 mg/L...-
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Published: 01 May 1992
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RB 97/00023 Hydrogeology of the Moorook New Residence irrigation district.
Following a request from the SA Department of Environment and Natural Resources at Berri in the Riverland, a hydrogeological assessment of the Moorook and New Residence irrigation areas was carried out. The water table aquifer occurs in fine to...-
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Published: 01 Apr 1997
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RB 96/00017 River Murray water resource management. Assessment of salt load impacts and drainage hazard for new irrigation development along the River Murray in South Australia.
The Murray-Darling Basin Commission (MDBC) has a commitment in the national interest to managing the health of the River Murray and floodplain environment by mitigating both decreases in river water quality and associated environmental degradation...-
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Published: 01 May 1996
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RB 66/00060 Chowilla Project. Saline water disposal, Tilmy Flat. Geological investigation progress report no. 3. Co. Hamley - EWS Department.
This report describes the results of geological investigations carried out on the right bank of the River Murray, at and adjacent to Tilmy Flats. A summary of the work is as follows: 8 shallow observation wells to detect lateral movement of...-
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Published: 01 Jan 1968
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RB 74/00152 Investigation of potential evaporation basins, Upper Murray, South Australia. Progress report 1. Appendix Analogue model experiments to determine saline groundwater flow into the Murray River system
Groundwater flow in the Upper Murray region is generally towards the River Murray except in the Noora area where contours show a depression in the water table surface. The Noora area appears to be the most suitable site for an evaporation basin for...-
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Published: 01 Jan 1974
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RB 76/00016 Investigation of potential evaporation basins, Upper Murray, South Australia. Progress report no. 3.
Further drilling and aquifer testing between the proposed Noora evaporation basin and the River Murray yielded an average value of about 100 m3/day/m for transmissivity of the Loxton Sand aquifer. It is therefore expected that initial effects of such...-
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Published: 16 Feb 1976
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RB 2003/00013 North-western Murray Basin geological synthesis, South Australia.
The Murray Basin is an intracratonic basin filled with Cainozoic fluvial to shallow marine sediments. Deposition in the Eocene and early Oligocene was characterised by floodplain and swamp deposits, emplaced with occasional interbeds of shelly clays...-
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Published: 01 Aug 2003
