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Collingham, E.B. and Newman, R.J. 1984. A Permanent Wellpoint Scheme for the Control of Saline Groundwater. Fourth Australian - New Zealand Conference on Geomechanics, Perth, 14 - 18 May, 1984.
Saline groundwater stored beneath Lake Victoria in south-west NSW is discharging to Rufus River and thereby effecting the salinity of the water in the Murray River. A case study is presented which details the investigation, design, construction and commissioning stages of a permanent wellpoint scheme for the extraction of the highly saline groundwater beneath the Lake.The interception scheme, known as the Rufus River Groundwater Interception Scheme, was commissioned in late 1983 and funded by the River Murray Commission at a cost of $3.3 million.
Lake Victoria is the source of the salinity problem in the area. The lake was a natural lake which has since been converted into a massive off-stream storage for the River Murray by raising its top water level. Freshwater stored in the lake forces salty groundwater in the sands beneath the lake to migrate towards the Rufus River.Rufus River is used as the discharge channel which returns water stored in the lake back to the River Murray. Although Rufus River is only 3 km in length, the natural groundwater salinity adjacent to it is so high and the groundwater inflow rate is so large that the channel collects salt in the order of 200 tonnes per day.A typical soil profile beneath the lake consisted of clays to 4 metres, followed by medium grained sand to 12 meters. From 12 metres to 28 metres a coarse sand with clay floc is present, which is underlain by clayey sand.
Prior to construction, the design and performance of the wellpoint system was modelled to enable for maximum economic efficiency.
At the time the report was written, the performance of the scheme had not been monitored.
The technical and economic feasibility of the trial interception scheme undertaken at Rufus River are yet to be determined. If successful, the primary benefit derived from the interception scheme is the protection of the River Murray from highly saline groundwater inflows, and as a result significant economic returns are generated.The economic viability and technical practicalities of such an interception scheme in a dryland context would require the value and degree of protection provided to a receiving water body to be determined on a site by site basis.
The following are key determining factors for the successful implementation of groundwater interception schemes in dryland areas:
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