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construction and refurbishment of earthen irrigation channel banks

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21.8.6 Surface interception drainage21.8.6.1 Surface drains at toe <strong>of</strong> bankOpen surface drains along a <strong>channel</strong> will not generally intercept seepage as theywill be too high above the free surface. To make open drains deep enough to beeffective, the high <strong>construction</strong> cost, extensive l<strong>and</strong> requirements <strong>and</strong> highmaintenance costs make them impractical. (Refer Figure 21-6). However theycan be useful to intercept leakage from deteriorated <strong>channel</strong>s <strong>banks</strong>.Drains require effective disposal which may be achieved by pumping back intothe <strong>channel</strong>.21.8.6.2 Regional Drainage SystemsMost <strong>irrigation</strong> areas in Victoria <strong>and</strong> New South Wales are in very flat areas. Forinstance the natural grade <strong>of</strong> l<strong>and</strong> in Central Goulburn area <strong>of</strong> Goulburn-MurrayWater is 1 in 10,000. The natural drainage lines tend to be depressions that fill inwet years rather than perennial streams. Construction <strong>of</strong> regional drains alongthese depressions has intercepted seepage due to the high watertables (2 metres orless from the surface) experienced over much <strong>of</strong> the <strong>irrigation</strong> areas.21.8.7 Interception DrainageThis seepage control method can be more accurately described as a countermeasureagainst seepage water reaching the watertable. Essentially, the concept aims toretrieve the water that has already leaked out <strong>of</strong> the <strong>channel</strong> <strong>and</strong> to return it to the<strong>channel</strong>.The concept consists <strong>of</strong> a horizontal perforated pipe set at 2 to 3 metre depthrunning along each side <strong>of</strong> the <strong>channel</strong> <strong>and</strong> between 5 to 10 metres away from the<strong>channel</strong>, with collection sumps <strong>and</strong> pumps, to pump the water back into the<strong>channel</strong>.This concept is only effective where the watertable is already shallow. Wherewatertables are deeper than the intercepting pipeline, seepage water tends tomigrate vertically downwards from the <strong>channel</strong> <strong>and</strong> will not be picked up by thepipe. Refer to Figure 21-4. Also the soil in the vicinity needs to be sufficientlypermeable to enable seepage water to be efficiently drawn to the pipeline.There are on-going costs associated with the pumping <strong>and</strong> pipeline maintenance(root clearing) <strong>and</strong> the recurrent costs can be relatively high.21.8.8 Groundwater interceptionAn alternative to preventing <strong>channel</strong> seepage is the <strong>construction</strong> <strong>of</strong> groundwaterinterception schemes involving groundwater pumping for shallow bores or tiledrainage located adjacent to the <strong>channel</strong>. Groundwater pumping may be the mostsuitable option where a pumpable aquifer is present. Where hydraulicconductivities are lower, tile drainage may be a more practical <strong>and</strong> cost-effectiveoption.Construction <strong>and</strong> Refurbishment <strong>of</strong> Earthen Channel Banks August 2002 – Edition 1.0 21-38

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