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7.2.6 Artificially Drained <strong>Systems</strong><br />

7.2.6.1 Description<br />

High water tables that limit the use of trenches, beds or seepage pits<br />

can sometimes be artificially lowered to permit the use of these dispo-<br />

sal methods. Vertical drains, curtain drains <strong>and</strong> underdrains are com-<br />

monly used subsurface drainage techniques. Soil <strong>and</strong> site conditions<br />

determine which method is selected.<br />

Curtain drains <strong>and</strong> vertical drains are used to lower perched water<br />

tables. These methods are most effective where the perched water is<br />

moving laterally under the soil absorption site. The drains are placed<br />

upstream of the absorption area to intercept the groundwater as it flows<br />

into the area.<br />

Curtain drains are trench excavations in which perforated drainage pipe<br />

is placed. These are placed around the upslope perimeter of the soil<br />

absorption site to intercept the groundwater moving into the area (see<br />

Figure 7-15). If the site has sufficient slope, the drains are brought<br />

to the surface downslope to allow free drainage. <strong>On</strong> level sites, pumps<br />

must be used to remove the collected water. If the restrictive layer<br />

that creates the water table is thin <strong>and</strong> overlies permeable soil, verti-<br />

cal drains may be used. These are trench excavations made through the<br />

restrictive layer into the more permeable soil below <strong>and</strong> backfilled with<br />

porous material (see Figure 7-16). Thus, water moving toward the ex-<br />

cavation is able to drain into the underlying soil. Vertical drains are<br />

susceptible to sealing by fine sediment transported by the water.<br />

Underdrains are used where water tables exist 4 to 5 ft (1.2 to 1.5 m)<br />

below the surface in permeable soils. The drains are similar to curtain<br />

drains in construction, but several drains may be necessary to lower the<br />

water table sufficiently (see Figure 7-17). Depth <strong>and</strong> spacing of the<br />

drains are determined by the soil <strong>and</strong> water table characteristics.<br />

7.2.6.2 <strong>Site</strong> Considerations<br />

Successful design of artificially drained systems depends upon the cor-<br />

rect diagnosis of the drainage problem. The source of the groundwater<br />

<strong>and</strong> its flow characteristics must be determined to select the proper<br />

method of drainage. Particular attention must be given to soil strati-<br />

fication <strong>and</strong> groundwater gradients.<br />

260

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