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  2. Swale (landform) - Wikipedia

    en.wikipedia.org/wiki/Swale_(landform)

    In US usage in particular, it is a shallow channel with gently sloping sides. Such a swale may be either natural or human-made. Artificial swales are often infiltration basins , designed to manage water runoff , filter pollutants , and increase rainwater infiltration . [ 2 ]

  3. Trench drain - Wikipedia

    en.wikipedia.org/wiki/Trench_drain

    A trench drain (also known as a channel drain, line drain, slot drain, linear drain, or strip drain) is a specific type of floor drain featuring a trough- or channel-shaped body. It is designed for the rapid evacuation of surface water or for the containment of utility lines or chemical spills.

  4. Percolation trench - Wikipedia

    en.wikipedia.org/wiki/Percolation_trench

    It is a shallow excavated trench filled with gravel or crushed stone that is designed to infiltrate stormwater though permeable soils into the groundwater aquifer. [ 1 ] [ 2 ] A percolation trench is similar to a dry well , which is typically an excavated hole filled with gravel. [ 3 ]

  5. Drainage - Wikipedia

    en.wikipedia.org/wiki/Drainage

    Drainage is the natural or artificial removal of a surface's water and sub-surface water from an area with excess water. The internal drainage of most agricultural soils can prevent severe waterlogging (anaerobic conditions that harm root growth), but many soils need artificial drainage to improve production or to manage water supplies.

  6. Ditch - Wikipedia

    en.wikipedia.org/wiki/Ditch

    A ditch can be used for drainage, to drain water from low-lying areas, alongside roadways or fields, or to channel water from a more distant source for plant irrigation. Ditches are commonly seen around farmland, especially in areas that have required drainage, such as The Fens in eastern England and much of the Netherlands.

  7. Rill - Wikipedia

    en.wikipedia.org/wiki/Rill

    A downslope view of part of the eroding rill network from County Tyrone, Northern Ireland.See below for a close-up view of a single rill. In hillslope geomorphology, a rill is a shallow channel (no more than a few inches/centimeters deep) cut into soil by the erosive action of flowing surface water.

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