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  2. Aqueduct (water supply) - Wikipedia

    en.wikipedia.org/wiki/Aqueduct_(water_supply)

    The Catskill Aqueduct carries water to New York City over a distance of 120 miles (190 km), but is dwarfed by aqueducts in the far west of the country, most notably the 242-mile (389-km) Colorado River Aqueduct, which supplies the Los Angeles area with water from the Colorado River nearly 250 miles to the east and the 701.5-mile (1,129.0 km ...

  3. 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.

  4. Bioswale - Wikipedia

    en.wikipedia.org/wiki/Bioswale

    They consist of a swaled drainage course with gently sloped sides (less than 6%). [2]: 19 Bioswale design is intended to safely maximize the time water spends in the swale, which aids the collection and removal of pollutants, silt and debris. Depending on the site topography, the bioswale channel may be straight or meander.

  5. Two-stage drainage ditch - Wikipedia

    en.wikipedia.org/wiki/Two-stage_drainage_ditch

    The two stage drainage ditch is classified as a 'surface' sustainable drainage system, contrary to a sub-surface system. The two stage drainage ditch is a modification of the land whereby grass benches which serve as floodplains are formed within the land of the watershed of the water system, shown in the diagram to the right. [1]

  6. Irrigation - Wikipedia

    en.wikipedia.org/wiki/Irrigation

    Irrigation water can also come from non-conventional sources like treated wastewater, [20] desalinated water, drainage water, or fog collection. In countries where humid air sweeps through at night, water can be obtained by condensation onto cold surfaces. This is practiced in the vineyards at Lanzarote using stones to condense water.

  7. Surface irrigation - Wikipedia

    en.wikipedia.org/wiki/Surface_irrigation

    Deep drainage - Overirrigation may cause water to move below the root zone resulting in rising water tables. In regions with naturally occurring saline soil layers (for example salinity in south eastern Australia ) or saline aquifers, these rising water tables may bring salt up into the root zone leading to problems of irrigation salinity .

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  9. Swale (landform) - Wikipedia

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

    In this context a swale is usually a water-harvesting ditch on contour, also called a contour bund. [4] [5] A natural swale. Swales as used in permaculture are designed by permaculturalists to slow and capture runoff by spreading it horizontally across the landscape (along an elevation contour line), facilitating runoff infiltration into the soil.

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