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Last edited 25 Mar 2019
Swales are natural or man-made linear depressions (or ditches), usually grass covered, with shallow-sloping sides. They are becoming more common as components in the drainage strategies of residential, commercial and municipal schemes.
‘…grass-lined channels which transport rainwater from a site as well as controlling flow and quality of surface runoff. Some of the flow infiltrates into the ground. There may be an overflow at the end into another form of infiltration device or a watercourse. They are particularly suitable for treatment of runoff from small residential developments, parking areas and roads.’
Their function is to:
- Slow the movement of water through the landscape after heavy rainfall;
- Reduce peak flows;
- Form a temporary reservoir;
- Direct water to a storage or discharge system and
- Facilitate the absorption of water into the ground.
Swales are frequently located alongside road verges, near the source of water run-off and can form a network linking storage ponds and wetlands. They can constitute an efficient way of capturing rainwater and may form part of a sustainable urban drainage system (SuDS).
They are both sustainable and economic because they are relatively easy to create and can obviate the construction of costly kerbs, gullies and gratings, as well as requiring little maintenance, other than mowing during the growing season. A grass length of around 150mm is considered optimal. Furthermore, swales can form good habitats for toads, newts and other amphibians which might have lower survival rates in conventional man-made gullies.
 How they work
In dry weather, a swale will hold little or no water. After a period of heavy rainfall, water will flow into the swale but its flow will be slowed by the grass which also filters out sediments and organic matter that remain on the top surface to be broken down naturally. Optimum performance of the swale usually relies on shallow slopes – both along the swale and on its sides. Enhanced performance may be achieved by installing check dams across the flow direction in the swale; this will further reduce the rate of flow and lower the erosion risk in the swale.
Further enhancing the swale’s regulating function will be the processes of evaporation, transpiration and infiltration into the surrounding soil. If periods of exceptionally heavy rain are anticipated, overflows can be created to link to watercourses, storage ponds or wetlands.
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- Water Act 2014.
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