This article is about installations designed to capture and convey surface runoff along a vegetated channel, whilst also promoting infiltration.
For underground conveyance systems which promote infiltration, see Exfiltration trenches.
Swales are linear landscape features consisting of a drainage channel with gently sloping sides. Underground they may be filled with engineered soil and/or contain a water storage layer of coarse gravel material. Two variations on a basic swale are recommended as low impact development strategies, although using a combination of both designs may increase the benefits:
Bioswales are sometimes referred to as 'dry swales', 'vegetated swales', or 'water quality swales'. This type of BMP is form of bioretention with a long, linear shape (surface area typically >2:1 length:width) and a slope which conveys water and generally contains various water tolerant vegetation,
Enhanced grass swales are a lower maintenance alternative, but generally have lower stormwater management potential. The enhancement over a basic grass swale is in the addition of check dams to slow surface water flow and create small temporary pools of water which can infiltrate the underlying soil.
Grass swales are a relatively common landscape feature already and a great opportunity for retrofit, to reduce flow and improve water quality by encouraging settling and infiltration behind a series of check dams.
Retention swales can be imagined as linear, sloped dry ponds. They typically make relatively small contributions to water volume and quality control than many other BMPs, but they may feature as part of a site-wide treatment train approach.
Take a look at the downloadable Enhanced Grass Swales Factsheet below for a .pdf overview of this LID Best Management Practice:
Swales are an ideal technology for:
- Sites with long, linear landscaped areas, such as parking lots
- Connecting with one or more other types of LID
|Property||Bioswale||Enhanced grass swale|
Any surface flow can be slowed with check dams
|Ponding is encouraged with check dams|
|Soil||Filter media required||Amendment preferable when possible|
|Maintenance||Medium to high||Low|
|Biodiversity benefit||Increased with native planting||Typically lower|
Enhanced swales and in some cases bioswales include check dams that can be designed to pond substantial volumes of water on the swale surface between flow events, so provide both stormwater conveyance and infiltration functions. For information about constraints to infiltration practices, and approaches and tools for identifying and designing within them see Infiltration. For guidance on infiltration testing and selecting a design infiltration rate see Design infiltration rate.
A linear design (surface area typically >2:1 length:width) is a common feature of swales:
- An absolute minimum width of 0.6 m is required for bioswales to promote healthy plant growth, and to facilitate construction,
- Grassed swales are usually mown as part of routine maintenance, so the cross section will be triangular or trapezoidal in shape with maximum side slopes of 1:3. The minimum width for this type would be 2 m. See Best cross sections
Swales may be graded along longitudinal slopes between 0.5 - 6 %:
- Between 1 - 6 %, check dams are recommended to bring the compensation gradient <1 %.
- Slopes > 6% can accommodate a series of stepped bioretention cells, each overflowing into the next with a spillway.
For a table summarizing information on planning considerations and site constraints see Site considerations.
Pretreatment and inlets
To minimize erosion and maximize the functionality of the swale, sheet flow of surface water should be directed into the side of the BMP. Gravel diaphragms, vegetated filter strips and shallow side slopes are ideal. Alternatively, a series of curb inlets can be employed, where each has some form of flow spreader incorporated. Single point inflow can cause increased erosion and sedimentation, which will damage vegetation and contribute to BMP failure. Again, flow spreading devices can mitigate these processes, where concentrated point inflow is required.
A review of swale-like practices was published by STEP in 1999. The project page and additional tools are available here.
While few field studies of the pollutant removal capacity of bioswales are available from cold climate regions like Ontario, it can be assumed that they would perform similar to bioretention cells. Bioretention provides effective removal for many pollutants as a result of sedimentation, filtering, plant uptake, soil adsorption, and microbial processes. It is important to note that there is a relationship between the water balance and water quality functions. If a bioswale infiltrates and evaporates 100% of the flow from a site, then there is essentially no pollution leaving the site in surface runoff. Furthermore, treatment of infiltrated runoff will continue to occur as it moves through the native soils.
|No underdrain||Washington||>98 %|
|No underdrain||United Kingdom||>94 %|
|With underdrain||Maryland||46 - 54 %|
|Runoff reduction estimate||85 %|
Enhanced grass swales
Simple grass swales
Grass swale in CVC headquarters parking lot, Mississauga ON
Water distributed into a wide grass swale with a rock level spreader
Flow in this wide swale is being reduced by taller vegetation on some sections (See Manning's n)
Streetside swale in Seattle
Bioswale located in Downsview Park, Toronto ON. with Check dams.
Grassed bioswale with Vegetated filter strips
Also see Jen's Pinterest board of check dams
- Horner RR, Lim H, Burges SJ. HYDROLOGIC MONITORING OF THE SEATTLE ULTRA-URBAN STORMWATER MANAGEMENT PROJECTS: SUMMARY OF THE 2000-2003 WATER YEARS. Seattle; 2004. http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.365.8665&rep=rep1&type=pdf. Accessed August 11, 2017.
- Jefferies, C. 2004. Sustainable drainage systems in Scotland: the monitoring programme. Scottish Universities SUDS Monitoring Project. Dundee, Scotland. https://www.climatescan.nl/uploads/projects/8126/files/1277/SNIFFERSR_02_51MainReport.pdf