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*'''Swale depth''': Swale depth will be estimated based on the relative stage-dependent flow driven cross-sectional area. | *'''Swale depth''': Swale depth will be estimated based on the relative stage-dependent flow driven cross-sectional area. | ||
*'''Additional considerations''': In watersheds with unstable soils or lack of vegetative cover (e.g., construction, farmland and highly impervious surfaces) or where some compaction occurred during construction, [https://stormwater.pca.state.mn.us/index.php/Alleviating_compaction_from_construction_activities compaction should be alleviated] or the [[Design infiltration rates|hydrologic soil classification]] for the site should be downgraded for feasibility study purposes. | *'''Additional considerations''': In watersheds with unstable soils or lack of vegetative cover (e.g., construction, farmland and highly impervious surfaces) or where some compaction occurred during construction, [https://stormwater.pca.state.mn.us/index.php/Alleviating_compaction_from_construction_activities compaction should be alleviated] or the [[Design infiltration rates|hydrologic soil classification]] for the site should be downgraded for feasibility study purposes. | ||
+ | |||
+ | ==Filter media== | ||
+ | Filtration media is comprised of a combination of sand and organic material on top of a pea gravel bed that encases a perforated drain pipe. The media assists in the removal of fine particulate and dissolved pollutants, improving on the overall performance of swale systems. | ||
+ | |||
+ | ===Underdrains=== | ||
+ | Underdrains are comprised of a perforated, PVC pipe laid within filter media to convey runoff to either a stable day-lit area, a second form of treatment, or the storm sewer. A solid-walled PVC section of piping should be connected to the perforated drain pipe with a “tee” junction piece and extended to the swale’s surface to serve as an inspection and cleanout access point. These observation/maintenance ports are spaced throughout the system. | ||
+ | |||
+ | ===Treatment=== | ||
+ | Stormwater treatment in dry swales varies by design, relying on several functions. Organic and mineral sediments suspended in stormwater flows are deposited onto the swale bottom, depending on their size and mass as well as water retention time in a process termed sedimentation. Though swales generally do not detain or retain water for extended periods, this function can be enhanced through the use of check dams or weirs that hold back flows for a design period. The second function in pollutant removal is sorption of particulate matter via the swale’s soils and vegetation as it passes through the system. For dry swales with or without filter media, a portion of the stormwater flows percolate through soil where fine particulate and dissolved pollutants are treated. In fully infiltrating soils, 100% of that portion of pollutant is removed from the surface conveyance to downstream waterbodies, though some shallow ground water connections to nearby water bodies or aquifers should be considered. For swales with filter media and underdrains, a significant portion of non-dissolved contaminants are removed before being conveyed via drain pipe to downstream stormwater treatment practices or a receiving body of water. The last form of treatment swales provide is plant uptake of pollutants. | ||
+ | |||
+ | In most cases, swales are not considered a volume reduction practice unless there is suitable in-situ soil for infiltration to occur, though some volume reduction can occur through evapotranspiration. | ||
+ | |||
+ | ===Vegetation=== | ||
+ | Vegetation plays a crucial role in dry swale treatment capacity, flow attenuation and stabilization of the swale itself (i.e., erosion control). It is HIGHLY RECEOMMENDED that preference is given to robust native, non-clump forming grasses as the predominant plant type within the swale flow area. Care must also be taken to consider species selection in light of sun exposure duration/timing as well as soil moisture, ponding depth and ponding duration. | ||
+ | |||
+ | ==Landscaping== | ||
+ | Swales can be effectively integrated into the site planning process and aesthetically designed as attractive green spaces planted with native vegetation. Because vegetation is fundamental to the performance and function of the swale, aesthetically chosen vegetation may only be possible on the surface of the swales. | ||
+ | |||
+ | ===Snow considerations=== | ||
+ | Considering management of snow, the following are recommended | ||
+ | *Plan a plow path during design phase and tell snowplow operators where to push the snow. Plan trees around (not in) plow path, with a 16 foot minimum between trees. | ||
+ | *Plan for snow storage (both temporary during construction and permanent). Don’t plow into dry swales routinely. Dry swales should be a last resort for snow storage (i.e. only for very large snow events as “emergency overflow”. | ||
+ | *Snow storage could be, for example, a designed pretreatment area. | ||
+ | For more information and example photos, see the section on snow and ice management. | ||
+ | |||
+ | ===Safety=== | ||
+ | Swales do not pose any major safety hazards. Potential hazards could occur from the steep side slope and rock checks of the swales if they are close to pedestrian traffic or roadways with no shoulders. |
This page provides a discussion of design elements and design steps for dry swales, which are often called grass swales. The following discussion includes dry swales used as filtration or infiltration practices, with the distinction being the presence of an underdrain for filtration practices.
The following terminology is used throughout this design page.
HIGHLY RECOMMENDED - Indicates design guidance that is extremely beneficial or necessary for proper functioning of the practice, but not specifically required by the MPCA CGP.
RECOMMENDED - Indicates design guidance that is helpful for practice performance but not critical to the design.
Use this link to access .pdf diagrams of CADD drawings. To see all filtration CADD images in a combined pdf, click here.
Before deciding to use a dry swale practice for stormwater management, it is helpful to consider several items that bear on the feasibility of using such a device at a given location. This section describes considerations in making an initial judgment as to whether or not a dry swale is the appropriate BMP for the site.
The following links provide additional information on specific constraints to infiltration. The Construction Stormwater General Permit prohibits infiltration under certain conditions, which are summarized and discussed in detail at this link.
The RECOMMENDED maximum drainage area is typically 5 acres, although in practicality it is difficult to control the contributing drainage area to a swale.
Unless slope stability calculations demonstrate otherwise (see [1], [2], [3]), it is HIGHLY RECOMMENDED that swales be located a minimum horizontal distance of 200 feet from down-gradient slopes greater than 20 percent, and that slopes in contributing drainage areas be limited to 15 percent
If the swale is constructed as an infiltration practice, the following table summarizes horizontal and vertical setback distances for required and recommended minimum distances from an infiltration practice to an above-ground or underground structure. It will be necessary to consult local ordinances for further guidance on siting infiltration practices.
.
Required and recommended minimum vertical and horizontal separation distances. This represents the minimum distance from the infiltration practice to the structure of concern. If the structure is above-ground, the distance is measured from the edge of the BMP to the structure. If the structure is underground, the vertical separation distance represents the distance from the point of infiltration through the bottom of the system to the structure, while the horizontal separation (often called setback) distance is the shortest distance from the edge of the system to the structure.
Link to this table
Structure | Distance (feet) | Requirement or recommendation | Note(s) | |
---|---|---|---|---|
Vertical | Saturated soil | 3 | Requirement1 | |
Bedrock | 3 | Requirement1 | ||
Horizontal | Public supply well | 100 for sensitive wells; 50 for others3 | Requirement | |
Building/structure/property line2 | 10 | Recommended | ||
Surface water | none unless local requirements exist | If nearby stream is impaired for chloride, see [4] | ||
Septic system | 35 | Recommended | ||
Contaminated soil/groundwater | No specific distance. Infiltration must not mobilize contaminants. | |||
Slope | 200 | Recommended | from toe of slope >= 20% | |
Karst | 1000 up-gradient 100 down-gradient | Requirement1 | active karst |
1 Required under the Construction Stormwater General Permit
2 Minimum with slopes directed away from the building
3If treating an average of 10,000 gallons per day; otherwise separation distance is 300 feet
A separation distance of at least 3 feet is REQUIRED under the MPCA CGP between the bottom elevation of infiltration swales and the elevation of the seasonally high water table. Shallow bedrock areas should be avoided for dry swales with a minimum separation distance of 3 feet.
A field soil properties investigation is HIGHLY RECOMMENDED.
It is HIGHLY RECOMMENDED that infiltration practices not be used in active karst formations without adequate geotechnical testing.
See stormwater and wellhead protection for guidance and recommendations for determining the appropriateness of infiltrating stormwater in a Drinking Water Supply Management Area (DWSMA). For more information on source water protection see Minnesota Department of Health.
See NRCS Web Soil Survey for hydrologic soil descriptions for the swale location. A and B soils are potentially suitable for an infiltration swale. The maximum allowed field-measured infiltration rate shall not exceed 8.3 inches per hour for an infiltration swale.
Several considerations are made in this section for the conceptual design of dry swales. Further design guidance and specifications are made in the following sections.
It is HIGHLY RECOMMENDED that the designer provides non-erosive flow velocities within the swale and at the outlet point to reduce downstream erosion. During the 10-year or 25-year storm (depending on local drainage criteria), discharge velocity should be kept below 4 feet per second for established grassed channels. Erosion control matting or rock should be specified if higher velocities are expected.
If there is space for pretreatment prior to the swale it should be evaluated. Pretreatment should also be considered when runoff entering the swale has high concentrations of sediment. See the pretreatment section for more information.
If the dry swale is being used to meet the Construction Stormwater General Permit, pretreatment is required.
Filtration media is comprised of a combination of sand and organic material on top of a pea gravel bed that encases a perforated drain pipe. The media assists in the removal of fine particulate and dissolved pollutants, improving on the overall performance of swale systems.
Underdrains are comprised of a perforated, PVC pipe laid within filter media to convey runoff to either a stable day-lit area, a second form of treatment, or the storm sewer. A solid-walled PVC section of piping should be connected to the perforated drain pipe with a “tee” junction piece and extended to the swale’s surface to serve as an inspection and cleanout access point. These observation/maintenance ports are spaced throughout the system.
Stormwater treatment in dry swales varies by design, relying on several functions. Organic and mineral sediments suspended in stormwater flows are deposited onto the swale bottom, depending on their size and mass as well as water retention time in a process termed sedimentation. Though swales generally do not detain or retain water for extended periods, this function can be enhanced through the use of check dams or weirs that hold back flows for a design period. The second function in pollutant removal is sorption of particulate matter via the swale’s soils and vegetation as it passes through the system. For dry swales with or without filter media, a portion of the stormwater flows percolate through soil where fine particulate and dissolved pollutants are treated. In fully infiltrating soils, 100% of that portion of pollutant is removed from the surface conveyance to downstream waterbodies, though some shallow ground water connections to nearby water bodies or aquifers should be considered. For swales with filter media and underdrains, a significant portion of non-dissolved contaminants are removed before being conveyed via drain pipe to downstream stormwater treatment practices or a receiving body of water. The last form of treatment swales provide is plant uptake of pollutants.
In most cases, swales are not considered a volume reduction practice unless there is suitable in-situ soil for infiltration to occur, though some volume reduction can occur through evapotranspiration.
Vegetation plays a crucial role in dry swale treatment capacity, flow attenuation and stabilization of the swale itself (i.e., erosion control). It is HIGHLY RECEOMMENDED that preference is given to robust native, non-clump forming grasses as the predominant plant type within the swale flow area. Care must also be taken to consider species selection in light of sun exposure duration/timing as well as soil moisture, ponding depth and ponding duration.
Swales can be effectively integrated into the site planning process and aesthetically designed as attractive green spaces planted with native vegetation. Because vegetation is fundamental to the performance and function of the swale, aesthetically chosen vegetation may only be possible on the surface of the swales.
Considering management of snow, the following are recommended
For more information and example photos, see the section on snow and ice management.
Swales do not pose any major safety hazards. Potential hazards could occur from the steep side slope and rock checks of the swales if they are close to pedestrian traffic or roadways with no shoulders.