Design infiltration rate

This article discusses the determination of a suitable infiltration rate to describe the native soils surrounding a proposed infiltration practice.
It does not relate to the hydraulic conductivity or permeability of filter media or planting media used within vegetated BMPs.

The design infiltration rate (f') is used in all sizing calculations for bioretention and bioswales, dry ponds, infiltration trenches and chambers, and exfiltration trenches. It is related to, but not always synonymous with 'permeability', 'field hydraulic conductivity' (K_fc), or 'saturated hydraulic conductivity' (K_sat). Before application a safety correction factor (SCF) is incorporated into the figure, depending upon the source of the raw data, and the risk of failure of the finished practice.

It is highly recommended that testing be conducted on site.

Sources of data

On site testing methods	Off site analysis methods	Unacceptable methods
Permeameter Double ring infiltrometer Percolation test	Grain size analysis (Hazen)	Single ring infiltrometer Soil textural classification

Becoming familiar with the different measurement practices

STEP have produced a free online module to provide some basic information on infiltration test methods. Access it HERE

Safety correction

To apply conservatism, the measured or calculated infiltration rate may be divided by a value between 2 and 3 before use in design calcualtions

Selecting a safety factor

Lower value (closer to 2)	Higher value (closer to 3)
Catchment < 100 m²	Catchment > 100 m²
Permeameter or percolation test on site	Double ring infiltrometer test on site, or grain size analysis used
Loamy or sandy soil	Clayey soil
No nearby sensitive receptors	Sensitive receptors in near proximity e.g. buildings, foundations or vulnerable natural heritage features.

Planning for testing

Background Evaluation

Prior to performing testing and developing a detailed site plan, existing site conditions should be inventoried and mapped including, but not limited to:

1. Surficial geology and underlying stratigraphy;
2. Watercourses (perennial and intermittent), water bodies, wetlands and floodplains;
3. Small headwater drainage features;
4. Topography, slope, and drainage patterns;
5. Existing land cover and land use;
6. Natural heritage conservation areas; and
7. Other man-made features or conditions that may impact design such as existing nearby structures (buildings, infrastructure, etc.).

A sketch plan or preliminary layout plan for the proposed development should be evaluated, including:

1. The preliminary grading plan and areas of cut and fill;
2. The location and water surface elevation of all existing, and location of proposed water supply sources and wells;
3. The location of all existing and proposed on-site wastewater (septic) systems;
4. The location of other features of note such as utility rights-of-way, water and sewer lines, etc.;
5. Existing data from borehole, well and geophysical testing; and
6. Proposed location of development features (buildings, roads, utilities, etc.).

Sampling

Infiltration testing should be carried out at relevant stages down through the profile of a test pit.

The number of test pits or soil borings varies depending on site conditions and the proposed development plan. General guidelines are as follows:

BMP footprint (m²)	Test pit	Bore hole
< 50	1	1
50 – 900 (alternative)	1	2
	2	0
> 900 (alternative)	1 every 450 m²	2 every 450 m²
	2 every 450 m²	0
Linear	1 every 450 m²	1 every 50 m

• Tests must be conducted within 10 m of the infiltration practice footprint area.
• Where multiple test are carried out, they should be planned equidistant and mapped accordingly.

The recommendations above are guidelines Additional tests should be conducted if local conditions indicate significant variability in soil types, geology, water table levels, depth and type of bedrock, topography, etc. Similarly, uniform site conditions may indicate that fewer test pits are required. Excessive testing and disturbance of the site prior to construction is not recommended.

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The rate at which stormwater percolates into the subsoil measured in inches per hour.

A parameter that describes the capability of a medium to transmit water.

The engineered soil component of bioretention cell or dry swale designs, typically with a high rate of infiltration and designed to retain contaminants through filtration and adsorption to particles.

Sustainable Technologies Evaluation Program

The land draining to a single reference point (usually a structural BMP); similar to a subwatershed, but on a smaller scale.

Referring to the source of a stream or river.

Best management practice. State of the art methods or techniques used to manage the quantity and improve the quality of wet weather flow. BMPs include: source, conveyance and end-of-pipe controls.

The upper surface of the zone of saturation, except where the surface is formed by an impermeable body.

Subsurface water level which is defined by the level below which all the spaces in the soil are filled with water; The entire region below the water table is called the saturated zone.

The slow movement of water into or through a soil or drainage system.

Penetration of water through the ground surface.

The slow movement of water into or through a soil or drainage system.

Penetration of water through the ground surface.