Testing

A simulated storm event test taking place on porous concrete to ensure proper infiltration function is still occurring in the practice after construction (STEP, 2019)

Soil Characterization Testing

The soil component of an LID BMP contributes substantially to its stormwater treatment performance and overall function. If the soil is overly compacted or very finely textured, it may drain too slowly. If the soil is highly organic or contains excessive amounts of chemical fertilizer it may contribute to nutrient loads to receiving waters rather than reduce them. If the soil is too shallow it may not provide adequate treatment of contaminated stormwater or may not support healthy vegetation. Whether it be the engineered filter media of bioretention cells, the growing media of green roofs or the topsoil of enhanced swales, vegetated filter strips and soil amendment areas, it is important that the soil provide a healthy growing environment for plantings while being within design specifications for key parameters specific to the type of BMP.

It is most important to sample and test soil characteristics as a part of Construction and Assumption inspections, to confirm the BMP has been constructed with materials that meet design specifications and that installation of the soil component is acceptable. Testing to confirm that the material meets quality specifications (i.e., particle-size distribution, organic matter, pH, cationic exchange capacity, nutrients and soluble salts) needs to be completed prior to it being delivered to the construction site. Testing to confirm that installation of the soil component is acceptable (i.e., depth and compaction) should be performed after the installed material has been allowed to settle for at least two (2) weeks, and prior to planting.

Sampling and testing is also recommended as a part of Verification inspections, to determine if the BMP is being adequately maintained and if soil characteristics are still within acceptable ranges. It may also be done as part of Forensic inspection and Testing (FIT) work to help diagnose the cause of poor vegetation cover, drainage or treatment performance and decide on corrective actions.

Critical soil characteristics, acceptance criteria and tests by LID BMP type

LID BMP Type	Soil Characteristic	Acceptance Criteriai	Test
Bioretention / Bioswales / Dry swale
	Textureii	Loamy Sand or Sandy Loam; 70 to 88% sand-sized particles; 12 to 30% silt- and clay-sized particles; <20% clay-sized particles.	Particle-Size Distribution (PSD), or % Sand/Silt/Clay (i.e., Soil Texture) plus Sand Fraction
	Organic Matter (OM)	3 to 10% by dry weightii	Walkley-Black method when OM <7.5% or Loss On Ignition (LOI) method when OM ≥7.5%iii
	Soil pH	6.0 to 7.8	pH of a Saturated Pasteiii
	Cationic Exchange Capacity (CEC)	>10 meq/100 g	Cationic Exchange Capacity Test
	Phosphorusiv	12 to 40 ppm	Extractable Phosphorus
	Soluble Saltsv	≤2.0 mS/cm (0.2 S/m)	Electrical Conductivity of a Soil-Water Slurry (2:1 water to soil ratio by volume)iii
	Depth	+/- 10% of design specification	Soil Cores, Test Pits or Cone Penetration Tests
	Compactionvi	Surface Resistance: ≤110 PSI; Sub-surface Resistance: ≤260 PSI Bulk Density: ≤1.60 g/cm3	Cone Penetration Tests or Bulk Density Tests
	Permeability	i ≥25 mm/h (KS ≥ 1 x 10-5 cm/s); and i ≤203 mm/h (KS ≤ 0.02 cm/s).	Surface Infiltration Rate Tests
Enhanced swale (topsoil)
	Texture	Same soil texture classification as specified in the final design or recorded on the as-built drawing	Particle-Size Distribution (PSD), or % Sand/Silt/Clay (i.e., Soil Texture) plus Sand Fraction
	Organic Matter (OM)ii	5 to 10% by dry weight	Walkley-Black method when OM <7.5% or Loss On Ignition (LOI) method when OM ≥7.5%iii
	Soil pH	6.0 to 7.8	pH of a Saturated Pasteiii
	Phosphorusiv	12 to 40 ppm	Extractable Phosphorus
	Soluble Saltsv	≤2.0 mS/cm (0.2 S/m)	Electrical Conductivity of a Soil-Water Slurry (2:1 water to soil ratio by volume)iii
	Depth	+/- 10% of design specification	Soil Cores, Test Pits
	Compaction	Surface Resistance: ≤110 PSI; Sub-surface Resistance: Use soil texture class and "Soil & Texture Class Table" (below) to determine maximum acceptable value; Bulk Density: Use PSD to interpolate maximum bulk density value from bulk density figure beside this table.	Cone Penetration Tests or Bulk Density Tests
	Permeability	i ≥15 mm/h (KS ≥ 1 x 10-6 cm/s)	Surface Infiltration Rate Tests
Vegetated filter strips and Soil Amendment Areas (topsoil)
	Texture	Same soil texture classification as specified in the final design or recorded on the as-built drawing	Particle-Size Distribution (PSD), or % Sand/Silt/Clay (i.e., Soil Texture) plus Sand Fraction
	Organic Matter (OM)ii	5 to 10% by dry weight	Walkley-Black method when OM <7.5% or Loss On Ignition (LOI) method when OM ≥7.5%iii
	Soil pH	6.0 to 7.8	pH of a Saturated Pasteiii
	Phosphorusiv	12 to 40 ppm	Extractable Phosphorus
	Soluble Saltsv	≤2.0 mS/cm (0.2 S/m)	Electrical Conductivity of a Soil-Water Slurry (2:1 water to soil ratio by volume)iii
	Compaction	Surface Resistance: ≤110 PSI; Sub-surface Resistance: Use soil texture class and "Soil & Texture Class Table" (below) to determine maximum acceptable value; Bulk Density: Use PSD to interpolate maximum bulk density value from bulk density figure beside this table.	Cone Penetration Tests or Bulk Density Tests
	Permeability	i ≥15 mm/h (KS ≥ 1 x 10-6 cm/s)	Surface Infiltration Rate Tests
Green roof (growing media)
	Texture	See product vendor or BMP designer for specifications	Particle-Size Distribution (PSD), or % Sand/Silt/Clay (i.e., Soil Texture) plus Sand Fraction
	Maximum Media Density	See product vendor or BMP designer for specification	Maximum Media Density Test (ASTM E2399/E2399M-15)
	Water Storage Capacityvii	Extensive: ≥35% by volume / Intensive: ≥45% by volume	Both part of Maximum Media Density Test (ASTM E2399/E2399M-15)
	Air-Filled Porosityvii	≥10% by volume	Part of Maximum Media Density Test (ASTM E2399/E2399M-15)
	Permeability, Saturated Media	See product vendor or BMP designer for specification	Part of Maximum Media Density Test (ASTM E2399/E2399M-15)
	Organic Matter	See product vendor or BMP designer for specification	Walkley-Black method when OM <7.5% or Loss On Ignition (LOI) method when OM ≥7.5%iii
	Soil pHviii	6.5 to 7.8	pH of a Saturated Paste
	Soluble Saltsviii	≤0.85 mS/cm (0.085 S/m)	Electrical Conductivity of a Saturated Media Extract (SME)solution
	Phosphorusix	2.2 to 40 ppm	Electrical Conductivity of a Saturated Media Extract (SME)solution

Maximum allowable bulk density values by soil texture class (Sustainable Sites Initiative, 2009). Click to enlarge.

Notes
i Values represent acceptable ranges for established BMPs (i.e., in operation for 3 years or more). For Construction and Assumption inspections, final design and soil or media product specifications and permissible tolerance ranges should be used as the acceptance criteria, which may be smaller ranges than the values in this table.
ii Suggested range for diagnosing suspected problems with drainage function, vegetation cover or vegetation condition for established BMPs constructed with filter media that meets recommended guidelines (CVC & TRCA, 2010). For proprietary filter media products, different ranges may be acceptable. Product specifications should be provided by the media supplier. Test results should be compared to the media supplier’s specifications and permissible tolerance ranges
iii Based on Ontario Ministry of Food and Rural Affairs’ Soil Fertility Handbook guidance on soil fertility testing for crop production (OMAFRA, 2006).
iv Based on Minnesota Pollution Control Agency (MPCA, 2015) for minimum to sustain plant growth and Ontario Ministry of Agriculture, Food and Rural Affairs (OMAFRA, 2014) for a maximum to avoid unnecessary fertilization that would have low or no effect on plant health.
v Based on the threshold for non-saline soils (Whitney, 2011)
vi Interpolated value from bulk density figure beside this table. based on a sandy loam soil containing at least 70% sand-sized particles.
vii Based on German green roof standards (FLL, 2018). Specifications will vary depending on the green roof growing media product. Product specifications should be provided by the media supplier. Test results should be compared to the media supplier’s specifications and permissible tolerance ranges.
viii Based on Penn State University Center for Green Roof Research (Berghage et al. 2008).
ix Based on Penn State University Center for Green Roof Research (Berghage et al. 2008). for the minimum to sustain plant growth and Ontario Ministry of Agriculture, Food and Rural Affairs (OMAFRA, 2014) for the maximum to avoid unnecessary fertilization that would have low or no effect on plant health.

Acceptable Soil Cone Penetrometer Readings (Soil & Texture Class)

Surface Resistancei	'Sub-surface Resistancei
All Soil Textures	Sandy (includes loamy sand, sandy loam, sandy clay loam and sandy clay)	Silty (includes loam, silty loam, silty clay loam, and silty clay)	Clayey (includes clay loam and clay)
≤ 110 PSIii	≤ 260 PSI	≤ 260 PSI	≤ 225 PSI
≤ 7.7 kg/cm2	≤ 18.3 kg/cm2 iii	≤ 18.3 kg/cm2	≤ 15.8 kg/cm2
≤ 758 kPaiv	≤ 1793 kPa	≤ 1793 kPa	≤ 1551 kPa

Notes
i Adapted from Gugino et al. (2009)
ii PSI = pounds per square inch (lb/in2)
iii kg/cm2 = kilogram per square centimetre.
iv kPa = kilopascals

For further information regarding soil characteristics, acceptance criteria per LID BMP type and associated testing tools and protocols scroll down to the embedded 2016 guide below.

Sediment Accumulation Testing

A primary function of LID BMPs is to capture and retain sediment, trash and debris that are suspended in stormwater runoff. Over time, sediment and natural debris accumulates in certain portions of a BMP, particularly in pretreatment devices (e.g., forebays, gravel diaphragms, hydrodynamic separators, vegetated filter strips, grass swales, catchbasin/manhole sumps) and at inlets, where inflowing runoff is slowed down and spread out, which promotes sedimentation of suspended materials by design.

Without adequate inspection and maintenance (at least annually), accumulated sediment and debris in pretreatment devices and inlets can inhibit the flow of stormwater into the BMP or be transported onto the filter bed . Extensive sediment accumulation on the surface of a filter bed will eventually lead to drainage problems due to clogging of the filter media with fine-textured sediment. When sediment accumulation on the surface of a filter strip or swales becomes excessive the BMPs begin to export sediment and associated pollutants into receiving waters rather than retain them.

Key Components, Test Methods and Equipment

Key components of LID BMPs that should be the subject of sediment accumulation testing (i.e., depth measurements) are described in the table below along with recommended test methods. Depth measurements should be recorded on inspection field data forms provided on each associated BMP's I&M page on the wiki, used to determine if sediment removal maintenance is needed.

Picture of a typical Secchi disk to help measure sediment depth in underground holding structures. (Photo Source: Wildco, 2018)

Key components and test methods for sediment accumulation testing by BMP type

LID BMP Type	Key Components	Recommended Test Method
Bioretention / Bioswales / Dry swale / Enhanced grass swales / Vegetated filter strips
	Inlets; Pretreatment devices	Use a tape measure or probe to measure the depth from the bottom elevation of the pretreatment device or surface of the filter bed (adjacent to the inlet structure), below any stone or mulch cover present, to the highest elevation of accumulated sediment present. For catchbasins, manholes and hydrodynamic separator pretreatment devices a sludge sampler (e.g., “sludge judge” sampler) should be used to sample the sediment and estimate depth accumulated in sumps. Record the measurement and remove the sediment if it exceeds trigger values for follow-up action.
	Filter Bed	Use a tape measure or probe to measure sediment depth from the surface of the filter bed, below any stone or mulch cover present, to the elevation of accumulated sediment present in at least five (5) locations evenly distributed over the filter bed surface area. Record the measurements, calculate the mean sediment depth and compare to trigger values to determine if follow-up/corrective actions are needed.
Underground infiltration systems (Soakaways, infiltration trenches, infiltration chambers and perforated pipe storm sewer systems
	Inlets; Pretreatment devices	Use tape measure or probe to measure the depth from the bottom elevation of the inlet pipe or pretreatment device, below any stone or mulch cover present, to the highest elevation of accumulated sediment present. For catchbasins, manholes and hydrodynamic separator pretreatment devices a sludge sampler (e.g., “sludge judge” sampler) should be used to sample the sediment and estimate depth accumulated in sumps. A measuring tape or staff gauge installed in the structure and set to the bottom elevation can provide another means of tracking sediment accumulation. Record the measurement and remove the sediment if it exceeds trigger values.
	Filter Bed	(Applicable to vault-type infiltration chamber systems only) - Use a tape measure or probe to measure sediment depth from the surface of the gravel bed to the elevation of accumulated sediment in at least five (5) locations evenly distributed over the bed surface area. Record the measurements, calculate the mean sediment depth and compare to trigger values to determine if follow-up/corrective actions are needed.
Cisterns (Rainwater Harvesting & Rain barrels)
	Cistern	From outside the cistern use a tape measure or probe to measure the depth from a fixed point (e.g., rim of the access hatch) to the bottom elevation of the cistern and to the highest elevation of accumulated sediment present. Subtract the two values to calculate the sediment depth. A sludge sampler (e.g., “sludge judge” sampler) may also be used to sample the sediment and estimate depth. A staff gauge installed on the cistern wall and set to the bottom elevation provides another means of measuring sediment depth that does not require entry into the confined space. Record the measurement and remove the sediment if it exceeds trigger values for follow-up action.

Measuring sediment depth in a catchbasin utilizing the "two prong method" (Photo Source: King County, 2010)

Standard Equipment Used

Equipment needed for sediment accumulation testing can include the following:

• Safety apparel (hard hat, steel toed boots, gloves and eye protection)
• Safety cones or barriers (for restricting access around open hatches/grates/manhole covers)
• Clipboard, inspection field data forms, pens
• Pick shovel (for opening catchbasin grates or manhole covers)
• Measuring tape
• Probe (rigid)
• Secchi disk
• Sludge sampler
• Rope
• Flashlight or headlamp
• Harness
• Tripod (certified and tested)
• Winch (certified and tested)
• Multi-gas detector (recently calibrated and tested)

Sediment accumulation testing should be conducted frequently during construction (e.g., weekly and after any storm event of 15 mm depth or greater), as part of Assumption inspection work, once construction is fully completed and sediment accumulated on the CDA, in conveyances (e.g., gutters, catchbasins, storm sewers) and pretreatment devices has been removed, and as part of Routine Operation and Verification inspections.

For further information regarding soil characteristics, acceptance criteria per LID BMP type and associated testing tools and protocols scroll down to the embedded 2016 guide below.

Surface Infiltration Rate Testing

For LID BMPs like bioretention and bioswales, enhanced swales, vegetated filter strips and permeable pavements, the rate at which stormwater infiltrates through the BMP surface greatly affects its drainage performance. If the surface infiltration rate (i) is too low, inflowing stormwater will quickly begin to pond on the surface and, once the overflow outlet elevation is reached, will by-pass treatment by the BMP. In extreme cases the BMP may pond water on the surface for longer than 24 hours, creating nuisance conditions (e.g., poor vegetation cover, ice formation, ideal mosquito breeding ground habitat).

Causes of excessively low surface infiltration rates include use of soil during construction that does not meet design specifications, accumulation of fine sediment on the soil surface or in permeable pavement joints or pore spaces, and over-compaction of the soil, that can occur during construction or routine operation. Therefore it is important to test the surface infiltration rate of LID BMPs as part of Assumption and Verification inspections. As part of Assumption inspections it helps determine if the BMP is ready to be assumed by the property owner. As part of Verification inspections it provides an indication of whether or not the surface drainage performance of the BMP is still within an acceptable range, if it is being adequately maintained, and to diagnose the cause of any problems with drainage or vegetation detected through visual inspection or other types of testing. Tests may also be done as part of Forensic Inspection and Testing (FIT) work to diagnose the cause of problems with drainage or vegetation, with the number and locations of test determined by the nature of the problem being investigated.

Surface infiltration rate testing involves estimating the saturated hydraulic conductivity (K_S) of the BMP surface through measurement at several locations and calculation of an average value. A single measurement can take anywhere from 15 minutes to several hours (Erickson et al., 2013) depending on soil or surface characteristics.

Filter Bed Surface Infiltration Rate

To evaluate surface infiltration rate using a surface ponding well during a simulated storm event, the filter media bed should be thoroughly wetted prior to the test. Measurements of filter bed drainage rate and corresponding estimates of surface infiltration rate should be made following natural or simulated storm events that deliver enough water to the BMP to pond at least 75 mm of water on the surface of the filter media bed, in an effort to consistently approximate saturated soil flow conditions.

Calculation

Filter Bed Surface Infiltration Rate: $(i)$ = 50 $mm$ / ΔT₅₀

Where
ΔT₅₀ = Time to drain last 50 mm of surface ponded water
ΔT₅₀ = (T₂ – T₁) x 24
T₁ = Post-storm date and time (mm/dd/yyyy hh:mm:ss) when surface ponding water level reaches 50 mm in depth.
T₂ = Post-storm date and time (mm/dd/yyyy hh:mm:ss) when surface ponding is fully drained

BMP Components and Test Methods

Key components of LID BMPs that should be the subject of surface infiltration rate testing are described in the table below along with recommended test methods.

Key components for surface infiltration rate testing by BMP type and test methods

LID BMP Type	Key Components	Recommended Test Method
Bioretention / Bioswales / Dry swale / Enhanced grass swales / Vegetated filter strips
	Filter bed surface	Use an infiltrometer or permeameter to measure field saturated hydraulic conductivity (KS) in at least 5 locations or at a rate of one measurement for every 25 m2 of filter bed surface area, including inlet and lowest elevation areas. Compare mean and individual values to the design specification or trigger value (See Triggers for follow-up and corrective actions below) to determine if follow-up tasks are needed.
Permeable pavement
	Pavement surface	Use a single-ring infiltrometer to measure field saturated hydraulic conductivity (KS) in at least 5 locations or at a rate of one measurement for every 250 m2 of pavement surface area, evenly distributed. For permeable interlocking pavers, follow the procedure provided by ASTM C1781_C1781M – 15 (ASTM International, 2015). For pervious concrete or porous asphalt, follow the procedure provided by ASTM C1701_C1701M – 09 (ASTM International, 2009). Compare mean and individual values to the design specification or trigger value (See Triggers for follow-up and corrective actions below) to determine if follow-up tasks are needed.

Common Methods for Surface Infiltration Rate Testing

Description of common methods for surface infiltration rate testing

Method	Description	Photo Example
Double Ring Infiltrometer (constant head)	The double-ring infiltrometer (See photo example - Source: TRCA, 2012) is made of two concentric tubes typically of thin metal or hard plastic, that are both continuously filled with water such that a constant water level is maintained as water infiltrates into the soil (ASTM International, 2005). The rate at which water is added to the centre tube is measured to determine the infiltration rate. For detailed guidance on how to perform the testing, refer to ASTM D3385-09 Standard Test Method for Infiltration Rate of Soils in Field Using Double-Ring Infiltrometer (ASTM International, 2018) and ASTM D5093-15 Standard Test Method for Infiltration Rate of Soils in Field Using Double-Ring Infiltrometer with Sealed-Inner Ring (ASTM International, 2018 Accuracy is only moderate relative to permeameter methods (ASTM International, 2010) and results tend to be biased towards higher values due to lateral flow. Potentially requires large volume of water and significant length of time for each measurement to reach steady state.
Single Ring Infiltrometer (constant or falling head)	Similar to the double-ring infiltrometer, except with only one ring (See photo example - Source: Werner, 2010) Can be used to measure the vertical movement of water through a soil or permeable pavement. The standard design is a ring that is 30 cm in diameter and 20 cm tall, driven 5 cm into the soil or sealed to the surface of a permeable pavement and filled with water (Klute, 1986). For detailed guidance on how to perform the testing on permeable interlocking pavers, follow the procedure provided by ASTM C1781_C1781M – 15 (ASTM International, 2015). For pervious concrete or porous asphalt, follow the procedure provided by ASTM C1701_C1701M – 09 (ASTM International, 2009). Accuracy for soil testing is only moderate relative to permeameter methods (ASTM International, 2010). and results tend to be biased towards higher values due to lateral flow. Potentially requires large volume of water and significant length of time for each measurement to reach steady state when used for soil testing.
Modified Philip Dunne Infiltrometer (falling head)	The Modified Philip-Dunne infiltrometer (See photo example - Source: Ahmed et al. 2011) is a falling head test device made of an open ended 50 cm long clear plastic cylinder with 2 mm thick walls, a 10 cm inner diameter and graduations, inserted into a machined metal base. Unlike the Philip-Dunne permeameter, which requires digging a borehole (i.e., not a surface infiltration test method), it is inserted 5 cm into the surface of the soil without the need for removing vegetation cover. Water level measurements in the tube can be obtained using the graduations on the side of the cylinder and a stopwatch, or continuously recorded through use of a data logger and pressure transducer installed in a piezometer tube. Measurements of soil moisture (e.g., using a handheld soil moisture probe) are needed before and after each test. Using relationships established by Ahmed and Gulliver (2011), the observed infiltration rate and initial and final soil moisture measurements are used to calculate a value for saturated hydraulic conductivity. A quicker test to perform than constant head tests. Superior to the single-ring infiltrometer falling head test as lateral flow is incorporated into the calculations.
Guelph Permeameter with Tension Disk (constant head)	The Guelph permeameter (See photo example - Source: Hoskin Scientific Ltd., 2022)is another test device for measuring saturated hydraulic conductivity of a soil surface when used with a tension disc attachment. The method is similar to a Tension infiltrometer, but with water being directed to the tension disc from an inner or outer Mariotte reservoir, giving it the capacity to test low and high permeability soils (Soil Moisture Equipment Corp. 1986. Infiltration rates are calculated from monitoring the water level drop in the reservoir until a steady state is approached. Like the Tension infiltrometer method below, tests are run with two applied tensions. Steady state infiltration rates from the two applied tensions are used to calculate a value for saturated hydraulic conductivity. Potentially requires large volume of water and significant length of time for each measurement to reach steady state.
Tension Infiltrometer (constant or falling head)	This test involves a porous disc of 10 or 20 cm diameter that is connected to a Marriotte bottle (water reservoir) and a bubbling tower where a negative pressure or tension is set (See photo example - Source: ICT International, n.d.). The porous disc must be placed in contact with the soil surface which usually requires removal of any vegetation and debris. In many cases it is necessary to place a thin layer of fine sand onto the soil surface to provide good contact between the disc and the soil. Infiltration rates are measured based on the water level drop in the water reservoir. The steady state infiltration rate into the soil is measured for two applied water pressures. To estimate saturated hydraulic conductivity the pressures need to be slightly negative (i.e., tensions) and it is recommended that successive pressures of -5 cm and -1 cm be used (Erickson et al., 2013). The measured steady state infiltration rates are used in equations derived by Reynolds and Elrick (1991) For detailed guidance on how to perform the testing, refer to Reynolds and Elrick (1991). The Mini-disc Tension infiltrometer (4.5 cm porous disc) uses a falling head method developed by Zhang (1997) to estimate saturated hydraulic conductivity. It is a quicker test to perform than the constant head method but potentially more difficult to achieve adequate contact with the soil surface.

Standard Equipment Used

Equipment needed for surface infiltration rate testing will vary depending on the chosen test method (constant head and falling head methods) but can include the following:

• Safety apparel (steel toed boots)
• Safety cones or barriers (for restricting access when testing permeable pavements)
• Clipboard, inspection field data forms, pens
• Testing instrument (e.g., infiltrometer or permeameter) and instruction manual
• Stopwatch
• Water reservoir (e.g., truck mounted tank or cistern filled with water)
• Buckets or jugs (for filling the instrument)
• Plastic graduated cylinder (for measuring volume of water added during constant head infiltrometer tests)
• Soil moisture probe
• Fine sand (for even contact between Tension infiltrometer and soil surface)

Triggers for Follow-Up and Corrective Actions

Surface infiltration rate – triggers for follow-up and corrective actions by BMP type

BMP Type	Trigger	Follow-up and Corrective Actions
Bioretention / Bioswales / Stormwater Tree Trenches / Stormwater planters and Dry swales (filter media bed surface)	i < 25 mm/h; KS < 1 x 10-5 cm/s i > 203 mm/h; KS 0.02 cm/s	When part of an Assumption inspection, issue a stop work order and contact the construction site supervisor, design professionals and property owner or project manager to determine follow-up tasks. Follow-up tasks involve scheduling FIT work to do further testing to determine the affected area and depth and decide on corrective actions. Corrective actions may involve removal of any accumulated sediment, mulch or stone cover and plantings and tilling of the top 20 to 30 cm of filter media to eliminate surface crusting or macropores and reduce compaction. Alternatively, removal and replacement of all or the uppermost 15 cm of filter media with material that meets design specifications may be necessary.
Permeable pavements (pavement surface)	i < 250 mm/h	When part of an Assumption inspection, issue a stop work order and contact the construction site supervisor, design professionals and property owner or project manager to determine follow-up tasks. Follow-up tasks involve scheduling FIT work to do further testing to determine the affected area and decide on corrective actions. Corrective action should first involve thoroughly sweeping and vacuuming the affected pavement area when dry in an attempt to remove sediment accumulated in the pavement joints or pore spaces. If vacuuming does not restore surface infiltration rate to an acceptable value (i.e., ≥ 250 mm/h) try manual or pressure washing means to remove surface crust and sediment from paver joints or pore spaces. In extreme cases, removal of the affected portion of the surface course and bedding and reinstallation with materials that meet design specifications may be necessary.
Enhanced swales / Vegetated filter strips & Soil Amendment Areas (topsoil surface)	i < 15 mm/h; KS < 1.5 x 10-6 cm/s	When part of an Assumption inspection, issue a stop work order and contact the construction site supervisor, design professionals and property owner or project manager to determine follow-up tasks. Follow-up tasks involve scheduling FIT work to do further testing to determine the affected area and depth and decide on corrective actions. Corrective actions may involve removal of any accumulated sediment and plantings and tilling of the topsoil to between 20 and 30 cm depth to eliminate surface crusting, increase porosity and reduce compaction. If testing indicates low organic matter content, topsoil should be amended with compost prior to tilling.

For further information regarding soil characteristics, acceptance criteria per LID BMP type, associated testing tools and protocols along with corrective actions, scroll down to the embedded 2016 guide below.

Natural or Simulated Storm Event Testing

Example of a simulated storm event test being conducted in a bioswale with a large water truck. (Source: TRCA, 2016)

For LID BMPs that receive stormwater via conveyances like gutters, concrete inlets and leader pipes from roofs or catchbasins (i.e., bioretention and bioswales, enhanced swales, soakaways, infiltration trenches, exfiltration trenches infiltration chambers and soil cells) it is critically important to confirm that these conveyances have been designed and constructed properly. If the conveyances are obstructed or improperly graded or constructed, the BMP may not receive flows from their CDA or a significant quantity of stormwater may by-pass treatment. This is particularly important for underground BMPs where inlets are not visible from the surface. Therefore, confirming that these types of BMPs actually receive stormwater from their CDA should be a part of Assumption and Verification inspections.

The simplest approach to confirming that conveyances to LID BMPs are constructed properly and functioning well is through observation of the path of water flow and measuring water level in the BMP during a natural storm event. If timelines for completing inspections cannot be coordinated to coincide with a natural storm event, an alternative approach is to simulate a storm event over the CDA by directing water onto it through the use of a water tanker truck or fire hydrant while observing conveyances and measuring water level in the BMP. Such testing not only confirms that conveyances to the BMP are functioning properly but also helps to confirm the size of the CDA (i.e., that site grading is correct) and that sub-drain systems are functioning properly.

Natural or simulated storm event testing can also be undertaken to confirm that an LID BMP drains at an acceptable rate. Designing such tests is much more involved and requires the deployment of specialized field monitoring equipment like continuous water level loggers (i.e., pressure transducers) in monitoring wells, flow measurement apparatuses (e.g., area-velocity sensors) in sub-drain or outlet pipes and rain gauges, in addition to staff familiar with the use and calibration of such equipment and the processing and analysis of the data. See the "Continuous Monitoring Section" below which provides guidance on the utility and design of continuous monitoring programs along with key references for further reading.

If the primary objective of natural or simulated storm event testing is only to confirm that conveyances are delivering stormwater to the BMP, this is easily done by observing where water flows as it is delivered to the CDA. Prior to and after the release of water, measurements of water level in monitoring wells should be made and recorded to be able to detect whether or not flows are reaching the water storage portion of the BMP if it cannot be observed visually. Manual water levels measurements can be taken by lowering a rod, level tape or string with a weight on the end into the well until the bottom is reached and measuring the height of water present from the maximum water level indicated on the device.

• Water level can also be measured using a pressure transducer installed to just above the bottom of the well and set to continuously record water level at 1 minute intervals. For BMPs that contain sub-drains that can be accessed and visually inspected, observations should be made to determine if flow from the sub-drain pipe occurs following delivery of water to the BMP.

Standard Equipment Used

Equipment needed for natural or simulated storm event testing will vary depending on the BMP type, objectives of testing and the chosen method but can include the following:

• Water source of sufficient quantity (e.g., water truck, fire hydrant, truck mounted cistern)
• Safety apparel (steel toed boots)
• Safety cones or barriers (for restricting access when testing permeable pavements)
• Clipboard, inspection field data forms, pens
• Camera
• Water level tape or dip stick
• Measuring tape
• Surface ponding well
• Sub-surface water storage reservoir monitoring well
• Pressure transducers data logger (optional ,for detecting water level change in sub-drains)
• Hydrant coupling kit (for connecting to fire hydrant)
• Magnetic flow meter and data logger (for measuring quantity of water delivered to the BMP)
• Pipes (to distribute flow to the CDA or BMP itself)
• Pipe couplings (to connect water truck or fire hydrant hose/nozzle to flow meter and distribution pipes);
• Pick for opening manholes or catch basin grates;
• Multi-gas sensor (for safe access of manholes or catch basins)

Acceptance Criteria

Acceptance criteria for LID BMP drainage performance for both natural and simulated storm event testing:

1. Water flows into the BMP as intended;
2. For bioretention, bioswales and enhanced swales, the surface water storage reservoir (i.e., surface ponding) fully drains within 24 hours of the end of the storm;
3. For bioretention and bioswales, the filter bed surface infiltration rate ≥25 mm/h and ≤203 mm/h, or consult manufacturer or vendor for an acceptable range specific to the filter media product.
4. For enhanced swales, vegetated filter strips and Absorbent landscapes / soil amendment areas, the surface infiltration rate ≥15 mm/h and ≤203 mm/h, or consult manufacturer or vendor for an acceptable range specific to the topsoil product.
5. For newly constructed BMPs (i.e., Assumption inspection), the active sub-surface water storage reservoir volume drains within 48 to 72 hours of the end of the storm and sub-drain peak flow rate is within +/- 15% of design specification; and,
6. For aged BMPs (i.e., Performance Verification inspections), active sub-surface water storage reservoir volume drains within 48 to 96 hours of the end of the storm and sub-drain peak flow rate is within +/- 15% of design specification.

For further information regarding natural and simulated storm event testing, acceptance criteria per LID BMP type and associated testing tools and protocols scroll down to the embedded 2016 guide below.

Continuous Monitoring

Continuous monitoring is the most comprehensive approach to inspection of stormwater BMPs that can provide quantitative information about drainage and water treatment performance during actual storm events, which can be directly compared to design specifications and regulatory criteria to determine if it is functioning and performing as intended. Continuous monitoring is the most costly and time-consuming approach to inspection, but warranted in certain situations.

At a minimum, continuous monitoring should be undertaken as part of Assumption and Verification inspections in the following situations:

1. For infiltration BMPs designed without sub-drains to determine active sub-surface water storage reservoir volume drainage time and filter bed surface infiltration rate.
2. For infiltration BMPs designed with flow-restricted sub-drains, to determine sub-drain peak flow rate, active sub-surface water storage reservoir volume drainage time and filter bed surface infiltration rate.
3. As part of Forensic inspection and Testing (FIT) work to determine corrective actions for suspected problems with drainage or effluent quality detected through other inspection and testing work.
4. When little information is available about the effectiveness of a certain type of BMP in a certain environmental context, or when a new technology is being implemented for the first time in a certain context or geographic region.
5. Where the sensitivity of the receiving water warrants a high level of inspection and testing to determine if BMP effluent quality meets design specifications or regulatory criteria.

External guidance on monitoring the performance of stormwater BMPs

Diagram of a typical water level logger installation in an infiltration BMP sub-surface water storage reservoir monitoring well (City of Philadelphia, 2014).

• Optimizing Stormwater Treatment Practices: A Handbook of Assessment and Maintenance (Erickson et al., 2013);
• Technical Guidance Manual for Evaluating Emerging Stormwater Treatment Technologies (Washington State Department of Ecology, 2018);
• Urban Stormwater BMP Performance Monitoring (Geosyntec Engineers and Wright Water Engineers, 2009);
• Center for Watershed Protection, Managing Stormwater Post-Construction Guide, BMP Performance Verification Tool (Tool 8) Appendix A (CWP, 2008)
• Green Cities, Clean Waters Comprehensive Monitoring Plan, Appendices C and D (City of Philadelphia, 2014)

Drainage Performance Evaluations

It is recommended that at a minimum, the drainage performance of stormwater infiltration BMPs be evaluated as part of Assumption and Verification inspections. Drainage performance, or the ability of the BMP to fully drain runoff from a certain size storm event within a certain time period, can be evaluated by continuous monitoring during natural or simulated storm events. When a water source of sufficient size to fill the sub-surface water storage reservoir is available, it is recommended that drainage performance evaluations be performed by simulated storm event testing as results can be produced within a much shorter time period (e.g., within a week) as opposed to natural storm event testing, which can require field monitoring activities over 6 months to 2 years in duration.

The general approach involves installing water level logger sensors (i.e., pressure transducers) in:

• a perforated standpipe on the BMP surface to measure the time required to drain water ponded on the surface (i.e., the surface water storage reservoir component) and estimate filter bed surface infiltration rate; and,
• a monitoring well screened within the sub-surface water storage reservoir component of the BMP

Simulated Storm Event Test Procedures

For infiltration BMPs designed with flow-restricted sub-drains, continuous monitoring to evaluate drainage performance should be performed by conducting a simulated storm event test using the following stepwise procedure below:

1. Select a date for the test when no rainfall is forecast for at least 3 days.
2. Install flow monitoring apparatus downstream of the sub-drain flow restrictor device.
3. Temporarily plug the sub-drain pipe.
4. Direct enough water to the BMP to completely fill the sub-surface water storage reservoir.
5. Remove the sub-drain plug.
6. Allow the BMP to fully drain.
7. Determine the maximum flow rate from the sub-drain from flow measurements
8. Determine the drainage time from the water level measurements
9. Calculate the infiltration rate based on water level measurements once flow from the subdrain has stopped as the change in storage volume over time divided by the infiltration area.
10. If more than 13 m³ of water (i.e., the typical capacity of water tanker trucks) is needed to fill the sub-surface water storage reservoir, a fire hydrant will need to be used as the water source.

For infiltration BMPs that contain unrestricted sub-drains, continuous monitoring to evaluate drainage performance should capture the full drainage periods for at least one storm event large enough to completely fill the sub-surface water storage reservoir to the elevation of the sub-drain pipe invert or at least 3 rain events between 15 and 25 mm in depth.

• Mean values for drainage time and infiltration rate should be calculated and compared to design specifications or regulatory criteria to determine if the BMP is draining at an acceptable rate.
• Alternatively, a simulated storm event test can be performed, using the stepwise procedure described above.

Water Treatment Performance Evaluations

When the objectives of BMP inspection include determining if the BMP is providing a minimum level of water treatment performance, design of the continuous monitoring program needs considerable thought. Table 8.10 describes some key considerations in program design.

Key considerations in designing continuous monitoring programs for water treatment evaluation.

Variable	Key Considerations	Recommendations
BMP Water Storage Capacity	Many LID BMPs contain sub-drains that only flow during large storm events which will limit the number of events that produce water samples in a given year.	Focus on BMPs that generate outflow during storm events of 25 mm depth or less. Budget for continuous monitoring periods of 6 months to 2 years to capture samples from enough storm events to produce meaningful results (at least 15) with site visits every 2 weeks to check on equipment and download and QA/QC check data.
Inlet configuration	Measuring and sampling inflow is often not feasible for BMPs that receive sheet flow or have multiple inlets.	Parallel measurement and sampling of outflow from a nearby, untreated drainage area is needed to evaluate water treatment performance of BMPs where inlet monitoring is not feasible.
Flow-Weighted Sampling Method	How individual water samples are combined to produce the composite sample for laboratory testing will greatly affect results.	Composite samples should be generated by examining flow rate over the period each sample was taken, calculating what proportion of the total flow during the event that represents, and using this relationship to measure the quantity taken from each sample bottle to produce the composite sample.
Storm Event Size and Duration	To adequately characterize water treatment performance, monitoring results from a range of storm event sizes is needed which requires that the programming of automated water samplers should be capable of capturing flow from a range of storm event depths and durations.	Start with collecting 500 mL aliquots every 10 minutes after flow is initiated. For an automated water sampler that contains 24 one litre bottles, this allows sampling over an 8 hour period. Sampling frequency should be adjusted to optimize between filling all the bottles in the sampler with capturing as much of the period of flow as possible. Alternatively, automated samplers can be coupled with flow measurement apparatuses to alter sampling frequency as flow rate changes.
Water Quality Parameters of Interest	The cost of laboratory testing of water samples increases with the number of parameters to be tested. Water treatment performance evaluations should focus on the parameters of greatest concern from regulatory or receiving water sensitivity perspectives.	As most pollutants common to urban stormwater runoff are associated with suspended solids, focus on evaluating Total Suspended Solids (TSS) removal efficiency. For nutrient-limited receiving waters, add nutrient testing (Total Phosphorus and Phosphate, Total Nitrogen, Nitrate and Nitrite). For bacteria limited receiving waters add bacteria testing. When bacteria removal performance is to be evaluated, samples must be submitted for laboratory testing within 48 hours of the end of the storm event or refrigerated samplers are needed.
Security of Monitoring Equipment	In some cases, monitoring equipment will need to be installed at the ground surface, and require means of preventing tampering or sabotage.	House automated water samplers in protective structures that are securely locked and inaccessible. Samplers should also be placed directly into manholes where possible.
Confined Space Entry	Installing and checking flow monitoring and sampling equipment often requires entry into confined spaces.	Monitoring that involves confined space entry requires adequately trained staff equipped with certified and recently calibrated safety equipment.

Water quality analysis testing taking place in an accredited lab (Photo Source: City of Markham, n.d.).

Accredited Water Testing Laboratories (ON)

• Accuracy Environmental Laboratories Ltd.
• AGAT Laboratories Ltd.
• ALS Laboratory Group (Env. Division)
• Caduceon Environmental Laboratories
• City of Hamilton Environmental Laboratory
• City of Ottawa Laboratory Services
• Exova Canada Ltd. - Now "element"
• Maxxam Analytics - Now Bureau Veritas
• Ontario Ministry of the Environment Conservation & Parks (MECP)
• Paracel Laboratories
• Regional Municipality of Waterloo, Environmental Laboratory
• Testmark Laboratories Ltd.
• Toronto Water Laboratory
• York-Durham Regional Environmental Laboratory

For further information regarding natural and simulated storm event testing, acceptance criteria per LID BMP type and associated testing tools and protocols scroll down to the embedded 2016 guide below.

Green Roof Irrigation System Testing

In dry or temperate climates, an irrigation system can be crucial for establishing and maintaining green roofs. Extensive green roofs planted with drought tolerant plants do not always need an irrigation system, but intensive green roofs planted with a wider variety of plants would not be able survive without one. Most green roofs will require supplemental water either to enhance or speed up the establishment process or to protect the plantings during times of sustained drought. This can be accomplished by hand watering or installing an automated irrigation system.

Picture of a spray nozzle used in an automatic spray irrigation system on a green roof (Photo Source: Vegetal I.D., n.d.)

Irrigation systems vary greatly in level of complexity:

• Simply hand watering systems using hose bibs on the roof and manual sprayers;
• Installed automated systems that are activated by timers; or,
• Sophisticated “smart irrigation” systems that can be remotely controlled and coupled with rain sensors or sources of local weather data to only operate during extended dry periods (i.e., droughts).
  • Drip irrigation is the most common type of irrigation system for green roofs because it transfers the water directly to the growing medium via drip emitters installed at or near the surface with relatively little loss to evaporation.
  • Other types of irrigation systems use handheld or installed spray nozzles to distribute water to the plants. If an automatic irrigation system is in place, individuals performing inspection testing, maintenance and repairs on it should refer to the operator’s manual from the product vendor or installer for instructions specific to that product.

Triggers for Corrective Action

A green roof irrigation system test involves:

1. inspecting the supply lines,
2. fittings and
3. distribution points (e.g., drip emitters or spray heads)

All while the system is running to check for leaking, damaged, obstructed or misaligned components and dry or saturated portions of the filter bed/growing medium.

Triggers for Action include:

1. A leaking or damaged supply line will often wash out or saturate a small area.
2. An obstructed drip emitter or spray nozzle will create dry spots.
3. If visual assessments of vegetation cover and condition reveal locations where plantings have died or are not thriving, make sure it is not due to irrigation system malfunction or damage.
4. If the irrigation system test results in ponding on the filter bed/growing medium surface or in/around overflow outlets, repair or routine maintenance of those components may be necessary.

Green Roof Leak Detection Testing

On buildings featuring a green roof, a waterproofing membrane layer that covers the whole roof is essential to prevent water damage to the building. In some cases, a root barrier layer is also a part of the green roof design that protects the waterproofing membrane from being penetrated by roots and degraded by soil microbial activity. On top of these protective layers are the water retention and drainage layer, filter cloth, growing media and plants, making it impossible to visually inspect them for damage or leaks. There are two main approaches to leak detection for green roofs – flood tests and low-voltage leak detection tests.

A technician checking for water penetration below the membrane of a green roof by conducting a low-voltage leak detection test (Source: Construction Canada, 2012)

Flood Tests

Flood tests for detection of green roof leaks can be conducted as part of Construction inspections, prior to planting. The test requires an experienced professional to narrow down a small area where the leak may be originating from. The suspected area is isolated from the rest of the roof, the roof drains are plugged, 10 cm of water depth is introduced and observations are made. Once the leak is found, the area is opened up and the waterproofing membrane is repaired. This process is time-consuming and costly, as the leak is not always found during the first round of patch flooding (US GSA, 2011)

Low-Voltage Leak Tests

The low-voltage leak detection test utilizes electricity to locate water penetrations through the waterproofing membrane. Such leak detection systems can also be referred to as Electric Field Vector Mapping (EFVM®) systems. They require a grounded, conductive material be directly below the waterproofing membrane, such as reinforced concrete or metal, and that the membrane be a nonconductive material. During roof construction and prior to green roof installation, a conductive wire is looped around the surface of the waterproofing membrane and connected to an impulse generator.

Testing involves the inspector or leak detection technician introducing a low-voltage, pulsating electric charge onto the surface of the waterproofing membrane which should be moist at the time. A watertight membrane will isolate the potential difference between the wetted surface and the underlying grounded conductive material layer, while breaches in the membrane will cause an electrical connection to occur. The inspector or leak detection technician reads the directional flow of current with a potentiometer to locate the point of entry with pinpoint accuracy. Low-voltage leak detection tests can be performed before and after a green roof is installed. As such, the location of leaks can be very precisely located and repaired with minimal disturbance to the rest of the roof (US GSA, 2011).

Testing & Inspection Types

It is important to test green roofs for leaks as part of Construction, Assumption and Verification inspections.

• As part of Construction inspections, testing confirms that the roof layers have been installed correctly and that it is ready for planting.
• As part of Assumption inspections it helps determine if the green roof is ready to be assumed by the property owner/manager/municipality.
• Tests may also be done as part of Verification inspections (i.e., every five years) to check for leaks, and as part of FIT work to locate and repair leaks discovered through visual inspection work.

Cistern Pump Testing

A simplified cross-section view showing key components of a rainwater harvesting system used in a residential setting. The cistern pump located in the basement along with the pressure tank over time through general use will begin to decline and this will be noted in reduced water pressure in flushing the toilet or for the shower, kitchen sink, etc. (Photo Source: TRCA, 2018)

Most rainwater cisterns are placed in basements or outdoors, and require a pump to distribute the water to service its designated locations throughout the property, generally located at higher elevations. Typically, a pump is arranged with a pressure tank, which includes a centrifugal pump that draws the water out of the storage tank and into the pressure tank, where it is stored and ready for distribution. As part of this distribution system, an appropriately sized pump is required to produce a sufficient flow to efficiently transport water that feeds into the pressure tank. With prolonged usage, the pump capacity may decline, which would be reflected by a reduction in flow rate.

Flow Rate testing

A simple flow rate measurement using a bucket, stopwatch and volume measurement device (e.g., graduated cylinder) at the outlet location can reveal whether the pump is functioning. Once the flow rate is measured the value can be compared to the design flow rate. If the pump is not creating sufficient pressure, then the flow rate will be inadequate. If the flow rate is below the design specification, servicing of the pump by a skilled technician should be scheduled.

Water Quality Testing

In addition to confirming that the pump is functioning and checking on the flow rate, routinely conducting cistern pump tests also provides the opportunity to visually inspect the water produced by the system. If the water delivered from the cistern is discoloured or highly turbid (i.e., murky), it indicates that the pretreatment device or filtration system is malfunctioning or needs maintenance.

Embedded Reference Guide

To gain further insight into various testing requirements/methods, acceptance requirements, associated tools, equipment and components from STEP on the inspection and maintenance of different BMP LID practices, please see our complete guide here or embedded below:

Sustainable Technologies Evaluation Program

Low Impact Development. A stormwater management strategy that seeks to mitigate the impacts of increased urban runoff and stormwater pollution by managing it as close to its source as possible. It comprises a set of site design approaches and small scale stormwater management practices that promote the use of natural systems for infiltration and evapotranspiration, and rainwater harvesting.

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.

Watercourses and Lake Ontario, to which Stormwater and Combined Sewer Overflows discharge.

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.

A shallow excavated surface depression containing prepared filter media, mulch, and planted with selected vegetation.

A shallow constructed channel, often grass-lined, which is used as an alternative to curb and channel, or as a pretreatment to other measures. Swales are generally characterized by a broad top width to depth ratio and gentle grades.

The practice of adding organic material, such as mulch or compost to topsoil to improve fertility, and tilling of the native soils to reverse compaction and restore its water retaining capacity.

Refers to the conditions in which an organism lives and survives or the conditions in which an organism resides. These conditions can be described as aspects of a “physical”, “social” or an “economic” environment, depending on the perspective perceived by the observer.

FIT work involves the application of a similar set of inspection and testing indicators as those used in Performance Verification inspections, but focuses on diagnosing suspected problems with the following objectives in mind: (1) Confirm whether or not problems with BMP function exist; (2) Identify the causes of confirmed problems; (3) Determine corrective actions needed.

Mineral particles which are smaller than 2 mm, and which are free of appreciable quantities of clay and silt. Coarse sand usually designates sand grains with particle size between 0.2 and 0.02 mm.

Mineral particles which are smaller than 2 mm, and which are free of appreciable quantities of clay and silt. Coarse sand usually designates sand grains with particle size between 0.2 and 0.02 mm.

Soil or media particles smaller than sand and larger than clay (3 to 60 m)

1. A mineral soil separate consisting of particles less than 0.002 millimeter in equivalent diameter. 2. A soil texture class. 3. (Engineering) A fine-grained soil (more than 50 percent passing the No. 200 Sieve) that has a high plasticity index in relation to the liquid limit. (Unified Soil Classification System).

Soil or media particles smaller than sand and larger than clay (3 to 60 m)

1. A mineral soil separate consisting of particles less than 0.002 millimeter in equivalent diameter. 2. A soil texture class. 3. (Engineering) A fine-grained soil (more than 50 percent passing the No. 200 Sieve) that has a high plasticity index in relation to the liquid limit. (Unified Soil Classification System).

The porosity (n) of a mixture is the ratio of the volume of void-space to the total or bulk volume of the mixture. It is closely related to the concept of void ratio (e) where void ratio is the ratio of the volume of void-space to the volume of solids. n = Volume of voids/Total volume of mixture = e/(1+e)

A thin layer of vegetation and growing medium installed on top of a conventional flat or sloped roof, also referred to as living roofs or rooftop gardens.

Soil, sand and minerals washed from land into water, usually after rain. They pile up in reservoirs, rivers and harbors, destroying fish-nesting areas and holes of water animals and cloud the water so that needed sunlight might not reach aquatic plans. Careless farming, mining and building activities will expose sediment materials, allowing them to be washed off the land after rainfalls.

Soil, sand and minerals washed from land into water, usually after rain. They pile up in reservoirs, rivers and harbors, destroying fish-nesting areas and holes of water animals and cloud the water so that needed sunlight might not reach aquatic plans. Careless farming, mining and building activities will expose sediment materials, allowing them to be washed off the land after rainfalls.

The portion of water precipitated onto a catchment area, which then flows as surface discharge from the catchment area past a specified point.

Water from rain, snow melt, or irrigation that flows over the land surface.

Box like underground concrete structure with openings in curb and gutter designed to collect runoff from streets and pavement.

Deposition of material of varying size, both mineral and organic away from its site of origin by the action of water, wind, gravity or ice.

Settling-out or deposition of particulate matter suspended in runoff.

Initial capturing and removal of unwanted contaminants, such as debris, sediment, leaves and pollutants, from stormwater before reaching a best management practice; Examples include, settling forebays, vegetated filter strips and gravel diaphragms.

a gently sloping, densely vegetated areas that treat runoff as sheet flow from adjacent impervious areas. They function by slowing runoff velocity and filtering out suspended sediment and associated pollutants, and by providing some infiltration into underlying soils.

a top dressing over vegetation beds that provides suppresses weeds and helps retain soil moisture in bioretention cells, stormwater planters and dry swales.

Tank used to store rainwater (typically roof runoff) for later use.

Tank used to store rainwater (typically roof runoff) for later use.

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

A body of water smaller than a lake, often artificially formed.

An alternative practice to traditional impervious pavement, prevents the generation of runoff by allowing precipitation falling on the surface to infiltrate through the surface course into an underlying stone reservoir and, where suitable conditions exist, into the native soil.

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

A mixture of mineral aggregates bound with bituminous materials, used in the construction and maintenance of paved surfaces.

Toronto and Region Conservation Authority

FIT work involves the application of a similar set of inspection and testing indicators as those used in Performance Verification inspections, but focuses on diagnosing suspected problems with the following objectives in mind: (1) Confirm whether or not problems with BMP function exist; (2) Identify the causes of confirmed problems; (3) Determine corrective actions needed.

The porosity (n) of a mixture is the ratio of the volume of void-space to the total or bulk volume of the mixture. It is closely related to the concept of void ratio (e) where void ratio is the ratio of the volume of void-space to the volume of solids. n = Volume of voids/Total volume of mixture = e/(1+e)

Decayed organic material used as a plant fertilizer. Compost helps to support healthy plant growth through the slow release of nutrients and the retention of moisture in the soil.

An underlying bed filled with aggregate or other void-forming fill material that temporarily stores stormwater before infiltrating into the native soil or being conveyed by an underdrain pipe.

Ground depression acting as a flow control and water treatment structure, that is normally dry.

Ground depression acting as a flow control and water treatment structure, that is normally dry.

The period between the maximum water level and the minimum level (dry weather or antecedent level).

The total surface area upstream of a point on a stream that drains toward that point. Not to be confused with watershed. The drainage area may include one or more watersheds.

The total amount of particulate matter that is suspended in the water column.

Total suspended solids

Human application of water to agricultural or recreational land for watering purposes. City of Toronto Wet Weather Flow Management November 2006 47

Human application of water to agricultural or recreational land for watering purposes. City of Toronto Wet Weather Flow Management November 2006 47

Abiotic transfer of water vapour to the atmosphere.

Tank used to store rainwater (typically roof runoff) for later use.

The practice of intercepting, conveying and storing rainwater for future use. Captured rainwater is typically used for outdoor non-potable water uses such as irrigation, or in the building to flush toilets.

The technique of removing pollutants from runoff as it infiltrates through the soil.

Credit Valley Conservation

Low impact development is a stormwater management and land development strategy applied at the parcel and subdivision scale that emphasizes conservation and use of on-site natural features integrated with engineered, small scale hydrologic controls to more closely mimic pre-development hydrologic functions.

A stormwater management strategy that seeks to mitigate the impacts of increased urban runoff and stormwater pollution by managing it as close to its source as possible. It comprises a set of site design approaches and small scale stormwater management practices that promote the use of natural systems for infiltration and evapotranspiration, and rainwater harvesting.

A stormwater management strategy that seeks to mitigate the impacts of increased urban runoff and stormwater pollution by managing it as close to its source as possible. It comprises a set of site design approaches and small scale stormwater management practices that promote the use of natural systems for infiltration and evapotranspiration, and rainwater harvesting.

The total mass of a pollutant entering a waterbody over a defined time period.

Refers to the conditions in which an organism lives and survives or the conditions in which an organism resides. These conditions can be described as aspects of a “physical”, “social” or an “economic” environment, depending on the perspective perceived by the observer.

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.