(Created page with "Designers should evaluate soil properties during preliminary site layout with the intent of installing bioretention or bioinfiltration practices on soils with the highest infi...")
 
m
 
(12 intermediate revisions by the same user not shown)
Line 1: Line 1:
Designers should evaluate soil properties during preliminary site layout with the intent of installing bioretention or bioinfiltration practices on soils with the highest infiltration rates (HSG A and B). Preliminary planning for the location of an infiltration device may be completed using a county soil survey or the [http://websoilsurvey.nrcs.usda.gov/app/HomePage.htm NRCS Web Soil Survey]. These publications provide HSG information for soils across Minnesota.  To ensure long-term performance, however, field soil measurements are desired to provide site-specific data.
+
[[File:MPD Infiltrometer image.jpg|300px|thumb|alt=image of MPD infiltrometer|<font size=3>The modified Philip-Dunne infiltrometer, as well as other direct infiltration measurements such as double ring infiltrometers, are preferred methods for measuring infiltration rates, compared to soil borings and pits. Image: [http://stormwaterbook.safl.umn.edu/water-budget-measurement/infiltration University of Minnesota, St. Anthony Falls Laboratory]</font size>.]]
  
If the initial evaluation indicates that a bioretention practice would be a good BMP for the site, it is ''RECOMMENDED'' that soil borings or pits be dug within the proposed boundary of the bioretention practice to verify soil types and infiltration capacity characteristics and to determine the depth to groundwater and bedrock.  Soil borings for building structural analysis are not acceptable. In all design scenarios, a minimum of one soil boring (two are recommended) shall be completed to a depth 5 feet below the bottom of the proposed bioretention Stormwater Control Measure (SCM or BMP) (Dakota County Soil and Water Conservation District, 2012) per ASTM D1586 ([http://www.astm.org/ ASTM], 2011).  For bioretention SCMs with surface area between 1000 and 5000 square feet, two borings shall be made.  Between 5000 and 10000 square feet, three borings are needed, and for systems with greater than 10000 square feet in surface area, 4 or more borings are needed. For each additional 2500 square feet beyond 12,500 square feet, an additional soil boring should be made.  Soil borings must be undertaken during the design phase (i.e. prior to the commencement of construction) to determine how extensive the soil testing will be during construction. Borings should be completed using continuous split spoon sampling, with blow counts being recorded to determine the level of compaction of the soil.  Soil borings are needed to understand soil types, seasonally high groundwater table elevation, depth to karst, and bedrock elevations.
+
{{alert|The [[Construction stormwater program|Construction Stormwater permit]] includes the following requirements.
 +
16.10. Permittees must provide at least one soil boring, test pit or infiltrometer test in the location of the infiltration practice for determining infiltration rates.<br>
 +
16.11. For design purposes, permittees must divide field measured infiltration rates by 2 as a safety factor or permittees can use soil-boring results with the infiltration rate chart in the Minnesota Stormwater Manual to determine design infiltration rates. When soil borings indicate type A soils, permittees should perform field measurements to verify the rate is not above 8.3 inches per hour. This permit prohibits infiltration if the field measured infiltration rate is above 8.3 inches per hour.|alert-danger}}
 +
 
 +
 
 +
Designers should evaluate soil properties during preliminary site layout with the intent of installing infiltration practices on soils with the highest <span title="The infiltration rate is the velocity or speed at which water enters into the soil"> '''infiltration rates'''</span> (<span title="A soil classification system (Natural Resource Conservation System) based on runoff potential. Groups include A soils (coarse textured with very low runoff potential), B soils (medium coarse textured with low runoff potential), C soils (fine to moderate textured with moderate runoff potential), and D soils (fine textured with high runoff potential)."> '''[https://stormwater.pca.state.mn.us/index.php?title=Design_infiltration_rates hydrologic soil group]'''</span> A and B). Preliminary planning for the location of an infiltration device may be completed using a county soil survey or the [http://websoilsurvey.nrcs.usda.gov/app/HomePage.htm NRCS Web Soil Survey].  These publications provide HSG information for soils across Minnesota.  To ensure long-term performance, however, [https://stormwater.pca.state.mn.us/index.php?title=Determining_soil_infiltration_rates field soil measurements] are desired to provide site-specific data.
 +
 
 +
If the initial evaluation indicates that an infiltration practice would be a good BMP for the site, it is ''RECOMMENDED'' that [https://stormwater.pca.state.mn.us/index.php?title=Understanding_and_interpreting_soils_and_soil_boring_reports_for_infiltration_BMPs soil borings] or pits be dug within the proposed boundary of the infiltration practice to verify soil types and infiltration capacity characteristics and to determine the depth to groundwater and bedrock.  Soil borings for building structural analysis are not acceptable. In all design scenarios, a minimum of one soil boring (two are recommended) shall be completed to a depth 5 feet below the bottom of the proposed infiltration Stormwater Control Measure (SCM or BMP) (Dakota County Soil and Water Conservation District, 2012) per ASTM D1586 ([http://www.astm.org/ ASTM], 2011).  For infiltration SCMs with surface area between 1000 and 5000 square feet, two borings shall be made.  Between 5000 and 10000 square feet, three borings are needed, and for systems with greater than 10000 square feet in surface area, 4 or more borings are needed. For each additional 2500 square feet beyond 12,500 square feet, an additional soil boring should be made.  Soil borings must be undertaken during the design phase (i.e. prior to the commencement of construction) to determine how extensive the soil testing will be during construction. Borings should be completed using continuous split spoon sampling, with blow counts being recorded to determine the level of compaction of the soil.  Soil borings are needed to understand soil types, seasonally high groundwater table elevation, depth to karst, and bedrock elevations.
  
 
{{:Recommended number of soil boring, pits, and permeameter tests for bioretention design}}
 
{{:Recommended number of soil boring, pits, and permeameter tests for bioretention design}}
 
   
 
   
It is ''HIGHLY RECOMMENDED'' that soil profile descriptions be recorded and include the following information for each soil horizon or layer (Source: [http://dnr.wi.gov/topic/stormwater/documents/dnr1002-Infiltration.pdf ''Site Evaluation for Stormwater Infiltration''], Wisconsin Department of Natural Resources Conservation Practice Standards 2004):
+
It is ''HIGHLY RECOMMENDED'' that soil profile descriptions be recorded and include the following information for each soil horizon or layer (Source: [https://dnr.wi.gov/topic/Stormwater/standards/postconst_standards.html ''Site Evaluation for Stormwater Infiltration''], Wisconsin Department of Natural Resources Conservation Practice Standards 2004):
 
*thickness, in inches or decimal feet;
 
*thickness, in inches or decimal feet;
 
*Munsell soil color notation;
 
*Munsell soil color notation;
*soil mottle or redoximorphic feature color, abundance, size and contrast;
+
*soil mottle or <span title="redoximorphic refers to the reduction and oxidation chemical reactions and the resulting appearance or morphology of the soil horizon"> [https://stormwater.pca.state.mn.us/index.php?title=Identifying_and_characterizing_redoximorphic_features_in_soils_and_soil_borings '''redoximorphic''']</span> feature color, abundance, size and contrast;
 
*USDA soil textural class with rock fragment modifiers;
 
*USDA soil textural class with rock fragment modifiers;
*soil structure, grade size and shape;
+
*<span title="Soil structure describes the arrangement of the solid parts of the soil and of the pore space located between them. It is determined by how individual soil granules clump, bind together, and aggregate, resulting in the arrangement of soil pores between them."> '''soil structure'''</span>, grade size and shape;
*soil consistence, root abundance and size;
+
*<span title="Soil consistency is the strength with which soil materials are held together or the resistance of soils to deformation and rupture"> '''soil consistence'''</span>, root abundance and size;
 
*soil boundary; and
 
*soil boundary; and
 
*occurrence of saturated soil, impermeable layers/lenses, ground water, bedrock or disturbed soil.
 
*occurrence of saturated soil, impermeable layers/lenses, ground water, bedrock or disturbed soil.
  
It is RECOMMENDED that a standard soil boring form be used.  A good example is [[File:Boring Pit Log form.docx]]. The NRCS [http://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/ref/?cid=nrcs142p2_054184 Field Book for Describing and Sampling Soils] provide detailed information for identifying soil characteristics. Munsell color charts can be found at [http://www.masterplan.southsuburbanairport.com/Environmental/pdf2/Part%204%20-%20References/Reference%2016%20Munsell%20Color%20Charts/MunsellColorChart.pdf].
+
It is RECOMMENDED that a standard soil boring form be used.  A good example is [[File:Boring Pit Log form.docx]]. The NRCS [https://www.nrcs.usda.gov/resources/guides-and-instructions/field-book-for-describing-and-sampling-soils Field Book for Describing and Sampling Soils] provide detailed information for identifying soil characteristics. Munsell color charts can be found [https://munsell.com/color-products/color-communications-products/environmental-color-communication/munsell-soil-color-charts/ here].
{{alert|A separation distance of 3 feet is REQUIRED between the bottom of the bioretention practice and the elevation of the seasonally high water table ([[Glossary#S|saturated soil]]) or top of bedrock (i.e. there must be a minimum of 3 feet of undisturbed soil beneath the infiltration practice and the seasonally high water table or top of bedrock).|alert-danger}}
+
{{alert|A separation distance of 3 feet is REQUIRED between the bottom of the infiltration practice and the elevation of the seasonally high water table (saturated soil) or top of bedrock (i.e. there must be a minimum of 3 feet of undisturbed soil beneath the infiltration practice and the seasonally high water table or top of bedrock).|alert-danger}}
 
It is HIGHLY RECOMMENDED that the field verification be conducted by a qualified geotechnical professional.
 
It is HIGHLY RECOMMENDED that the field verification be conducted by a qualified geotechnical professional.
 +
 +
[[Category:Level 3 - Best management practices/Structural practices/Infiltration (trench/basin)]]
 +
[[Category:Level 3 - Best management practices/Specifications and details/Design criteria]]

Latest revision as of 19:18, 27 December 2022

image of MPD infiltrometer
The modified Philip-Dunne infiltrometer, as well as other direct infiltration measurements such as double ring infiltrometers, are preferred methods for measuring infiltration rates, compared to soil borings and pits. Image: University of Minnesota, St. Anthony Falls Laboratory.
Warning: The Construction Stormwater permit includes the following requirements.

16.10. Permittees must provide at least one soil boring, test pit or infiltrometer test in the location of the infiltration practice for determining infiltration rates.

16.11. For design purposes, permittees must divide field measured infiltration rates by 2 as a safety factor or permittees can use soil-boring results with the infiltration rate chart in the Minnesota Stormwater Manual to determine design infiltration rates. When soil borings indicate type A soils, permittees should perform field measurements to verify the rate is not above 8.3 inches per hour. This permit prohibits infiltration if the field measured infiltration rate is above 8.3 inches per hour.


Designers should evaluate soil properties during preliminary site layout with the intent of installing infiltration practices on soils with the highest infiltration rates ( hydrologic soil group A and B). Preliminary planning for the location of an infiltration device may be completed using a county soil survey or the NRCS Web Soil Survey. These publications provide HSG information for soils across Minnesota. To ensure long-term performance, however, field soil measurements are desired to provide site-specific data.

If the initial evaluation indicates that an infiltration practice would be a good BMP for the site, it is RECOMMENDED that soil borings or pits be dug within the proposed boundary of the infiltration practice to verify soil types and infiltration capacity characteristics and to determine the depth to groundwater and bedrock. Soil borings for building structural analysis are not acceptable. In all design scenarios, a minimum of one soil boring (two are recommended) shall be completed to a depth 5 feet below the bottom of the proposed infiltration Stormwater Control Measure (SCM or BMP) (Dakota County Soil and Water Conservation District, 2012) per ASTM D1586 (ASTM, 2011). For infiltration SCMs with surface area between 1000 and 5000 square feet, two borings shall be made. Between 5000 and 10000 square feet, three borings are needed, and for systems with greater than 10000 square feet in surface area, 4 or more borings are needed. For each additional 2500 square feet beyond 12,500 square feet, an additional soil boring should be made. Soil borings must be undertaken during the design phase (i.e. prior to the commencement of construction) to determine how extensive the soil testing will be during construction. Borings should be completed using continuous split spoon sampling, with blow counts being recorded to determine the level of compaction of the soil. Soil borings are needed to understand soil types, seasonally high groundwater table elevation, depth to karst, and bedrock elevations.

Recommended number of soil borings, pits or permeameter tests for bioretention design. Designers select one of these methods.
Link to this table

Surface area of stormwater control measure (BMP)(ft2) Borings Pits Permeameter tests
< 1000 1 1 5
1000 to 5000 2 2 10
5000 to 10000 3 3 15
>10000 41 41 202

1an additional soil boring or pit should be completed for each additional 2,500 ft2 above 12,500 ft2
2an additional five permeameter tests should be completed for each additional 5,000 ft2 above 15,000 ft2


It is HIGHLY RECOMMENDED that soil profile descriptions be recorded and include the following information for each soil horizon or layer (Source: Site Evaluation for Stormwater Infiltration, Wisconsin Department of Natural Resources Conservation Practice Standards 2004):

  • thickness, in inches or decimal feet;
  • Munsell soil color notation;
  • soil mottle or redoximorphic feature color, abundance, size and contrast;
  • USDA soil textural class with rock fragment modifiers;
  • soil structure, grade size and shape;
  • soil consistence, root abundance and size;
  • soil boundary; and
  • occurrence of saturated soil, impermeable layers/lenses, ground water, bedrock or disturbed soil.

It is RECOMMENDED that a standard soil boring form be used. A good example is File:Boring Pit Log form.docx. The NRCS Field Book for Describing and Sampling Soils provide detailed information for identifying soil characteristics. Munsell color charts can be found here.

Warning: A separation distance of 3 feet is REQUIRED between the bottom of the infiltration practice and the elevation of the seasonally high water table (saturated soil) or top of bedrock (i.e. there must be a minimum of 3 feet of undisturbed soil beneath the infiltration practice and the seasonally high water table or top of bedrock).

It is HIGHLY RECOMMENDED that the field verification be conducted by a qualified geotechnical professional.

This page was last edited on 27 December 2022, at 19:18.