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==Guidance and recommendations for conducting a higher level of engineering review== | ==Guidance and recommendations for conducting a higher level of engineering review== | ||
− | The two conditions requiring higher levels of engineering review differ. | + | ==Guidance and recommendations for conducting a higher level of engineering review== |
+ | The two conditions requiring higher levels of engineering review differ and therefore have different recommendations. | ||
− | + | {{alert|It is highly recommended that a higher level of review be provided by a licensed geoscientist or licensed engineer|alert-warning}} | |
− | * | + | 1. '''Condition 1: Moderate vulnerability overlying an ERA'''. Because there is a high degree of certainty regarding the boundaries of the ERA, the purpose of the engineering review in this case is to conduct a detailed geologic analysis or provide reasonable assurances that risk of contaminant exposure is limited. |
− | * | + | *Detailed geologic analysis: The goal of this analysis is to determine the likelihood that contaminants will be attenuated or rapidly transported in the unsaturated (vadose) zone overlying the aquifer. Soil borings are highly recommended [https://stormwater.pca.state.mn.us/index.php?title=Understanding_and_interpreting_soils_and_soil_boring_reports_for_infiltration_BMPs link here for guidance]. There is no clear line defining when sufficient protective material exists in the unsaturated zone. Modifying [https://files.dnr.state.mn.us/waters/groundwater_section/mapping/sensitivity/docs/assessing_geologic_sensitivity.pdf Minnesota Department of Natural Resources guidance], we make the following recommendations. |
− | * | + | **For non-carbonate aquifers, a minimum of 10 feet of low permeability units overlying the aquifer. The units may be aggregated (e.g. one 10-foot low permeability unit, two 5-foot low permeability units, etc.). Low permeability materials include [[Design infiltration rates|Hydrologic Soil Group]] (HSG) D soils/material, clayey tills, lake clays, and shale. |
+ | **For non-carbonate aquifers, a minimum of 20 feet of moderate permeability units overlying the aquifer. The units may be aggregated (e.g. one 20-foot moderate permeability unit, two 10-foot moderate permeability units, etc.). Moderate permeability materials include [[Design infiltration rates|HSG]] C soils/material. | ||
+ | **For carbonate aquifers, at least one continuous low permeability unit 10 feet or greater in thickness, or an aggregate of 20 feet of low permeability units. | ||
+ | |||
+ | If borings are not utilized, other sources of information may be used, but these should be used with caution. Examples include multiple well boring logs that show similar driller interpretation, or hydrogeologic assessments or studies conducted by professional organizations, such as the United States Geological Survey or Minnesota Pollution Control Agency. | ||
+ | |||
+ | An alternative approach to ensuring protection of a public water supply well is to ensure a minimum risk of contaminants exposure. This includes the following recommendations. | ||
+ | *Ensure there are no [https://stormwater.pca.state.mn.us/index.php?title=Potential_stormwater_hotspots stormwater hotspots] in the area contributing runoff to the infiltration practice. | ||
+ | *Ensure there are no existing contaminant sources within the area contributing to the infiltration practice. The [[Screening assessment for contamination at potential stormwater infiltration sites]] guidance may be used for this. | ||
+ | *Develop a spill response procedure for the area. | ||
+ | *Ensure there are land use controls in place to prevent introduction of contaminants sources into the future. | ||
+ | |||
+ | 2. '''Condition 2: High and very high vulnerability outside an ERA'''. | ||
+ | While a geologic assessment can be used in this situation, it is not necessary. If a geologic assessment is conducted, the goal would be to ensure there is sufficient protective material to retard contaminants before reaching the aquifer. The recommendations for conducting a geologic analysis described for condition 1 above can be used. | ||
+ | |||
+ | The primary concern for this condition, however, is to identify or protect other receptors, which typically will be private well owners. This can be achieved by limiting the risk of contaminant exposure, as described above for condition 1. A second option is to conduct a receptor survey. This is a two step process. | ||
+ | *Determine the one year travel time surrounding the infiltration practice. This can be estimated using simple calculators ([http://www.groundwatersoftware.com/calculator_1_average_linear_velocity.htm example]). For information on typical aquifer properties, [https://stormwater.pca.state.mn.us/index.php?title=Factors_that_affect_the_height_and_extent_of_a_groundwater_mound_beneath_a_stormwater_infiltration_system link here]. If the aquifer properties are unknown, assume a one mile radius around the infiltration practice. | ||
+ | *Determine if there are any active receptors utilizing the aquifer within the one year travel time area. | ||
+ | |||
+ | Note that these recommendations are relatively conservative and professional geoscientists or engineers may utilize other methods, including modeling. | ||
==Examples== | ==Examples== |
The Construction Stormwater Permit requires a higher level on engineering review for proposed infiltration projects in areas overlying an Emergency Response Area (ERA) where the vulnerability of the DWSMA (Drinking Water Supply Management Area) is classified as moderate, or in areas outside the ERA where the vulnerability of the DWSMA (Drinking Water Supply Management Area) is classified as high or very high. This page provide guidance and recommendations for conducting a higher level of engineering review.
The figure at the right illustrates protection designations used to manage public water supply wells that have wellhead protection plans.
A public water supply well is vulnerable if:
Five classes of vulnerability exist: very low, low, moderate, high, and very high. Within high and very high vulnerability designations, contaminants at the land surface have the potential to move quickly to the underlying aquifer.
There are two conditions in which infiltration is prohibited under the Construction Stormwater General Permit unless a higher level of engineering review is conducted and demonstrates that a functioning treatment system will prevent adverse impacts to groundwater.
It is important to understand limitations of maps depicting vulnerability. These maps are typically based on a limited number of borings that have been drilled and analyzed by geologic experts. Although in some locations there are numerous well boring logs, these logs are compiled by well drillers. Well logs therefore lack sufficient detail and expert interpretation to provide precise interpretations by geologic experts reviewing the boring logs. In addition, soils and geologic deposits can vary widely over short vertical and horizontal distances, particularly in more complex geologic settings. Consequently, classification of vulnerability represent best professional judgement.
In the first condition above, a contaminant will potentially be transported to an underlying aquifer within a moderate time frame (e.g. one year to a decade). The concern is that contaminants reaching an aquifer within the ERA can be transported to a public supply well within a short time (less than one year). It is therefore important to collect additional information about the geologic materials overlying the aquifer or ensure a minimal risk of contaminant exposure in these settings.
In the second condition, contaminants will potentially be transported quickly to an aquifer, but the public supply well is outside the ERA. Determinations of ERA are based on sound geologic analysis and modeling, but other receptors beyond the public water supply well are not considered. Thus, private wells in these settings are at risk. Engineering review in this situation entails either conducting more detailed geologic analysis or modeling or conducting a well receptor survey.
The two conditions requiring higher levels of engineering review differ and therefore have different recommendations.
1. Condition 1: Moderate vulnerability overlying an ERA. Because there is a high degree of certainty regarding the boundaries of the ERA, the purpose of the engineering review in this case is to conduct a detailed geologic analysis or provide reasonable assurances that risk of contaminant exposure is limited.
If borings are not utilized, other sources of information may be used, but these should be used with caution. Examples include multiple well boring logs that show similar driller interpretation, or hydrogeologic assessments or studies conducted by professional organizations, such as the United States Geological Survey or Minnesota Pollution Control Agency.
An alternative approach to ensuring protection of a public water supply well is to ensure a minimum risk of contaminants exposure. This includes the following recommendations.
2. Condition 2: High and very high vulnerability outside an ERA. While a geologic assessment can be used in this situation, it is not necessary. If a geologic assessment is conducted, the goal would be to ensure there is sufficient protective material to retard contaminants before reaching the aquifer. The recommendations for conducting a geologic analysis described for condition 1 above can be used.
The primary concern for this condition, however, is to identify or protect other receptors, which typically will be private well owners. This can be achieved by limiting the risk of contaminant exposure, as described above for condition 1. A second option is to conduct a receptor survey. This is a two step process.
Note that these recommendations are relatively conservative and professional geoscientists or engineers may utilize other methods, including modeling.