Line 71: | Line 71: | ||
Where | Where | ||
− | + | I<sub>R</sub> is an infiltration rate into the native soils of 0.06 inches per hour; | |
− | + | A<sub>B</sub> is the surface area at the bottom of the BMP in ft2; and | |
DDT is the drawdown time in hours. | DDT is the drawdown time in hours. | ||
The default infiltration rate is set at 0.06 inches per hour to represent a D soil. This rate was selected because it is assumed most of the stormwater will pass through the underdrain before it can infiltrate through the bottom of the BMP. This may be a conservative assumption if underdrains are small, spaced | The default infiltration rate is set at 0.06 inches per hour to represent a D soil. This rate was selected because it is assumed most of the stormwater will pass through the underdrain before it can infiltrate through the bottom of the BMP. This may be a conservative assumption if underdrains are small, spaced | ||
+ | far apart, and the underlying soil has an infiltration rate greater than 0.06 inches per hour. Conversely, more closely spaced or larger underdrains may allow the basin to drain in less than the required drawdown time, resulting in a slight overestimation of infiltration loss through the basin bottom. If the user specifies that an impermeable liner is present at the bottom of the BMP, then no credit is given for infiltration into the bottom soils. | ||
+ | |||
+ | Under saturated conditions within the filter media, water will infiltrate through the sides of the basin as the stormwater draws down through the underdrain. Stormwater lost from a sloped sidewall (Vinf_s) is considered to infiltrate vertically into the surrounding soil. The volume of water infiltrated through the sidewalls equals the following | ||
+ | |||
+ | <math>V_(In〖f_〗_S )=I_R*(DDT/2)*(A_O-A_U )/(12in/ft) </math> | ||
+ | |||
+ | Where: | ||
+ | |||
+ | A<sub>O</sub> is the surface area at overflow in ft<sup>2</sup>; and | ||
+ | A<sub>U</sub> is the surface area at the underdrain in ft<sup>2</sup> | ||
+ | |||
+ | The drawdown time is reduced by a factor of 2 to account for the drop in water level within the BMP over the drawdown period. The drop in water level is therefore considered to be linear over the drawdown time. A conservative default infiltration rate of 0.06 inches per hour is used because it is assumed that most of the stormwater will pass through the underdrain before it can infiltrate through the side walls of the BMP. If the user specifies that an impermeable liner is present on the sides of the BMP, then no credit is given for infiltration into the side soils. | ||
+ | |||
+ | The volume of water lost through evapotranspiration (VET) is the smaller of two calculated values, potential ET and measured ET. | ||
+ | |||
+ | *Potential ET (ET<sub>pot</sub>) is equal to the amount of water stored between [http://stormwater.pca.state.mn.us/index.php/Glossary#F field capacity] and the [http://stormwater.pca.state.mn.us/index.php/Glossary#W wilting point] in the media above the underdrain. ET<sub>pot</sub> is given by | ||
+ | |||
+ | <math>ET_pot=((D_M-D_U )*(A_M+A_U)/2*(FC-WP))</math> | ||
+ | |||
+ | where D<sub>M</sub> is the total media depth in feet, D<sub>U</sub> is the depth under the underdrain in feet, A<sub>M</sub> is the surface area of the media in square feet, AU is the surface area at the underdrain in square feet, and (FC – WP) is the difference between field capacity and wilting point. | ||
+ | |||
+ | *Measured ET (ET<sub>mea</sub>) is the amount of water lost to ET as measured using available data. Pan evaporation (PE) measurements collected at the University of Minnesota Southwest Experiment Station at Lamberton, Minnesota were used to estimate an average daily PE (Source: Climate of Minnesota Part XII- The Hydrologic Cycle and Soil Water, 1979). A rate of 0.2 inches per day was used, which is an intermediate value between the summertime maximum rate and the lowest rates in October. PE is converted to ET by multiplying by a correction factor of 0.5. Analysis of rainfall patterns indicates that a typical time period between precipitation events is 72 hours in Minnesota. Therefore, a volume loss from ET is calculated over a 3 day period to measure conformance to the MIDS performance goal. Therefore, the measured ET volume equals the media surface area (A<sub>M</sub>) in square feet times the daily ET rate in inches per day times 3 days. | ||
+ | |||
+ | <math>〖ET〗_mea=A_M*0.2 in/day*0.5*3 days/12 in/ft = 0.025A_M</math> | ||
+ | |||
+ | If trees are planted in the bioretention basin then ETmea is multiplied by a factor of 3. | ||
+ | |||
+ | Measured ET and potential ET are compared and the volume lost to ET is the smaller of the two values. | ||
+ | |||
+ | Elevated Underdrain: If the underdrain is elevated above the bottom of the BMP, then the volume reduction credit is determined based on the storage capacity in the media between the underdrain and the native soils, infiltration through the sides of the BMP (Vinf_s), and evapotranspiration in the planting media above the underdrain (VET). | ||
+ | |||
+ | When the underdrain is elevated, storage capacity becomes available in the media between the underdrain and the native soils. The storage capacity credit replaces the credit given for infiltration into the bottom of the BMP below the underdrain (V_(Inf_B)). The volume of water captured below the underdrain equals the following | ||
+ | |||
+ | <math>V= [(A_U+A_B)/2*(n-FC)*D_U ]</math> | ||
+ | |||
+ | Where: | ||
+ | |||
+ | A<sub>U</sub> is the surface area at the underdrain in ft2; | ||
+ | |||
+ | A<sub>B</sub> is the surface area at the bottom of the basin in ft2; | ||
+ | |||
+ | (n - FC) is the media porosity – field capacity of the soils; and | ||
+ | |||
+ | D<sub>U</sub> is the depth of the media below the underdrain in ft | ||
+ | |||
+ | The stored water must drain within the specified drawdown time. The underlying soil controls the infiltration rate. The user must input the soil with the most restrictive hydraulic conductivity in the 3 feet directly below the basin. | ||
+ | |||
+ | In addition to the credit given for the storage capacity below the underdrain, a biofiltration system with an elevated underdrain also receives volume reduction credit for infiltration into the sloped sidewall as |
For a biofiltration BMP with an underdrain at the bottom, most of the stormwater captured by the BMP is lost to the underdrain. However, some stormwater infiltrates through the basin bottom and sidewalls if these do not have an impermeable liner. Evapotranspiration also occurs from vegetation in the biofiltration BMP. For a biofiltration system with an elevated underdrain, in addition to volume losses through the sidewalls and through evapotranspiration, the water stored between the underdrain and the native soils is captured and infiltrated. In a bioretention BMP with an underdrain, all pollutants in infiltrated water are removed, while pollutants are removed through filtration for the water that flows through an underdrain.
For biofiltration systems, the user must input the following parameters to calculate the volume and pollutant load reductions associated with the BMP.
The following are requirements or recommendations for inputs into the MIDS calculator. If the following are not met, an error message will inform the user to change the input to meet the requirement.
\(DDT_calc=D_U/(I_R/ 12)\)
Where DU is the depth below the underdrain (ft); and IR is the infiltration rate of the native soils (inches/hr).
If the DDTcalc is greater than the user defined required drawdown time then the user will be prompted to enter a new depth below the underdrain or infiltration rate of the native soils.
“Required treatment volume,” or the volume of stormwater runoff delivered to the BMP, equals the performance goal (1.1 inches or user-specified performance goal) times the impervious area draining to the BMP plus any water routed to the BMP from an upstream BMP. This stormwater is delivered to the BMP instantaneously following the Kerplunk method.
The volume reduction achieved by a BMP compares the capacity of the BMP to the required treatment volume. The “Volume reduction capacity of BMP [V]” is calculated using BMP inputs provided by the user. For this BMP, the volume reduction credit methodology is determined by the location of the underdrain.
Underdrain located at BMP bottom: If the underdrain is located at the bottom of the BMP, then the “Volume reduction capacity of BMP [V]” is determined based on infiltration into the bottom of the BMP (Vinf_b), infiltration into the side slopes of the BMP (Vinf_s), and evapotranspiration in the planting media above the underdrain (VET).
Even with an underdrain present, under saturated media conditions some water will infiltrate through the bottom soils as water in the basin draws down. The volume of water lost through the bottom (Vinf_b) of the BMP equals the following
\(V_(Inf_B)=I_R*(DDT)*A_B/(12in/ft)\)
Where
IR is an infiltration rate into the native soils of 0.06 inches per hour; AB is the surface area at the bottom of the BMP in ft2; and DDT is the drawdown time in hours.
The default infiltration rate is set at 0.06 inches per hour to represent a D soil. This rate was selected because it is assumed most of the stormwater will pass through the underdrain before it can infiltrate through the bottom of the BMP. This may be a conservative assumption if underdrains are small, spaced far apart, and the underlying soil has an infiltration rate greater than 0.06 inches per hour. Conversely, more closely spaced or larger underdrains may allow the basin to drain in less than the required drawdown time, resulting in a slight overestimation of infiltration loss through the basin bottom. If the user specifies that an impermeable liner is present at the bottom of the BMP, then no credit is given for infiltration into the bottom soils.
Under saturated conditions within the filter media, water will infiltrate through the sides of the basin as the stormwater draws down through the underdrain. Stormwater lost from a sloped sidewall (Vinf_s) is considered to infiltrate vertically into the surrounding soil. The volume of water infiltrated through the sidewalls equals the following
\(V_(In〖f_〗_S )=I_R*(DDT/2)*(A_O-A_U )/(12in/ft) \)
Where:
AO is the surface area at overflow in ft2; and AU is the surface area at the underdrain in ft2
The drawdown time is reduced by a factor of 2 to account for the drop in water level within the BMP over the drawdown period. The drop in water level is therefore considered to be linear over the drawdown time. A conservative default infiltration rate of 0.06 inches per hour is used because it is assumed that most of the stormwater will pass through the underdrain before it can infiltrate through the side walls of the BMP. If the user specifies that an impermeable liner is present on the sides of the BMP, then no credit is given for infiltration into the side soils.
The volume of water lost through evapotranspiration (VET) is the smaller of two calculated values, potential ET and measured ET.
\(ET_pot=((D_M-D_U )*(A_M+A_U)/2*(FC-WP))\)
where DM is the total media depth in feet, DU is the depth under the underdrain in feet, AM is the surface area of the media in square feet, AU is the surface area at the underdrain in square feet, and (FC – WP) is the difference between field capacity and wilting point.
\(〖ET〗_mea=A_M*0.2 in/day*0.5*3 days/12 in/ft = 0.025A_M\)
If trees are planted in the bioretention basin then ETmea is multiplied by a factor of 3.
Measured ET and potential ET are compared and the volume lost to ET is the smaller of the two values.
Elevated Underdrain: If the underdrain is elevated above the bottom of the BMP, then the volume reduction credit is determined based on the storage capacity in the media between the underdrain and the native soils, infiltration through the sides of the BMP (Vinf_s), and evapotranspiration in the planting media above the underdrain (VET).
When the underdrain is elevated, storage capacity becomes available in the media between the underdrain and the native soils. The storage capacity credit replaces the credit given for infiltration into the bottom of the BMP below the underdrain (V_(Inf_B)). The volume of water captured below the underdrain equals the following
\(V= [(A_U+A_B)/2*(n-FC)*D_U ]\)
Where:
AU is the surface area at the underdrain in ft2;
AB is the surface area at the bottom of the basin in ft2;
(n - FC) is the media porosity – field capacity of the soils; and
DU is the depth of the media below the underdrain in ft
The stored water must drain within the specified drawdown time. The underlying soil controls the infiltration rate. The user must input the soil with the most restrictive hydraulic conductivity in the 3 feet directly below the basin.
In addition to the credit given for the storage capacity below the underdrain, a biofiltration system with an elevated underdrain also receives volume reduction credit for infiltration into the sloped sidewall as