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[[File:BMP terminology 2.png|300px|thumb|alt=image showing BMP terms|<font size=3>Schematic illustrating some of the terms and dimensions used in the Stormwater Manual.</font size>]] | [[File:BMP terminology 2.png|300px|thumb|alt=image showing BMP terms|<font size=3>Schematic illustrating some of the terms and dimensions used in the Stormwater Manual.</font size>]] | ||
− | *Bottom surface area (A<sub>B</sub>): This is the surface area at the bottom of the engineered media in a BMP. It represents the area where the engineered media changes to native soils. Units are typically in square feet. | + | *Bottom surface area (A<sub>B</sub>): This is the surface area at the bottom of the engineered media in a BMP. It represents the area where the engineered media changes to native soils. Units are typically in square feet. Engineered media is used in nearly all structural BMPs and includes media designed for vegetation (e.g. [http://stormwater.pca.state.mn.us/index.php/Design_criteria_for_bioretention#Materials_specifications_-_filter_media bioretention, [http://stormwater.pca.state.mn.us/index.php/Design_guidelines_for_soil_characteristics_-_tree_trenches_and_tree_boxes#Soil_quality_guidelines tree trenches/tree boxes], [green roofs]) |
*Canopy projection (CP): The tree canopy diameter at maturity. CP varies with species. | *Canopy projection (CP): The tree canopy diameter at maturity. CP varies with species. | ||
*Channel length (L<sub>C</sub>): This is the length of the swale channel from the furthest upstream point to the furthest downstream point. Units are typically in feet. | *Channel length (L<sub>C</sub>): This is the length of the swale channel from the furthest upstream point to the furthest downstream point. Units are typically in feet. | ||
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*Total media depth (D<sub>M</sub>): This is the depth of the engineered media between the media surface and the native soils. Units are typically in feet. | *Total media depth (D<sub>M</sub>): This is the depth of the engineered media between the media surface and the native soils. Units are typically in feet. | ||
*Volume reduction below underdrain (V<sub>U</sub>): The volume of water that can be instantaneously stored in the media beneath an underdrain and above the native soil and that will infiltrate into the underlying soil. This volume is equal to the volume of the media below the underdrain and above the native soil times the difference between porosity and field capacity. | *Volume reduction below underdrain (V<sub>U</sub>): The volume of water that can be instantaneously stored in the media beneath an underdrain and above the native soil and that will infiltrate into the underlying soil. This volume is equal to the volume of the media below the underdrain and above the native soil times the difference between porosity and field capacity. | ||
− | *Volume reduction from ET (V<sub>ET</sub>): Evapotranspiration (ET) of the portion of the water stored in the media between field capacity and wilting point. The volume of water lost through evapotranspiration ( | + | *Volume reduction from ET (V<sub>ET</sub>): Evapotranspiration (ET) of the portion of the water stored in the media between field capacity and wilting point. The volume of water lost through evapotranspiration (V<sub>ET</sub>) is assumed to be the smaller of two calculated values, potential ET and measured ET. Units are typically in cubic feet. |
*Volume reduction from basin bottom (V<sub>inf<sub>b</sub></sub>): Water that infiltrates through the bottom soils rather than pass through the underdrain. Units are typically in cubic feet. | *Volume reduction from basin bottom (V<sub>inf<sub>b</sub></sub>): Water that infiltrates through the bottom soils rather than pass through the underdrain. Units are typically in cubic feet. | ||
− | *Volume reduction from basin sides (V<sub>inf<sub>s</sub></sub>): Under saturated conditions within the filter media, water that infiltrates through any existing sloped sidewalls of the basin as the stormwater draws down through the underdrain. Stormwater lost from a sloped sidewall (Vinfs) is considered to infiltrate vertically into the surrounding soil. Units are typically in | + | *Volume reduction from basin sides (V<sub>inf<sub>s</sub></sub>): Under saturated conditions within the filter media, water that infiltrates through any existing sloped sidewalls of the basin as the stormwater draws down through the underdrain. Stormwater lost from a sloped sidewall (Vinfs) is considered to infiltrate vertically into the surrounding soil. Units are typically in cubic feet. |
*Volume capacity of a bioretention base (V<sub>BB</sub>): a layer of engineered soils above the native soils in a swale, capable of storing water and allowing it to infiltrate into the underlying native soils | *Volume capacity of a bioretention base (V<sub>BB</sub>): a layer of engineered soils above the native soils in a swale, capable of storing water and allowing it to infiltrate into the underlying native soils | ||
− | *Volume reduction capacity achieved through infiltration along the swale main channel ( | + | *Volume reduction capacity achieved through infiltration along the swale main channel (V<sub>MC</sub>): |
*Volume reduction capacity of a BMP (V): The total volume reduced by a BMP. Encompasses infiltration, ET, and interception, depending on the BMP. Units are typically in cubic feet. | *Volume reduction capacity of a BMP (V): The total volume reduced by a BMP. Encompasses infiltration, ET, and interception, depending on the BMP. Units are typically in cubic feet. | ||
*Volume reduction from interception (V<sub>I</sub>): The volume of water intercepted by a tree canopy. Intercepted water may evaporate or be slowly released such that it does not contribute to stormwater runoff. Units are typically in cubic feet. | *Volume reduction from interception (V<sub>I</sub>): The volume of water intercepted by a tree canopy. Intercepted water may evaporate or be slowly released such that it does not contribute to stormwater runoff. Units are typically in cubic feet. |