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basin_efficiency [2022/05/12 16:15] adminbasin_efficiency [2022/05/24 15:07] (current) admin
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 If the basin is located in the watershed of a cold-water stream, the design must provide [[thermal mitigation]].   Possible ways to prevent stream warming from the basin include eliminating permanent pool storage, providing extended draw down by use of tile drainage, or installing stone cribs at the outlet.    If the basin is located in the watershed of a cold-water stream, the design must provide [[thermal mitigation]].   Possible ways to prevent stream warming from the basin include eliminating permanent pool storage, providing extended draw down by use of tile drainage, or installing stone cribs at the outlet.   
  
-Basins must have the volume of storage necessary to settle the particle size necessary to meet either the soil loss standard during the construction phase or the TSS reduction standard for post-development. Stormwater models (HydroCAD and WinSLAMM) are now frequently used to determine peak rates, infiltration and sediment reductions, but the process described below can help to determine the approximate size of a stormwater facility to meet the peak rate standard.+Basins must have the volume of storage necessary to settle the particle size necessary to meet either the soil loss standard during the construction phase or the TSS reduction standard for post-development. Stormwater models (HydroCAD and WinSLAMM) are now frequently used to determine peak rates, infiltration and sediment reductions, but the process described below can help to determine the approximate size of a stormwater facility.
  
 :!: Please note that MSE4 rainfall distributions must be used to model peak flow rates in Dane County. :!: Please note that MSE4 rainfall distributions must be used to model peak flow rates in Dane County.
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   - The volume of storage necessary can now be calculated by multiplying the ratio from the table by the post-development runoff.   - The volume of storage necessary can now be calculated by multiplying the ratio from the table by the post-development runoff.
  
-====Approximate detention basin routing for rainfall types I, IA, II, and III====+**Approximate detention basin routing for rainfall types I, IA, II, and III**
  
-[[File:/Images/Storage Volume.PNG]]+[{{ :wiki:images:storage_volume.png?600 |Source: [[https://www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb1044171.pdf|Technical Release 55. United States Department of Agriculture, Natural Resources Conservation Service. Washington, D.C. 1988.]])}}]
  
-Source: [[https://www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb1044171.pdf|Technical Release 55. United States Department of Agriculture, Natural Resources Conservation Service. Washington, D.C. 1988.]]) +=====Calculating Trapping Efficiency=====
- +
-==Calculating Trapping Efficiency==+
 The sediment reduction is selected from the particle size versus expected efficiency for a Plano silt loam during construction.  The expected efficiency is given by the USLE in the column named “Percent reduction required to meet Ordinance.”  With this expected efficiency, use the chart below to obtain the particle size required to be retained in the pond.  The particle size has a settling velocity that may be calculated using Stokes Law. The sediment reduction is selected from the particle size versus expected efficiency for a Plano silt loam during construction.  The expected efficiency is given by the USLE in the column named “Percent reduction required to meet Ordinance.”  With this expected efficiency, use the chart below to obtain the particle size required to be retained in the pond.  The particle size has a settling velocity that may be calculated using Stokes Law.
  
-====Expected trapping efficiency of a Plano silt loam====+**Expected trapping efficiency of a Plano silt loam**
  
-[[File:/Images/Trapping_Efficiency.PNG]]+{{ :wiki:images:trapping_efficiency.png?600 |}}
  
 Convert the storage volume from the 1-year, 24-hour storm event into cubic feet.  This volume of storage is then divided by the time required to settle the particle obtained by Stokes Law. Convert the storage volume from the 1-year, 24-hour storm event into cubic feet.  This volume of storage is then divided by the time required to settle the particle obtained by Stokes Law.
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 Q<sub>maximum</sub> is the rate at which the basin must be released in order to obtain the expected efficiency. The time required to trap the necessary particle can be found on the table below. Q<sub>maximum</sub> is the rate at which the basin must be released in order to obtain the expected efficiency. The time required to trap the necessary particle can be found on the table below.
  
-===Settling velocities for spherical particles based on Stokes Law=== +**Settling velocities for spherical particles based on Stokes Law**
- +
-[[File:/Images/Stokes_Law.PNG]]+
  
-=====Note: Assumes specific gravity of 2.65 for soil particles and 20 degrees C water temperature.=====+[{{ :wiki:images:stokes_law.png?600 |Note: Assumes specific gravity of 2.65 for soil particles and 20 degrees C water temperature.}}]
  
  
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