Difference between revisions of "Dry ponds"

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==Design==
 
==Design==
<h3>Sizing</h3>
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===Sizing===
The surface storage volume of a dry pond (''A<sub>p</sub>'') is simply determined:
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The surface storage volume of a dry pond (''A<sub>p</sub>'') is determined:
 
   
 
   
 
<math>A_{p}=\frac{RVC_T\times A_{c}}{q\times t_{drawdown}}</math>
 
<math>A_{p}=\frac{RVC_T\times A_{c}}{q\times t_{drawdown}}</math>
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*''RVC<sub>T</sub>'' = [[Runoff volume control target]] (mm)
 
*''RVC<sub>T</sub>'' = [[Runoff volume control target]] (mm)
 
*''A<sub>c</sub>'' = Area of the catchment (m<sup>2</sup>)
 
*''A<sub>c</sub>'' = Area of the catchment (m<sup>2</sup>)
*''q'' = infiltration rate (mm/hr)
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*''f''' = design infiltration rate (mm/hr)
 
*''t'' = [[drawdown time]] (hrs)}}
 
*''t'' = [[drawdown time]] (hrs)}}
  

Revision as of 21:35, 6 March 2018

Also known as infiltration basins.

Overview[edit]

Dry ponds are recommended as flood control structures to accommodate occasional excess overflow downstream of other structural BMPs. They should be integrated into the landscape as useful, accessible public space.


Design[edit]

Sizing[edit]

The surface storage volume of a dry pond (Ap) is determined:

Where:


Modeling[edit]

Dry ponds are found in storage element in the LID TTT
The largest area is at the top, level 0 m; each subsequent lower depth has a smaller area

TTT.png

A dry pond as a storage element (key parameters) in the Treatment Train Tool.
Stage Storage
Name Important to have a unique name, to connect it with the catchment area
Storage type Dry detention ponds
Bottom elevation (m) This is important to correspond with other components,
e.g. when the overflow is coupled to another BMP within a treatment train
Maximum depth (m)
Lined/unlined Unlined (ideally)
Underlying soil Choose from five; sandy soils drain more quickly.
Evaporation factor ?
Suction head (mm) ?
Saturated conductivity (mm/hr) ?
Initial soil moisture deficit (fraction) ?
Curves
The Curves table is designed to accommodate the side slopes. The top line begins at 0 m, with subsequent depths in the following lines.

Gallery[edit]