Difference between revisions of "Bioretention: Internal water storage"
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− | <p>An internal water storage zone | + | <p>An internal water storage zone/reservoir (IWS or IWSZ) is created by including an upturned 90 deg on the outflow pipe to force an elevated outlet. For practical reasons, this is commonly applied within a manhole or other nearby piece of infrastructure, rather than being buried directly adjacent. The effect is to create longer term, water-logged, low-oxygen environment within the bottom of the bioretention cell. <br> |
This has two primary benefits: | This has two primary benefits: | ||
<ol> | <ol> |
Revision as of 19:15, 17 June 2022
An internal water storage zone/reservoir (IWS or IWSZ) is created by including an upturned 90 deg on the outflow pipe to force an elevated outlet. For practical reasons, this is commonly applied within a manhole or other nearby piece of infrastructure, rather than being buried directly adjacent. The effect is to create longer term, water-logged, low-oxygen environment within the bottom of the bioretention cell.
This has two primary benefits:
- Additional infiltration is promoted by holding the water in place over the native soil for longer,
- The types of microbes that grow in a low-oxygen environment are also better at completing the removal of nitrogen compounds from the water. This effect is enhanced by using a low-nutrient carbon source in the bioretention filter media and storage reservoir aggregate.
Saturated soil conditions can kill plants in the bioretention cell, so a minimum of 30 cm vadose zone (free draining depth) must be included for healthy rooting at the top of the cell[1]. Nitrogen removal rates are linked to increased depth of IWS, so that a minimum of 45 cm of IWS is recommended where the depth of the native soils and bioretention cell permit[2]. However, any depth of IWS would be expected to make some improvement on water retention and infiltration.