2011
DOI: 10.1061/(asce)he.1943-5584.0000315
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Bioretention Outflow: Does It Mimic Nonurban Watershed Shallow Interflow?

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Cited by 64 publications
(22 citation statements)
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“…A study was conducted that compared underdrain flow from four bioretention cells in North Carolina within comparably sized, undeveloped watersheds draining to small streams, normalized by drainage area. The results indicated no statistical difference between flow rates from the undeveloped watersheds and bioretention outflow rates for the two days following the commencement of flow [45]. This study confirmed that bioretention outflow can mimic non-urban, shallow interflow to streams, and thus help restore the natural hydroperiod.…”
Section: Hydrologic Restorationsupporting
confidence: 57%
“…A study was conducted that compared underdrain flow from four bioretention cells in North Carolina within comparably sized, undeveloped watersheds draining to small streams, normalized by drainage area. The results indicated no statistical difference between flow rates from the undeveloped watersheds and bioretention outflow rates for the two days following the commencement of flow [45]. This study confirmed that bioretention outflow can mimic non-urban, shallow interflow to streams, and thus help restore the natural hydroperiod.…”
Section: Hydrologic Restorationsupporting
confidence: 57%
“…Lined systems with appropriate filter media may provide a high degree of detention and very slow release (if sized appropriately), matched for example to the pre-development interflow or baseflow rate for their contributing catchment area (DeBusk, Hunt, & Line, 2011;Hunt et al, 2006). Unlined and undrained biofiltration systems constructed to maximize exfiltration have the additional advantage of increasing soil moisture in surrounding areas (dependent on constraints imposed by nearby infrastructure), thus improving the urban landscape and microclimate (Gomez, Jabaloyes, & Vano, 2004).…”
Section: Potential Tools For Flow-regime Managementmentioning
confidence: 98%
“…The discharge magnitudes were, however, at or below the threshold-flow criterion during these periods. DeBusk et al (2011) showed that the outflow rates from a bioretention mimicked the shallow interflow to a stream (draining an undeveloped watershed) after a storm event, thereby suggesting that the low outflow rates from a SCM need not be considered as runoff. In addition, a longer cumulative duration of discharge is required to release the excess volume generated due to the increased postdevelopment total runoff volume (Booth and Jackson 1997).…”
Section: Comparison To Reference Flow Durationsmentioning
confidence: 96%