2018
DOI: 10.1016/j.jenvman.2018.07.040
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Hydrologic and water quality performance of permeable pavement with internal water storage over a clay soil in Durham, North Carolina

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Cited by 75 publications
(54 citation statements)
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“…Water in the scarified soil took approximately 16 days to exfiltrate completely; given the average dry period was 4.7 days, the scarified soil completely drained only once during the monitoring period. This meant that there was ample time for anaerobic conditions to form in the scarified soil during inter-event periods; Braswell et al (2018) found these conditions develop within 36 hours of the cessation of rainfall.…”
Section: Resultsmentioning
confidence: 99%
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“…Water in the scarified soil took approximately 16 days to exfiltrate completely; given the average dry period was 4.7 days, the scarified soil completely drained only once during the monitoring period. This meant that there was ample time for anaerobic conditions to form in the scarified soil during inter-event periods; Braswell et al (2018) found these conditions develop within 36 hours of the cessation of rainfall.…”
Section: Resultsmentioning
confidence: 99%
“…In this case, the dissolved and particulate organic matter in the stormwater apparently provided enough carbon for denitrifying bacteria to thrive, since little organic matter is expected in the soil underlying the permeable pavement (B horizon). Denitrification has been observed in a permeable pavement employing IWS (Braswell et al 2018); this occurred in the 72 hours following a storm event, during which the dissolved oxygen present in stormwater declined due to aerobic bacterial respiration. It is theorized that similar processes are occurring in the permeable pavement studied herein, suggesting that an additional carbon source beyond that found in stormwater is not needed for denitrification to occur in the scarified soil beneath permeable pavements.…”
Section: Resultsmentioning
confidence: 99%
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“…Palmer et al [19] found that the removal rate of NO3 --N increased from 33% in the bioretention systems without SZ to 71% in those with SZ. Manka et al [20] found that the activity of denitrifying microorganisms increased in the field-scale bioretention systems with SZ, which consequently contributed to the more complete removal of NO3 --N. By monitoring NO3 --N concentration in SZ of bioretention systems every 24 hours after rainfall events, Braswell, et al [21] revealed that denitrification might mainly occur in SZ. Furthermore, the NO3 --N removal performance of a bioretention system could be affected by the depth of SZ.…”
Section: Introductionmentioning
confidence: 99%
“…On one hand, it is difficult to distinguish the effects on nitrogen removal at different periods and locations in bioretention systems. On the other hand, the effects of SZ during dry periods varied with many factors, such as influent nitrogen concentration [30], influent volume or flux [31], rainfall intensity and ADP [21], etc.…”
Section: Introductionmentioning
confidence: 99%