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Thursday, 2 March 2017

Phosphorus Retention in Stormwater Control Structures across Streamflow in Urban and Suburban Watersheds

Water 20168(9), 390; doi:10.3390/w8090390

Author


1
Department of Geology and Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD 20742, USA
2
Systems Exposure Division, Ecosystem Integrity Branch, U.S. Environmental Protection Agency, Cincinnati, OH 45268, USA
3
Western Ecology Division, National Health and Environmental Effects Research Lab, U.S. Environmental Protection Agency, Corvallis, OR 97333, USA
*
Author to whom correspondence should be addressed. 
Academic Editor: Andreas N. Angelakis
Received: 23 May 2016 / Revised: 11 August 2016 / Accepted: 29 August 2016 / Published: 9 September 2016
(This article belongs to the Special Issue Land Use, Climate, and Water Resources)
View Full-Text   |     Download PDF [2721 KB, uploaded 9 September 2016]   |    
 

Abstract 

Recent studies have shown that stormwater control measures (SCMs) are less effective at retaining phosphorus (P) than nitrogen. We compared P retention between two urban/suburban SCMs and their adjacent free-flowing stream reaches at the Baltimore Long-Term Ecological Study (LTER) site, and examined changes in P retention in SCMs across flow conditions. Results show that, when compared with free-flowing stream reaches, the SCMs had significantly lower dissolved oxygen (%DO) and higher P concentrations, as well as lower mean areal retention rates and retention efficiencies of particulate P (PP). In all the SCMs, concentrations of total dissolved phosphorus (TDP) consistently exhibited inverse correlations with %DO that was lower during summer base flows. Particulate phosphorus (PP) concentrations peaked during spring high flow period in both streams and in-line pond/SCMs, but they were also higher during summer base flows in suburban/urban SCMs. Meanwhile, PP areal retention rates and retention efficiencies of the SCMs changed from positive (indicating retention) during high flows to negative (indicating release) during low flows, while such changes across flow were not observed in free-flowing stream reaches. We attribute the changing roles of SCMs from a PP sink to a PP source to changes in SCM hydrologic mass balances, physical sedimentation and biogeochemical mobilization across flows. This study demonstrates that in suburban/urban SCMs, P retained during high flow events can be released during low flows. Cultivation of macrophytes and/or frequent sediment dredging may provide potential solutions to retaining both P and nitrogen in urban SCMs. View Full-Text
 Figures

Figure 1
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. (CC BY 4.0).

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http://www.mdpi.com/2073-4441/8/9/390

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