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Wednesday, 1 March 2017

Urban Sediment Transport through an Established Vegetated Swale: Long Term Treatment Efficiencies and Deposition


Open AccessArticle
Water 20157(3), 1046-1067; doi:10.3390/w7031046

Urban Sediment Transport through an Established Vegetated Swale: Long Term Treatment Efficiencies and Deposition


1
Institute of Infrastructure and Environment, Heriot-Watt University, Edinburgh EH144AS, UK
2
Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride G750QF, UK
*
Author to whom correspondence should be addressed. 
Academic Editor: Miklas Scholz
Received: 31 October 2014 / Revised: 2 March 2015 / Accepted: 4 March 2015 / Published: 12 March 2015
(This article belongs to the Special Issue Sustainable Drainage Systems)
View Full-Text   |     Download PDF [1232 KB, uploaded 9 June 2015]   |      

Abstract 

Vegetated swales are an accepted and commonly implemented sustainable urban drainage system in the built urban environment. Laboratory and field research has defined the effectiveness of a vegetated swale in sediment detention during a single rainfall-runoff event. Event mean concentrations of suspended and bed load sediment have been calculated using current best analytical practice, providing single runoff event specific sediment conveyance volumes through the swale. However, mass and volume of sediment build up within a swale over time is not yet well defined. This paper presents an effective field sediment tracing methodology and analysis that determines the quantity of sediment deposited within a swale during initial and successive runoff events. The use of the first order decay rate constant, k, as an effective pollutant treatment parameter is considered in detail. Through monitoring tagged sediment deposition within the swale, the quantity of sediment that is re-suspended, conveyed, re-deposited or transported out of the swale as a result of multiple runoff events is illustrated. Sediment is found to continue moving through the vegetated swale after initial deposition, with ongoing discharge resulting from resuspension and conveyance during subsequent runoff events. The majority of sediment initially deposited within a swale is not detained long term or throughout its design life of the swale. View Full-Text
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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).

For further details log on website :
http://www.mdpi.com/2073-4441/7/3/1046

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