4.3 Article

Nutrient removal in a slow-flowing constructed wetland treating aquaculture effluent

期刊

AQUACULTURE ENVIRONMENT INTERACTIONS
卷 13, 期 -, 页码 363-376

出版社

INTER-RESEARCH
DOI: 10.3354/aei00411

关键词

Recirculating aquaculture system; Effluent treatment; Constructed wetland; Dissolved nutrients; Particulate nutrients; Removal rate constants

资金

  1. Ministry of Food, Agriculture and Fisheries of Denmark
  2. European Union through the European Maritime and Fisheries Fund (EMFF)

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The study found that particulate nutrient removal in MTF wetlands mainly occurs through sedimentation, while dissolved nutrient removal relies on biologically mediated processes. Nitrogen and phosphorus removal fluctuates seasonally, with temperature likely influencing nitrate removal. Overall, enhancing nitrate removal in slow-flowing MTF wetlands would require carbon dosing, while further improving ammonia and phosphorus removal would involve reducing their input into the wetlands.
Danish model trout farms (MTFs) use stream-like constructed wetlands for effluent polishing, and the industry is keen to improve wetland removal efficiency. To facilitate this, we examined longitudinal and seasonal nutrient removals in an MTF wetland with a hydraulic retention time (HRT) of 1.7 d, a free water surface (FWS) area of 7510 m(2), and a volume of 6008 m(3). Biweekly, 24-h composite water samples were obtained for 1 yr at 6 sampling stations along the wetland. Assuming plug flow conditions, reductions in particulate and dissolved nutrient concentrations were modelled as first-order removal processes, and removal rate constants (k(1,A), m d(-1)) were plotted to reveal seasonal fluctuations. Particulate phosphorus and organic matter k(1,A) fluctuated more or less randomly through the year, reflecting that particulate nutrient removal predominantly takes place by sedimentation. In contrast, dissolved nitrogen, phosphorus, and organic matter k(1,A) fluctuated seasonally, demonstrating that dissolved nutrient removal relies on biologically mediated processes. Temperature oscillations probably governed the observed seasonal fluctuations in nitrate-N k(1,A) and could be approximated with an Arrhenius temperature coefficient of 1.07. Furthermore, denitrification appeared to be carbon-limited. Incoming dissolved phosphorous and ammonia became incorporated in the natural wetland growth cycle that included periods of net removal and release, resulting in minimal annual net removal. In summary, this study shows that improving nitrate removal in a slow-flowing MTF wetland would require some kind of carbon dosing, while further improving ammonia and phosphorus removal would require a reduction of the amounts of ammonia and dissolved phosphorus entering the wetland.

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