Journal
ECOLOGICAL ENGINEERING
Volume 106, Issue -, Pages 597-608Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.ecoleng.2017.06.016
Keywords
Wetlands; Nitrate cycling; N-15 tracer; Denitrification; Plant uptake; Wetland restoration; Pulse-flow treatment wetland
Funding
- North Carolina Sea Grant
- Water Resources Research Institute of the University of North Carolina Research Grant
- United States Environmental Protection Agency (EPA) under the Science to Achieve Results (STAR) Graduate Fellowship Program
- National Science Foundation (NSF) [EAR 1024662]
- USGS Water Mission Area National Research Program
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Quantitative information about the fate of applied nitrate (NO3-N) in pulse-flow constructed wetlands is essential for designing wetland treatment systems and assessing their nitrogen removal services for agricultural and stormwater applications. Although many studies have documented NO3-N losses in wetlands, controlled experiments indicating the relative importance of different processes and N sinks are scarce. In the current study, (NO3)-N-15-N isotope enrichment tracer experiments were conducted in wetland mesocosms of two different wetland soil types at two realistic agricultural NO3-N source loads. The N-15 label was traced from the source NO3-N into plant biomass, soil (including organic matter and ammonium), and N-gas constituents over 7-10 day study periods. All sinks responded positively to higher NO3-N loading. Plant uptake exceeded denitrification 2-3 fold in the low NO3-N loading experiments, while both fates were nearly equivalent in the high loading experiments. One to two years later, soils largely retained the assimilated tracer N, whereas plants had lost much of it. Results demonstrated that plant and microbial assimilation in the soil (temporary N sinks) can exceed denitrification (permanent N loss) in pulse-flow environments and must be considered by wetland designers and managers for optimizing nitrogen removal potential. (C) 2017 Elsevier B.V. All rights reserved.
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