Nitrogen Removal in a Small Constructed Wetland: An Isotope Mass Balance Approach
The nitrogen (N) removal potential of constructed wetlands is increasingly used to lower the N load from agricultural nonpoint sources to inland and coastal waters. To determine the removal efficiency and key factors limiting wetland N removal, N fluxes were studied in a small constructed wetland in...
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Published in: | Environmental science & technology Vol. 40; no. 10; pp. 3313 - 3319 |
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Main Authors: | , , , |
Format: | Journal Article |
Language: | English |
Published: |
Washington, DC
American Chemical Society
15-05-2006
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Subjects: | |
Online Access: | Get full text |
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Summary: | The nitrogen (N) removal potential of constructed wetlands is increasingly used to lower the N load from agricultural nonpoint sources to inland and coastal waters. To determine the removal efficiency and key factors limiting wetland N removal, N fluxes were studied in a small constructed wetland in Central Switzerland. With an isotope mass balance approach integrating the natural isotope signature of nitrate (NO3 -), ammonium (NH4 +), and particulate nitrogen (PN), the N transformations such as assimilation, mineralization, nitrification, and denitrification were quantified. On average, the wetland removed 45 g m-2 yr-1 N during the studied 2.5 years, corresponding to a removal efficiency of 27%. Denitrification contributed 94% to the N removal, while only 6% of the removed N accumulated in the sediments. Denitrification was most efficient during periods with an oxic water column overlying anoxic sediments, as NH4 + released during mineralization of sediment organic matter was completely nitrified and subsequently denitrified at the sediment−water interface. During water column anoxia, NH4 + accumulated in the water and fueled assimilation by duckweed and internal recycling. The NO3−N isotope signature in the wetland mainly reflected the mineralization of sediment organic matter and subsequent nitrification, while denitrification at the sediment−water interface produced no fractionation. |
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Bibliography: | ark:/67375/TPS-SNQZS3Z6-2 istex:5DD3945FA72E862DC3B7303CE90E226E233C9403 ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 ObjectType-Article-1 ObjectType-Feature-2 |
ISSN: | 0013-936X 1520-5851 |
DOI: | 10.1021/es052393d |