Dissolved and particulate reactive nitrogen in the Elbe River/NW Europe: a 2-yr N-isotope study

Rivers collect and transport reactive nitrogen to coastal seas as nitrate, ammonium, dissolved organic nitrogen (DON), or particulate nitrogen. DON is an important component of reactive nitrogen in rivers and is suspected to contribute to coastal eutrophication, but little is known about seasonality...

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Main Authors: T. Schlarbaum, K. Dähnke, K. Emeis
Format: Article
Language:English
Published: Copernicus Publications 2011-12-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/8/3519/2011/bg-8-3519-2011.pdf
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author T. Schlarbaum
K. Dähnke
K. Emeis
author_facet T. Schlarbaum
K. Dähnke
K. Emeis
author_sort T. Schlarbaum
collection DOAJ
description Rivers collect and transport reactive nitrogen to coastal seas as nitrate, ammonium, dissolved organic nitrogen (DON), or particulate nitrogen. DON is an important component of reactive nitrogen in rivers and is suspected to contribute to coastal eutrophication, but little is known about seasonality of DON loads and turnover within rivers. We measured the concentrations and the isotope ratios <sup>15</sup>N/<sup>14</sup>N of combined DON + NH<sub>4</sub><sup>+</sup> (δ<sup>15</sup>DON + NH<sub>4</sub><sup>+</sup>), nitrate (δ<sup>15</sup>N − NO<sub>3</sub><sup>−</sup>) and particulate nitrogen (δ<sup>15</sup>PN) in the non-tidal Elbe River (SE North Sea, NW Europe) over a period of 2 yr (June 2005 to December 2007) at monthly resolution. Combined DON + NH<sub>4</sub><sup>+</sup> concentrations ranged from 22 to 75 μM and comprised nearly 23% of total dissolved nitrogen in the Elbe River in annual mean; PN and nitrate concentrations ranged from 11 to 127 μM, and 33 to 422 μM, respectively. Combined PN and DON + NH<sub>4</sub><sup>+</sup> concentrations were, to a first approximation, inversely correlated to nitrate concentrations. δ<sup>15</sup>DON + NH<sub>4</sub><sup>+</sup>, which varied between from 0.8‰ to 11.5‰, changed in parallel to δ<sup>15</sup>PN (range 6 to 10‰), and both were anti-correlated to δ<sup>15</sup>N − NO<sub>3</sub><sup>−</sup> (range 6 to 23‰). Seasonal patterns of DON + NH<sub>4</sub><sup>+</sup> concentrations and δ<sup>15</sup>DON + NH<sub>4</sub><sup>+</sup> diverge from those expected from biological DON + NH<sub>4</sub><sup>+</sup> production in the river alone and suggest that the elution of organic fertilisers significantly affects the DON + NH<sub>4</sub><sup>+</sup> pool in the Elbe River.
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spelling doaj.art-7191e4d1d0a242df8685436c2957a9c42022-12-21T18:10:26ZengCopernicus PublicationsBiogeosciences1726-41701726-41892011-12-018123519353010.5194/bg-8-3519-2011Dissolved and particulate reactive nitrogen in the Elbe River/NW Europe: a 2-yr N-isotope studyT. SchlarbaumK. DähnkeK. EmeisRivers collect and transport reactive nitrogen to coastal seas as nitrate, ammonium, dissolved organic nitrogen (DON), or particulate nitrogen. DON is an important component of reactive nitrogen in rivers and is suspected to contribute to coastal eutrophication, but little is known about seasonality of DON loads and turnover within rivers. We measured the concentrations and the isotope ratios <sup>15</sup>N/<sup>14</sup>N of combined DON + NH<sub>4</sub><sup>+</sup> (δ<sup>15</sup>DON + NH<sub>4</sub><sup>+</sup>), nitrate (δ<sup>15</sup>N − NO<sub>3</sub><sup>−</sup>) and particulate nitrogen (δ<sup>15</sup>PN) in the non-tidal Elbe River (SE North Sea, NW Europe) over a period of 2 yr (June 2005 to December 2007) at monthly resolution. Combined DON + NH<sub>4</sub><sup>+</sup> concentrations ranged from 22 to 75 μM and comprised nearly 23% of total dissolved nitrogen in the Elbe River in annual mean; PN and nitrate concentrations ranged from 11 to 127 μM, and 33 to 422 μM, respectively. Combined PN and DON + NH<sub>4</sub><sup>+</sup> concentrations were, to a first approximation, inversely correlated to nitrate concentrations. δ<sup>15</sup>DON + NH<sub>4</sub><sup>+</sup>, which varied between from 0.8‰ to 11.5‰, changed in parallel to δ<sup>15</sup>PN (range 6 to 10‰), and both were anti-correlated to δ<sup>15</sup>N − NO<sub>3</sub><sup>−</sup> (range 6 to 23‰). Seasonal patterns of DON + NH<sub>4</sub><sup>+</sup> concentrations and δ<sup>15</sup>DON + NH<sub>4</sub><sup>+</sup> diverge from those expected from biological DON + NH<sub>4</sub><sup>+</sup> production in the river alone and suggest that the elution of organic fertilisers significantly affects the DON + NH<sub>4</sub><sup>+</sup> pool in the Elbe River.http://www.biogeosciences.net/8/3519/2011/bg-8-3519-2011.pdf
spellingShingle T. Schlarbaum
K. Dähnke
K. Emeis
Dissolved and particulate reactive nitrogen in the Elbe River/NW Europe: a 2-yr N-isotope study
Biogeosciences
title Dissolved and particulate reactive nitrogen in the Elbe River/NW Europe: a 2-yr N-isotope study
title_full Dissolved and particulate reactive nitrogen in the Elbe River/NW Europe: a 2-yr N-isotope study
title_fullStr Dissolved and particulate reactive nitrogen in the Elbe River/NW Europe: a 2-yr N-isotope study
title_full_unstemmed Dissolved and particulate reactive nitrogen in the Elbe River/NW Europe: a 2-yr N-isotope study
title_short Dissolved and particulate reactive nitrogen in the Elbe River/NW Europe: a 2-yr N-isotope study
title_sort dissolved and particulate reactive nitrogen in the elbe river nw europe a 2 yr n isotope study
url http://www.biogeosciences.net/8/3519/2011/bg-8-3519-2011.pdf
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AT kdahnke dissolvedandparticulatereactivenitrogenintheelberivernweuropea2yrnisotopestudy
AT kemeis dissolvedandparticulatereactivenitrogenintheelberivernweuropea2yrnisotopestudy