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| Titel |
Nitrogen and dissolved organic carbon (DOC) losses from an artificially drained grassland on organic soils |
| VerfasserIn |
B. Tiemeyer, P. Kahle |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1726-4170
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| Digitales Dokument |
URL |
| Erschienen |
In: Biogeosciences ; 11, no. 15 ; Nr. 11, no. 15 (2014-08-06), S.4123-4137 |
| Datensatznummer |
250117538
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| Publikation (Nr.) |
 copernicus.org/bg-11-4123-2014.pdf |
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| Zusammenfassung |
| Nitrate–nitrogen (NO3–N) as well as dissolved organic carbon (DOC) and
nitrogen (DON) concentrations and losses were studied for three and
two years, respectively, in a small catchment dominated by a degraded peatland used as
intensive grassland. Concentrations in the shallow groundwater were spatially
and temporally very variable, with NO3–N being the most dynamic component
(7.3 ± 12.5 mg L−1) and ranging from 0 to 79.4 mg L−1.
Average NO3–N concentrations of 10.3 ± 5.4 mg L−1 (0 to
25.5 mg L−1) in the ditch draining the catchment and annual NO3–N
losses of 19, 35 and 26 kg ha−1 confirmed drained peatlands as an
important source of diffuse N pollution. The highest NO3–N losses
occurred during the wettest year. Resulting from concentration of
2.4 ± 0.8 mg L−1 (0.7 to 6.2 mg L−1), DON added a further
4.5 to 6.4 kg ha−1 to the N losses and thus formed a relevant
(15%) component of the total N losses. Ditch DOC concentrations of
24.9 ± 5.9 mg L−1 (13.1 to 47.7 mg L−1) resulted in DOC
losses of 66 kg ha−1 in the wet year of 2006/2007 and 39 kg ha−1
in the dry year of 2007/2008. Ditch DOC concentration were lower than the
groundwater DOC concentration of 50.6 ± 15.2 mg L−1 (14.9 to
88.5 mg L−1). Both DOC and N concentrations were governed by
hydrological conditions, but NO3–N reacted much faster and clearer on
rising discharge rates than DOC, which tended to be higher under drier
conditions. In the third year of the study, the superposition of a very wet
summer and land use changes from grassland to arable land in a part of the
catchment suggests that, under re-wetting conditions with a high groundwater
table in summer, NO3–N would diminish quickly, while DOC would remain on
a similar level. Further intensification of the land use, on the other hand,
would increase N losses to receiving water bodies. |
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