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A nitrate sink in estuaries? An assessment by means of stable nitrate isotopes in the Elbe estuary

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Daehnke, K., Bahlmann, E., & Emeis, K. (2008). A nitrate sink in estuaries? An assessment by means of stable nitrate isotopes in the Elbe estuary. Limnology and Oceanography, 53(4), 1504-1511. doi:10.4319/lo.2008.53.4.1504.


Cite as: http://hdl.handle.net/11858/00-001M-0000-0017-CAF0-F
Abstract
To elucidate the fate of river-borne nitrate in the estuarine environment, we measured nitrate concentrations and delta N-15 and delta O-18 of nitrate along the salinity gradient in the estuary of the river Elbe, one of the largest German rivers discharging into the North Sea. Nitrate concentrations in river waters ranged from 78 mu mol L-1 to 232 mu mol L-1; delta N-15 varied from 8.2% to 16.2%, and the delta O-18 values ranged from 20.1% to 3.2%. The nitrate concentrations in the German Bight were between 2 mu mol L-1 and 34 mu mol L-1, with delta N-15 between 8.0% and 12.2% and delta O-18 between 0.3% and 9.5%. Both riverine and marine end-member concentrations showed seasonal variations, with lower nitrate concentrations and more enriched isotope values during spring and summer compared to winter months. We found no indication in either concentrations or isotopic composition for a significant loss of nitrate within the estuary, but we found a significant increase of nitrate in the maximum turbidity zone in summer. We attribute this to nitrification reflected in a change in the oxygen isotopic composition. The entire riverine nitrate load is entrained into the North Sea by conservative mixing; this conflicts with both the presumed role of estuaries as effective N-sinks and with historical data from the Elbe estuary. Fundamental changes in the biogeochemical processes of the estuary have occurred over the past several decades due to extensive dredging and removal of sediment favorable for denitrification in the Elbe estuary that connects the port of Hamburg with the North Sea.