Articles | Volume 9, issue 11
Biogeosciences, 9, 4295–4307, 2012
Biogeosciences, 9, 4295–4307, 2012

Research article 06 Nov 2012

Research article | 06 Nov 2012

Nitrate removal in a restored riparian groundwater system: functioning and importance of individual riparian zones

S. Peter1,2, R. Rechsteiner1,2, M. F. Lehmann3, R. Brankatschk1, T. Vogt1,4, S. Diem4, B. Wehrli1,2, K. Tockner5, and E. Durisch-Kaiser1,2 S. Peter et al.
  • 1Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, 8092 Zurich, Switzerland
  • 2Eawag, Swiss Federal Institute of Aquatic Science and Technology, 6047 Kastanienbaum, Switzerland
  • 3Institute for Environmental Geosciences, University of Basel, 4056 Basel, Switzerland
  • 4Eawag, Swiss Federal Institute of Aquatic Science and Technology, 8600 Dübendorf, Switzerland
  • 5IGB, Leibniz-Institute of Freshwater Ecology and Inland Fisheries, 12587 Berlin, Germany

Abstract. For the design and the assessment of river restoration projects, it is important to know to what extent the elimination of reactive nitrogen (N) can be improved in the riparian groundwater. We investigated the effectiveness of different riparian zones, characterized by a riparian vegetation succession, for nitrate (NO3) removal from infiltrating river water in a restored and a still channelized section of the river Thur, Switzerland. Functional genes of denitrification (nirS and nosZ) were relatively abundant in groundwater from willow bush and mixed forest dominated zones, where oxygen concentrations remained low compared to the main channel and other riparian zones. After flood events, a substantial decline in NO3 concentration (> 50%) was observed in the willow bush zone but not in the other riparian zones closer to the river. In addition, the characteristic enrichment of 15N and 18O in the residual NO3 pool (by up to 22‰ for δ15N and up to 12‰ for δ18O) provides qualitative evidence that the willow bush and forest zones were sites of active denitrification and, to a lesser extent, NO3 removal by plant uptake. Particularly in the willow bush zone during a period of water table elevation after a flooding event, substantial input of organic carbon into the groundwater occurred, thereby fostering post-flood denitrification activity that reduced NO3 concentration with a rate of ~21 μmol N l−1 d−1. Nitrogen removal in the forest zone was not sensitive to flood pulses, and overall NO3 removal rates were lower (~6 μmol l−1 d−1). Hence, discharge-modulated vegetation–soil–groundwater coupling was found to be a key driver for riparian NO3 removal. We estimated that, despite higher rates in the fairly constrained willow bush hot spot, total NO3 removal from the groundwater is lower than in the extended forest area. Overall, the aquifer in the restored section was more effective and removed ~20% more NO3 than the channelized section.

Final-revised paper