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Biogeochemistry

, Volume 143, Issue 1, pp 67–83 | Cite as

Salinization lowers nutrient availability in formerly brackish freshwater wetlands; unexpected results from a long-term field experiment

  • Gijs van DijkEmail author
  • Leon P. M. Lamers
  • Roos Loeb
  • Piet-Jan Westendorp
  • Rick Kuiperij
  • Hein H. van Kleef
  • Marcel Klinge
  • Alfons J. P. Smolders
Article
  • 92 Downloads

Abstract

Worldwide, coastal freshwater wetlands are facing salinization at an increasing rate due to large-scale land use change, freshwater extraction, climate-driven sea level rise, droughts and land subsidence. Although it is known that increased surface water salinity does influence wetland functioning, effects on nutrient dynamics reported in literature are contradictory and evidence from controlled, long-term field experiments is scarce. We therefore tested the effects of 4 levels of increased surface water salinity, from oligohaline to mesohaline conditions (0.9, 2.25, 4.5, 9 PSU), on biogeochemical and physicochemical processes in the sediment of a formerly brackish freshwater wetland. For this, we used 16 enclosures in a controlled, 5-year field experiment. Salinization unexpectedly led to a dose dependent decreased availability of nitrogen and phosphorus in the sediment, both in the short and in the long term, even though sulfate reduction rates increased. Decreased phosphorus availability was probably caused by co-precipitation with calcium that was mobilized from sediment adsorption sites. Mobilization of ammonium from the sediment and coupled nitrification–denitrification most probably explained decreased nitrogen availability. Increasing sulfate concentrations associated with increased salinity shifted the dominant mineralization process from methanogenesis to sulfate reduction, also in the long term. We show surface water salinization to have major short-term and long-term consequences for the ecological and biogeochemical functioning of coastal freshwater wetlands.

Keywords

Phosphorus Ammonium Methanogenesis Sulfate reduction Brackish Cation exchange 

Notes

Acknowledgements

We would like to acknowledge D. Verheijen, J. Graafland, P. van der Ven, J. Eijgensteijn, M. Huitema, and S. Krosse of B-WARE Research Centre and the Radboud University for their assistance in the field and the laboratory. In addition, we would like to thank Landschap Noord-Holland for their kind permission to carry out the experiment in Ilperveld, and N. Hogeweg, F. de Vries, N. Dekker, C. Hartman, L. Vaal, B. van de Riet, J. Abma and O. Steendam, for their field assistance and for providing valuable information. A. Pol and K. Ettwig of the Department of Microbiology of Radboud University assisted with gas analyses. This research project was funded by the National Research Program ‘Knowledge Network for Restoration and Management of Nature in The Netherlands’ (OBN) of the Dutch Ministry of Economic Affairs, Agriculture and Innovation (OBN 170-LZ).

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© Springer Nature Switzerland AG 2019

Authors and Affiliations

  1. 1.B-WARE Research CentreRadboud UniversityNijmegenThe Netherlands
  2. 2.Department of Aquatic Ecology and Environmental Biology, Institute for Water and Wetland ResearchRadboud UniversityNijmegenThe Netherlands
  3. 3.Witteveen + Bos Engineering and ConsultingDeventerThe Netherlands
  4. 4.Bargerveen FoundationNijmegenThe Netherlands

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