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Marine and Freshwater Research Marine and Freshwater Research Society
Advances in the aquatic sciences
RESEARCH ARTICLE

Sediment deposition and net phosphorus retention in a hydraulically restored lowland river floodplain in Denmark: combining field and laboratory experiments

Brian Kronvang A C , Carl C. Hoffmann A and Rianne Dröge A B
+ Author Affiliations
- Author Affiliations

A Department of Freshwater Ecology, National Environmental Research Institute, University of Aarhus, Vejlsøvej 25, DK 8600 Silkeborg, Denmark.

B TNO Built Environment and Geosciences, PO Box 80015, 3508 TA Utrecht, The Netherlands.

C Corresponding author. Email: bkr@dmu.dk

Marine and Freshwater Research 60(7) 638-646 https://doi.org/10.1071/MF08066
Submitted: 1 March 2008  Accepted: 28 February 2009   Published: 28 July 2009

Abstract

Restoration of river systems allowing the transformation of former drained and dry riparian areas into riparian wetlands will increase the overbank storage of sediment and sediment-associated phosphorus (P). Wetland restoration is therefore a cost-effective mitigation measure to reduce the sediment and nutrient transport to river systems. The studied floodplain of the River Odense was restored in 2003 by remeandering the river channel along a 6-km reach. The restoration project involved 78 ha of riparian areas that were transformed from mainly arable land to extensive grassland and wetlands. The aim of the study was to quantify and model sediment and particulate P deposition on restored river floodplains. The present study suggests that during a 47-day flooding period, the river floodplain is able to retain 9–14.8% of the sediment and 1.1–3.7% of the particulate P transported in the river. Incubation experiments further showed that a maximum of 11–25% of the deposited phosphorus can be released as dissolved inorganic phosphorus following deposition. The results from the best deposition model (R2 = 0.42 for sediment and R2 = 0.44 for particulate P) show that work should be done to further improve the performance of these models.

Additional keywords: deposition models, flooding.


Acknowledgements

The BUFFALO-P project is supported by the Danish Ministry of Food, Agriculture and Fishery under the program ‘Animal Husbandry, the Neighbours and the Environment’ and the participating institutes. We also gratefully acknowledge the substantial assistance from Tommy Silberg with the laboratory experiments and the very helpful suggestions from the guest editor and referees for the improvement of the paper.


References

Aldous, A. , McCormick, P. M. , Ferguson, C. , Graham, S. , and Craft, C. (2005). Hydrologic regime controls soil phosphorus fluxes in restoration and undisturbed wetlands. Restoration Ecology 13, 341–347.
Crossref | GoogleScholarGoogle Scholar | Blackwell M. S. A., and Maltby E. (Eds) (2006). ‘Ecoflood Guidelines – How to Use Floodplains for Flood Risk Reduction.’ (Office for Official Publications of the European Communities: Luxembourg.) Available at http://bookshop.europa.eu/ [Verified June 2009]

Bostic, E. M. , and White, J. R. (2007). Soil phosphorus and vegetation influence on wetland phosphorus release after simulated droughts. Soil Science Society of America Journal 71, 233–238.
Danish Standards Association (1997). Water quality – determination of phosphorus – ammonium molybdate spectrometric method (identical to European Standard EN 1189:1996). Danish Standards Association, Copenhagen.

European Union (2000). Directive 2000/60/EC of the European Parliament and the Council establishing a framework for the community action in the field of water policy. European Commission, Official Journal European Community L137, 1.
Fustec E., Bonte P., Fardeau J. C., Khebibeche L., Chesterifoff A., and Carru A. M. (1996). ‘La rétention des MES et des polluants associés dans les zones inondables. In Piren-Seine Rapport 1996/II, Thème ‘corridor Fluvial’, Laboratoire de Géologie Appliquée.’ (Université Pierre et Marie Curie: Paris.)

Gibbons J. D. (1971). ‘Nonparametric Statistical Inference.’ (McGraw-Hill: Tokyo.)

He, Q. , and Walling, D. E. (1997). Spatial variability of the particle size composition of overbank floodplain deposits. Water, Air, and Soil Pollution 99, 71–80.
Crossref | GoogleScholarGoogle Scholar | CAS | Kuenzler E. J., Mulholland P. J., Yarbro L. A., and Smock L. A. (1980). Distributions and budgets of carbon, phosphorus, iron and manganese in a floodplain swamp ecosystem. Report no. 157. Water Resources Research Institute of The University of North Carolina, Raleigh, NC.

Middelkoop, H. , and Asselman, N. E. M. (1998). Spatial variability of floodplain sedimentation at the event scale in the Rhine–Meuse delta, the Netherlands. Earth Surface Processes and Landforms 23, 561–573.
Crossref | GoogleScholarGoogle Scholar | Poulsen H. D., and Rubæk G. H. (2005). Fosfor i dansk landbrug. Omsætning, tab og virkemidler mod tab. Danish Agricultural Reseach Centre DJF Report. Animal farms 68.

Psenner, R. , and Pucsko, R. (1988). Phosphorus fractionation: advantages and limits of the method for study of sediment P origins and interactions. Archiv für Hydrobiologie – Beiheft der Limnologie 30, 98–110.
Snedecor G. W., and Cochran W. G. (1989). ‘Statistical Methods.’ 8th edn. (Iowa State University Press: Ames, IA.)

Steiger, J. , and Gurnell, A. M. (2002). Spatial hydrogeomorphological influences on sediment and nutrient deposition in riparian zones: observations from the Garonne River, France. Geomorphology 49, 1–23.
Crossref | GoogleScholarGoogle Scholar |

Svendsen, L. M. , Kronvang, B. , Kristensen, P. , and Græsbøl, P. (1995). Dynamics of phosphorus compounds in a lowland river system: importance of retention and non-point sources. Hydrological Processes 9, 119–142.
Crossref | GoogleScholarGoogle Scholar |

Tockner, K. , Pennetzdorfer, D. , Reiner, N. , Schiemer, F. , and Ward, J. V. (1999). Hydrological connectivity, and the exchange of organic matter and nutrients in a dynamic river floodplain system (Danube, Austria). Freshwater Biology 41, 521–535.
Crossref | GoogleScholarGoogle Scholar |

Vannote, R. L. , Minshall, G. W. , Cummins, K. W. , Sedell, J. R. , and Cushing, C. E. (1980). The river continuum concept. Canadian Journal of Fisheries and Aquatic Sciences 37, 130–137.
Crossref | GoogleScholarGoogle Scholar |

Verhoeven, J. T. A. , Beek, S. , and van Storm, W. (1983). Nutrient dynamics in small mesotrophic fens surrounded by cultivated land. I. Productivity and nutrient uptake by the vegetation in relation to the flow of eutrophicated ground water. Oecologia 60, 25–33.
Crossref | GoogleScholarGoogle Scholar |

Walling, D. E. (1999). Linking land use, erosion and sediment yields in river basins. Hydrobiologia 410, 223–240.
Crossref | GoogleScholarGoogle Scholar |

Walling, D. E. , and He, Q. (1997). Investigating spatial patterns of overbank sedimentation on river floodplains. Water, Air, and Soil Pollution 99, 9–20.
Crossref | GoogleScholarGoogle Scholar | CAS |

Walling, D. E. , and He, Q. (1998). The spatial variability of overbank sedimentation on river floodplains. Geomorphology 24, 209–223.
Crossref | GoogleScholarGoogle Scholar |