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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 10 | Copyright
Hydrol. Earth Syst. Sci., 17, 4031-4042, 2013
https://doi.org/10.5194/hess-17-4031-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 17 Oct 2013

Research article | 17 Oct 2013

Spatio-temporal heterogeneity of riparian soil morphology in a restored floodplain

B. Fournier1,2,3,*, C. Guenat2,3,*, G. Bullinger-Weber4, and E. A. D. Mitchell1 B. Fournier et al.
  • 1Laboratory of Soil Biology, University of Neuchâtel, Rue Emile-Argand 11, 2000 Neuchâtel, Switzerland
  • 2WSL Swiss Federal Institute for Forest, Snow and Landscape Research, Research Unit Community Ecology, Site Lausanne, station 2, 1015 Lausanne, Switzerland
  • 3Ecole Polytechnique Fédérale de Lausanne (EPFL), School of Architecture, Civil and Environmental Engineering (ENAC), Laboratory of Ecological Systems (ECOS), station 2, 1015 Lausanne, Switzerland
  • 4Biogeosciences Laboratory, Institute of Geology and Paleontology, University of Lausanne, 1015 Lausanne, Switzerland
  • *These two authors contributed equally to this paper.

Abstract. Floodplains have been intensively altered in industrialized countries, but are now increasingly being restored. It is therefore important to assess the effect of these restoration projects on the aquatic and terrestrial components of ecosystems. However, despite being functionally crucial components of terrestrial ecosystems, soils are generally overlooked in floodplain restoration assessments. We studied the spatio-temporal heterogeneity of soil morphology in a restored (riverbed widening) river reach along the River Thur (Switzerland) using three criteria (soil diversity, dynamism and typicality) and their associated indicators. We hypothesized that these criteria would correctly discriminate the post-restoration changes in soil morphology, and that these changes correspond to patterns of vascular plant diversity.

Soil diversity and dynamism increased 5 yr after the restoration, but some typical soils of braided rivers were still missing. Soil typicality and dynamism were correlated to vegetation changes. These results suggest a limited success of the project, in agreement with evaluations carried out at the same site using other, more resource-demanding, methods (e.g., soil fauna, fish diversity, ecosystem functioning).

Soil morphology provides structural and functional information on floodplain ecosystems. The spatio-temporal heterogeneity of soil morphology represents a cost-efficient ecological indicator that could easily be integrated into rapid assessment protocols of floodplain and river restoration projects.

The follow-up assessment after several major floods (≥ HQ20) should take place to allow for testing the longer-term validity of our conclusion for the River Thur site. More generally, it would be useful to apply the soil morphology indicator approach in different settings to test its broader applicability.

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