06 Sep 2022
06 Sep 2022
Status: a revised version of this preprint is currently under review for the journal ESurf.

Back to pristine levels: a meta-analysis of suspended sediment transport in large German river channels

Thomas O. Hoffmann1, Yannik Baulig1, Stefan Vollmer1, Jan Blöthe2, and Peter Fiener3 Thomas O. Hoffmann et al.
  • 1Bundesanstalt für Gewässerkunde, 56068 Koblenz, Germany
  • 2Department of Geography, University of Freiburg, Schreiberstraße 20, 79098 Freiburg, Germany
  • 3Institute of Geography, University of Augsburg, Alter Postweg 118, 86165 Augsburg, Germany

Abstract. Suspended sediment is an integral part of riverine transport and functioning that has been strongly altered during the Anthropocene due to the overwhelming human pressure on soils, sediments and the water cycle. Understanding the controls of changing suspended sediment in rivers is therefore vital for effective management strategies. Here we present results from a trend analysis of suspended sediments covering 62 monitoring stations along the German waterways with more than 440 000 water samples taken between 1990 and 2010. Based on daily monitoring of suspended sediment concentration (SSC), we found significant declines of mean annual SSC and annual suspended sediment loads at 49 of 62 monitoring stations between 1990 and 2010. On average SSC declines by -0.92 mg l-1yr-1. At some stations decreases during the 20 years represent up to 50 % of the long-term average SSC. Significant decreases of SSC are associated with declining SSL loads. The contemporary suspended sediment loads of the Rhine at the German-Dutch border approaches the natural base level of ~1 Mt yr-1, which was achieved by the Rhine during the mid-Holocene when the suspended sediment load was adjusted to the Holocene climatic conditions and before the onset of increased loads due to human induced land use changes in the Rhine catchment. At this point we can only speculate regarding potential reasons for a decline in sediment supply to larger rivers. We argue that changes in soil erosion within the catchments and/or the sediment connectivity in upstream headwaters, e.g. due to the construction of small rainwater retention basins, are the major reason for declining SSC in the studied river channels.

Thomas O. Hoffmann et al.

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on esurf-2022-45', Anonymous Referee #1, 03 Dec 2022
  • RC2: 'Comment on esurf-2022-45', Oliver Francis, 12 Dec 2022
  • AC1: 'Comment on esurf-2022-45', Thomas Hoffmann, 20 Jan 2023

Thomas O. Hoffmann et al.

Thomas O. Hoffmann et al.


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Short summary
We analysed more than 440.000 measurements from the suspended sediment monitoring to show that suspended sediment concentration (SSC) in large rivers in Germany strongly decline by 50 % between 1990 and 2010. We argue that SSC achieves the natural back ground concentrations, due to reduced sediment supply. There is simple explanation for this decline, but effects of reduced supply from headwater streams are most likely the cause for declining SSC in large rivers.