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The Holocene
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Holocene floodplain sediment storage and hillslope erosion within the Rhine catchment

T. Hoffmann

Department of Geography, University of Bonn, Meckenheimerallee 166, 53115 Bonn, Germany, thomas.hoffmann{at}uni-bonn.de

G. Erkens

Department of Physical Geography, Utrecht University, P.O.Box 80.115, 3508 TC Utrecht, The Netherlands

K. M. Cohen

Department of Physical Geography, Utrecht University, P.O.Box 80.115, 3508 TC Utrecht, The Netherlands

P. Houben

Department of Physical Geography, University of Frankfurt, P.O.Box 11 19 32, 60054 Frankfurt am Main, Germany

J. Seidel

Department of Physical Geography, University of Freiburg, Werderring 4, 79085 Freiburg i. Br, Germany

R. Dikau

Department of Geography, University of Bonn, Meckenheimerallee 166, 53115 Bonn, Germany

The response of fluvial systems to land use and climate change varies depending on catchment size. While forcing-response mechanisms of small catchments are reasonably well understood, the response of larger drainage basins is less clear. In particular, the impact of land use and climate change on the Rhine system is poorly understood because of the catchment size (185 000 km2) and the long history of human cultivation, which started approximately 7500 years ago. A sediment budget is calculated to specify the amount of alluvial sediment that was deposited during the Holocene and to estimate long-term soil erosion rates. The results suggest that 59±14 X 109 t of Holocene alluvial sediment is stored in the non-alpine part of the Rhine catchment (South and Central Germany, Eastern France, The Netherlands). About 50% of Holocene alluvial sediment is deposited along the trunk valley and the delta (Upper Rhine, Lower Rhine, coastal plain), while the rest is stored along the tributary valleys. The floodplain sediment storage corresponds to a mean erosion rate of 0.55±0.16 t/ha per yr (38.5±10.7 mm/kyr) across the Rhine catchment outside the Alps. This Holocene-averaged estimate amounts for sediments that were delivered to the channel network and is at the lower limit of erosion rates from other studies of different methodology.

Key Words: Floodplain • sediment storage • alluvial deposition • soil erosion • Rhine catchment • Holocene

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The Holocene, Vol. 17, No. 1, 105-118 (2007)
DOI: 10.1177/0959683607073287
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