Holocene floodplain sediment storage and hillslope erosion within the Rhine catchment

@article{Hoffmann2007HoloceneFS,
  title={Holocene floodplain sediment storage and hillslope erosion within the Rhine catchment},
  author={Thomas Hoffmann and Gilles Erkens and Kim M. Cohen and Peter Houben and Jochen Seidel and Richard Dikau},
  journal={The Holocene},
  year={2007},
  volume={17},
  pages={105 - 118}
}
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… 

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References

SHOWING 1-10 OF 65 REFERENCES
Holocene alluvial sediment storage in a small river catchment in the loess area of central Belgium
Abstract Soil erosion and sediment deposition widely affect landscape development, particularly in erosion-prone areas with loess-derived soils. Nevertheless, until now, few attempts were made to
Changes in sediment flux and storage within a fluvial system: some examples from the Rhine catchment
The Rhine river system can look back on a long history of human impact. Whereas significant anthropogenic changes to the river channel started only 200 years ago, the impacts of land use have been
Holocene sediment budgets of the Rhine Delta (The Netherlands): a record of changing sediment delivery
Holocene sedimentation in the Rhine-Meuse Delta is facilitated by sea-level rise and tectonics, but most important is the result of the sediment flux received through rivers from the hinterland. The
The impact of changes in climate and land use on soil erosion, transport and deposition of suspended sediment in the River Rhine
The objective of this study was to estimate the potential effects of changes in climate and land use on the mobilization of fine sediment and the net transport of wash load from the upstream basin to
Land use and climatic impacts on the Rhine system (RheinLUCIFS): Quantifying sediment fluxes and human impact with available data
Abstract The RheinLUCIF project investigates the effects of land use and climatic impacts on sediment fluxes in the river Rhine catchment. Among the world's large rivers the Rhine system has been
HUMAN IMPACT AND VEGETATION CHANGE AS TRIGGERS FOR SEDIMENT DYNAMICS IN THE RIVER RHINE CATCHMENT
Summary: The main goal of the international LUCIFS project is to analyse the human impact on the hydrological dynamics of the river and the sediment budget. The main thesis is, that earlier human
Engineering impacts on river channels in the River Rhine catchment
It is not surprising that the entire catchment of the River Rhine was influenced by engineering projects modifying the river channel and related floodplains over a long time, based on human demand to
Sediment Flux to Basins: Causes, Controls and Consequences
There is an increasing trend in the Earth sciences towards the integration of many subdisciplines. The sedimendatry basin, is a fundamental focal point of many studies, which as a consequence often
Drainage basin structure, sediment delivery and the response to environmental change
  • K. Richards
  • Geology
    Geological Society, London, Special Publications
  • 2002
Abstract The purpose of this paper is to explore the role that drainage basins and networks play in filtering and modulating the effects of environmental change. The record of this change is often
35. Land-Ocean Sediment Transfer in Palaeotimes, and Implications for Present-Day Natural Fluvial Fluxes
Detrital fluxes to the ocean during the period from the late Jurassic to the Pliocene ranged between 2.7–5.2 Gt year–1, but increase up to 9.6–15.5 Gt –1 year in the Pliocene-Holocene. Of the
...
1
2
3
4
5
...