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Role of river bank erosion in sediment budgets of catchments within the Loire river basin

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HAL Id: hal-00956633

https://hal-brgm.archives-ouvertes.fr/hal-00956633

Submitted on 7 Mar 2014

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Role of river bank erosion in sediment budgets of

catchments within the Loire river basin

Aurore Gay, Olivier Cerdan, Cécile Poisvert, Valentin Landemaine

To cite this version:

Aurore Gay, Olivier Cerdan, Cécile Poisvert, Valentin Landemaine. Role of river bank erosion in sediment budgets of catchments within the Loire river basin. EGU General Assembly 2014, Apr 2014, Wiens, Austria. �hal-00956633�

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Role ofriver bank erosion in sediment budgets of catchments within the Loire river basin

A.Gay1,2, O.Cerdan1, C.Poisvert2, V.Landemaine3 (1) BRGM, 3 avenue Claude Guillemin, 45060 Orléans BP 36009 cedex 2, France (2) GéHCO, Université de Tours, Parc de Grandmont, 37200 Tours, France

(3)UMR 6143 CNRS M2C, Université de Rouen, Place E. Blondel, 76821 Mont Saint Aignan Cedex, France

Quantifying volumes of sediments produced on hillslopes or in channels and transported or stored within river systems is necessary to establish sediment budgets. If research efforts on

hillslopeerosion processes have led to a relatively good understanding and quantification of local sources,in-channel processes remain poorly understood and quasi inexistent in global budgets. However, profound landuse changes and agricultural practices have altered river functioning, caused river bank instability and stream incision. During the past decades in France, river channelization has been perfomedextensively to allow for new agricultural practices to take place.

Starting from a recent study on the quantification of sediment fluxes for catchmentswithin the Loire river basin (Gay et al. 2013), our aim is to complete sediment budgets by taking into account various sources and sinks both on hillslope and within channel. The emphasis of this study is on river bank erosion and how bank erosion contributes to global budgets.A model of bank retreat is developed for the entire Loire river basin.

In general, our results show that bank retreat is on average quite low with approximately 1 cm.yr-1. However, a strong variability existswithin the studyarea with channels displaying values of bank retreat up to~10 cm.yr-1. Our results corroborate those found by Landemaine et al. 2013 on a small agricultural catchment. From this first step, quantification of volumes of sediment eroded from banks and available for transport should be calculated and integrated in sediment budgets to allow for a better understanding of basin functioning.

Gay A., Cerdan O., Delmas M., Desmet M., Variability of sediment yields in the Loire river basin (France): the role of small scale catchments (under review).

Landemaine V., Gay A., Cerdan O., Salvador-Blanes S., Rodriguez S. Recent morphological evolution of a headwater stream in agricultural context after channelization in the Ligoireriver (France) (in prep)

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