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Modelling of the morphological evolution of an alluvial bed: application to the middle Loire

Published on 30 May 2011 - Updated 20 June 2011
Cet article date d'il y a plus de 12 ans

This was the subject of the thesis defended by Audrey Latapie on Thursday 26 May at the François Rabelais University, Tours. Fruit of a partnership between the University of Tours and Cemagref, Lyon, it was financed by Cemagref, EDF and Mission Val de Loire. The originality of the work carried out lay in the crossing of the two partners’ disciplinary fields: fluvial geomorphology and hydrosedimentary modelling. Its contributions to the field of study include high-quality data on a long section of the middle Loire (450 km between Bec d’Allier and Montjean-sur-Loire) and simplified modelling methods.

Urban development, construction of infrastructures, extraction of gravel from the beds of watercourses followed by stopping of dredging, along with ongoing climatic change, all contribute to modification of a river system’s sedimentary balance, and may therefore interfere with good hydro-system operation. Consequently, understanding of the processes by which the beds of watercourses evolve is of great importance to scientists, river basin managers and operators who seek to set up sustainable management systems and keep structures in place working smoothly, and to anticipate environmental restoration work. 

The thesis aims to propose methods for improving understanding of the processes by which a long watercourse (several hundred kilometres) evolves, and long-term modelling (several decades). With such time and space scales, simplification of the phenomena under study is required in order to reduce the time needed for calculation of models

Thesis Supervisors: 

  • Florentina Moata, Professor, University of Tours
  • André Paquier, I.C.G.R.E.F., Cemagref, Lyon

On the Internet: 

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