3–5 juil. 2023
Campus des Cézeaux - Aubière
Fuseau horaire Europe/Paris

Session

Lundi après-midi

3 juil. 2023, 14:00
Amphi Hennequin (Campus des Cézeaux - Aubière)

Amphi Hennequin

Campus des Cézeaux - Aubière

3, place Vasarely 63 178 Aubière

Documents de présentation

Aucun document.

  1. Raphael Maurin
    03/07/2023 14:00
    Présentation orale
    Présentation

    Bedload transport can be seen as an interaction between a granular medium and a fluid flow. This perspective and the associated modelling can benefit to both field, by on one hand considering a granular media approach to better understand and model bedload transport, and on the other hand challenging classical granular media description analyzing the complex bedload transport...

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  2. Clovis Lambert
    03/07/2023 14:50
    Présentation orale
    Présentation

    Granular media are ubiquitous in environmental processes and geophysical phenomenon such as sediment transport, landslides or avalanches. Granular media can be classified into three different regime : solid (quasi-static), liquid (dense flow) and gas (dilute flow). The transition between the motionless solid state and the dense flow state corresponding to the initiation of motion is an...

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  3. Philippe Frey (UGA, INRAE, ETNA, IGE, Grenoble)
    03/07/2023 16:00
    Présentation

    Bedload, the coarser material transported in contact with the bed by turbulent flow in stream channels, has major consequences for public safety, water resources, and environmental sustainability. Size sorting also named size segregation is responsible for our limited ability to predict sediment flux and river morphology, especially in mountains where steep slopes drive an intense transport of...

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  4. Elias Drach (Université Gustave Eiffel)
    03/07/2023 16:50
    Présentation orale
    Présentation

    In the context of modeling two-phase debris flows involving grains and fluid, some shallow water systems arise with internal variables.
    Our work focus on such a shallow water system with two internal variables and a topography $b$ which adds a nonconservative term. \

    For numerical purposes, it is desirable to deal with a system where the mathematical entropy (the physical energy of...

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