EGU24-15689, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-15689
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Particle-laden gravity currents: the lock-release slumping regime at the laboratory scale

Laurent Lacaze1, Cyril Gadal1, Jean Schneider2, Cyrille Bonamy3, Julien Chauchat3, Yvan Dossmann2, Sébastien Kiesgen de Richter2, Matthieu Mercier1, Florence Naaim-Bouvet4, and Marie Rastello3
Laurent Lacaze et al.
  • 1Institut de Mécanique des Fluides de Toulouse (IMFT), Université de Toulouse, CNRS, Toulouse, France (laurent.lacaze@imft.fr)
  • 2Laboratoire Energies et Mécanique Théorique et Appliquée (LEMTA), Université de Lorraine, CNRS, Nancy, France (yvan.dossmann@univ-lorraine.fr)
  • 3LEGI, Université Grenoble Alpes, CNRS, Grenoble INP, Grenoble, France (marie.rastello@univ-grenoble-alpes.fr)
  • 4INRAE, Université Grenoble Alpes, INRAE, CNRS, IRD, Grenoble INP, IGE, Grenoble, France (florence.naaim@inrae.fr)

Particle-laden gravity currents (PLGCs) are driven by the mass difference between a heavy fluid-particle mixture and a lighter ambient liquid. They often occur in natural and industrial situations, among which a typical situation is the release of a finite volume. Here, we focus on such `dam-break' situations, which are studied using lock-release devices at the laboratory scale. The objective of the presententation is to provide a description at the macroscopic scale of the early moments of the flow, namely the slumping regime, with respect to the relevant dimensionless parameters. For this, we combine a total of 288 runs from three different lock-release devices and from two-fluids numerical simulations, which allow us to cover a large range of particle types (size and density), volume fractions, bottom slopes and geometries. By tracking the front propagation through time, we extract the dimensionless slumping velocity Fr and dimensionless characteristic slumping duration τ, on which we base our description. Our results show that the slumping velocity increases with the bottom slope, but decreases with the particle volume fraction when the latter exceeds a critical value. However, it remains independent of particle settling processes, which on the other hand affects the slumping duration. Hence, above a critical threshold, τ decreases as the ratio between the settling velocity and characteristic current velocity increases. For all these regimes, we derive scalings and energetic balances that reproduce the observed trends. The latter comparison confirms the role of initial energy transfer from the initial state towards the slumping phase on the resulting dynamics. This initial process and its characterisation remain crucial to prescribe relevant initial conditions for large-scale predictive modelling.

How to cite: Lacaze, L., Gadal, C., Schneider, J., Bonamy, C., Chauchat, J., Dossmann, Y., Kiesgen de Richter, S., Mercier, M., Naaim-Bouvet, F., and Rastello, M.: Particle-laden gravity currents: the lock-release slumping regime at the laboratory scale, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-15689, https://doi.org/10.5194/egusphere-egu24-15689, 2024.