Formation of levees, troughs and elevated channels by avalanches on erodible slopes
From MaRDI portal
Publication:4594057
DOI10.1017/jfm.2017.309zbMath1415.76709OpenAlexW2611914384MaRDI QIDQ4594057
B. P. Kokelaar, J. M. N. T. Gray, Andrew N. Edwards, S. Viroulet
Publication date: 17 November 2017
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/jfm.2017.309
Related Items (14)
On the shape and size of granular roll waves ⋮ The granular monoclinal wave ⋮ An optimization-based discrete element model for dry granular flows: application to granular collapse on erodible beds ⋮ Retrogressive failure of a static granular layer on an inclined plane ⋮ A dynamical systems view of granular flow: from monoclinal flood waves to roll waves ⋮ The granular monoclinal wave: a dynamical systems survey ⋮ Partial regularisation of the incompressible 𝜇(I)-rheology for granular flow ⋮ Constitutive relations for compressible granular flow in the inertial regime ⋮ Self-channelisation and levee formation in monodisperse granular flows ⋮ Frictional hysteresis and particle deposition in granular free-surface flows ⋮ Erosion-deposition dynamics and long distance propagation of granular avalanches ⋮ Subcritical and supercritical granular flow around an obstacle on a rough inclined plane ⋮ On the structure of granular jumps: the dynamical systems approach ⋮ Particle-size segregation in self-channelized granular flows
Cites Work
- Unnamed Item
- Erosive granular avalanches: a cross confrontation between theory and experiment
- Non-oscillatory central differencing for hyperbolic conservation laws
- A new model of granular flows over general topography with erosion and deposition
- On new erosion models of Savage-Hutter type for avalanches
- High order explicit methods for parabolic equations
- New high-resolution central schemes for nonlinear conservation laws and convection-diffusion equations
- Segregation induced instabilities of granular fronts
- Granular flow in partially filled slowly rotating drums
- Well-posed and ill-posed behaviour of the -rheology for granular flow
- A two-dimensional depth-averaged -rheology for dense granular avalanches
- Segregation-induced fingering instabilities in granular free-surface flows
- Arrested coarsening of granular roll waves
- A depth-averaged -rheology for shallow granular free-surface flows
- Scaling laws in granular flows down rough inclined planes
- On the shape of granular fronts down rough inclined planes
- Dynamical equilibrium of avalanches on a rough plane
- The motion of a finite mass of granular material down a rough incline
- Gravity-driven free surface flow of granular avalanches over complex basal topography
- Friction law for dense granular flows: application to the motion of a mass down a rough inclined plane
- Long-surface-wave instability in dense granular flows
- Shock waves, dead zones and particle-free regions in rapid granular free-surface flows
- The effects of hydraulic resistance on dam-break and other shallow inertial flows
- Segregation, recirculation and deposition of coarse particles near two-dimensional avalanche fronts
- Static and flowing regions in granular collapses down channels: Insights from a sedimenting shallow water model
- Segregation-induced finger formation in granular free-surface flows
- Multiple solutions for granular flow over a smooth two-dimensional bump
- Kapiza waves as a test for three-dimensional granular flow rheology
- Crucial role of sidewalls in granular surface flows: consequences for the rheology
This page was built for publication: Formation of levees, troughs and elevated channels by avalanches on erodible slopes
