Formation of dry granular fronts and watery tails in debris flows
From MaRDI portal
Publication:5081389
DOI10.1017/JFM.2022.400OpenAlexW4281660914MaRDI QIDQ5081389
Xiannan Meng, J. M. N. T. Gray, C. G. Johnson
Publication date: 14 June 2022
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/jfm.2022.400
Related Items (2)
Two-phase MPM modeling of dry granular fronts and watery tails formed in debris flows ⋮ Particle-size segregation in self-channelized granular flows
Uses Software
Cites Work
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Modeling dynamic flows of grain-fluid mixtures by coupling the mixture theory with a dilatancy law
- The development of the concept of effective stresses
- Investigation of influence of an obstacle on granular flows by virtue of a depth-integrated theory
- New high-resolution central schemes for nonlinear conservation laws and convection-diffusion equations
- A two-dimensional depth-averaged -rheology for dense granular avalanches
- Segregation-induced fingering instabilities in granular free-surface flows
- Dense suspensions in rotating-rod flows: normal stresses and particle migration
- A depth-averaged -rheology for shallow granular free-surface flows
- A Roe-type scheme for two-phase shallow granular flows over variable topography
- A theoretical analysis of free-surface flows of saturated granular–liquid mixtures
- Scaling laws in granular flows down rough inclined planes
- On the shape of granular fronts down rough inclined planes
- A two-phase flow description of the initiation of underwater granular avalanches
- Steady inclined flows of granular-fluid mixtures
- Transition layer thickness at a fluid-porous interface
- Large particle segregation, transport and accumulation in granular free-surface flows
- Eulerian two-phase flow theory applied to fluidization
- 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 kinematics of bidisperse granular roll waves
- Particle Segregation in Dense Granular Flows
- The effects of hydraulic resistance on dam-break and other shallow inertial flows
- Instabilities and the formation of bubbles in fluidized beds
- A two-phase two-layer model for fluidized granular flows with dilatancy effects
- Discrete and continuum modelling of grain size segregation during bedload transport
- Segregation, recirculation and deposition of coarse particles near two-dimensional avalanche fronts
- Self-channelisation and levee formation in monodisperse granular flows
- A general fluid–sediment mixture model and constitutive theory validated in many flow regimes
- Ensemble averaged and mixture theory equations for incompressible fluid—particle suspensions
- A two-fluid model for avalanche and debris flows
- Sediment dynamics. Part 1. Bed-load transport by laminar shearing flows
- Segregation-induced finger formation in granular free-surface flows
- A depth-averaged debris-flow model that includes the effects of evolving dilatancy. I. Physical basis
- A depth-averaged debris-flow model that includes the effects of evolving dilatancy. II. Numerical predictions and experimental tests
- Kapiza waves as a test for three-dimensional granular flow rheology
- Shallow two-component gravity-driven flows with vertical variation
- Dynamics of particle settling and resuspension in viscous liquid films
- A theory for particle size segregation in shallow granular free-surface flows
- Open-Channel Flow
- Rheological stratification in experimental free-surface flows of granular–liquid mixtures
- Generation of Coulomb Wave Functions by Means of Recurrence Relations
- Erosion-deposition dynamics and long distance propagation of granular avalanches
This page was built for publication: Formation of dry granular fronts and watery tails in debris flows
