Arrays of baffles are widely used to prevent and mitigate granular flows (e.g., debris flows and landslides) in mountainous areas. A thorough understanding of the decelerating effect and the impact force of the baffle arrays is essential for engineering design and hazard mitigation. However, the interaction mechanism of granular flows and baffles is still not fully understood. In this work, numerical simulations based on the smoothed particle hydrodynamics (SPH) method are performed to investigate the influence of baffle height and inclination on the interaction between granular flows and baffles. It is found that the SPH model can well capture the flow kinematics of granular materials through the baffles and can obtain the impact force act...
Recently, debris-flow kinds of phenomena have been reproduced by means of Lagrangian methods, such a...
Shallow buried landmine explosions cause the ejection of a high velocity granular spray that impinge...
Debris avalanches develop along open slopes, with significant lateral spreading, bed entrainment and...
Rapid granular flows are one of the most catastrophic geo-disasters frequently encountered in mounta...
The use of baffle arrays behind a rigid barrier is an effective method to reduce impact force by dis...
AbstractMitigation of landslide debris hazards sometimes requires the use of structural countermeasu...
This study uses an incompressible Smoothed-Particle Hydrodynamics (SPH) model to investigate the int...
Debris flow is an important natural hazard in mountain zone because it can threaten human lives with...
A numerical study that utilizes three-dimensional discrete element method was undertaken to investig...
International audienceThis paper presents the SPH (Smoothed Particles Hydrodynamics) numerical metho...
Hazard mitigation against natural terrain landslide requires the understanding of its mobility and i...
Drainage channels are widely used for discharging debris flows into deposition basins or rivers. How...
Debris flows occur in mountainous regions during rainfall and can result in disastrous consequences ...
Since the tailing dam fails catastrophically with substantial instantaneous deformation, it is diffi...
Landslides are catastrophic geophysical phenomena, which may cause heavy fatality and property losse...
Recently, debris-flow kinds of phenomena have been reproduced by means of Lagrangian methods, such a...
Shallow buried landmine explosions cause the ejection of a high velocity granular spray that impinge...
Debris avalanches develop along open slopes, with significant lateral spreading, bed entrainment and...
Rapid granular flows are one of the most catastrophic geo-disasters frequently encountered in mounta...
The use of baffle arrays behind a rigid barrier is an effective method to reduce impact force by dis...
AbstractMitigation of landslide debris hazards sometimes requires the use of structural countermeasu...
This study uses an incompressible Smoothed-Particle Hydrodynamics (SPH) model to investigate the int...
Debris flow is an important natural hazard in mountain zone because it can threaten human lives with...
A numerical study that utilizes three-dimensional discrete element method was undertaken to investig...
International audienceThis paper presents the SPH (Smoothed Particles Hydrodynamics) numerical metho...
Hazard mitigation against natural terrain landslide requires the understanding of its mobility and i...
Drainage channels are widely used for discharging debris flows into deposition basins or rivers. How...
Debris flows occur in mountainous regions during rainfall and can result in disastrous consequences ...
Since the tailing dam fails catastrophically with substantial instantaneous deformation, it is diffi...
Landslides are catastrophic geophysical phenomena, which may cause heavy fatality and property losse...
Recently, debris-flow kinds of phenomena have been reproduced by means of Lagrangian methods, such a...
Shallow buried landmine explosions cause the ejection of a high velocity granular spray that impinge...
Debris avalanches develop along open slopes, with significant lateral spreading, bed entrainment and...