A kinematic model is developed to estimate the velocity and runout distance of a gravitative debris flow. The characteristics and the different stages of development of a gravitative flow are first described. The equations governing the motion during the flow are then derived based on the Newtonian translation motion with some simplified assumptions on the erosion process along the flow path. After the motion is initiated, the debris is considered to behave as a frictional material with the friction angle during motion being a function of the distance travelled measured from the initiation point. The equations derived are applied to two well-documented case records to assess their applicability. The application shows that the computed runou...
Debris flow is generally composed of a wide range of solid particles and viscous pore fluid. It flow...
Due to the complexity of the debris-flow process, numerical models to simulate propagation phenomeno...
Debris flows typically increase in scale by entraining soil, fluid, and boulders along the flow chan...
As it is known, debris flows are characterized by extreme propagation rapidity and by the ability to...
Several empirical relationships allowing a preliminary estimate of debris flow runout distances have...
Debris flows generally propagate along steep mountain torrents with dynamics primarily governed by g...
Rapid debris flows are identified among the most dangerous of all landslides. Due to their destructi...
Debris flows have proved to be a major worldwide hazard for more than 100 years owing to the destruc...
Debris flows and debris avalanches are complex, gravity-driven currents of rock, water and sediments...
Debris slides cannot be prevented because of their destructive forces, but certain measures may poss...
Debris flows are landslides that may involve large volumes of material and, due to their rapid propa...
Debris flows are landslides that may involve large volumes of material and, due to their rapid propa...
Debris flow is one of the many geo-hazards that cause a major damage worldwide. It can cause loss of...
We clarified the dynamics of debris flows in areas wherein the topography changes abruptly. First, t...
Debris flow is the natural hazard occurring in the mountainous topography. The geography of Norway m...
Debris flow is generally composed of a wide range of solid particles and viscous pore fluid. It flow...
Due to the complexity of the debris-flow process, numerical models to simulate propagation phenomeno...
Debris flows typically increase in scale by entraining soil, fluid, and boulders along the flow chan...
As it is known, debris flows are characterized by extreme propagation rapidity and by the ability to...
Several empirical relationships allowing a preliminary estimate of debris flow runout distances have...
Debris flows generally propagate along steep mountain torrents with dynamics primarily governed by g...
Rapid debris flows are identified among the most dangerous of all landslides. Due to their destructi...
Debris flows have proved to be a major worldwide hazard for more than 100 years owing to the destruc...
Debris flows and debris avalanches are complex, gravity-driven currents of rock, water and sediments...
Debris slides cannot be prevented because of their destructive forces, but certain measures may poss...
Debris flows are landslides that may involve large volumes of material and, due to their rapid propa...
Debris flows are landslides that may involve large volumes of material and, due to their rapid propa...
Debris flow is one of the many geo-hazards that cause a major damage worldwide. It can cause loss of...
We clarified the dynamics of debris flows in areas wherein the topography changes abruptly. First, t...
Debris flow is the natural hazard occurring in the mountainous topography. The geography of Norway m...
Debris flow is generally composed of a wide range of solid particles and viscous pore fluid. It flow...
Due to the complexity of the debris-flow process, numerical models to simulate propagation phenomeno...
Debris flows typically increase in scale by entraining soil, fluid, and boulders along the flow chan...