International audienceThe present study describes entrainment characteristics of bed material into debris flow, based on flume tests, numerical and dimensional analyses. Flume tests are conducted to investigate influences of bed sediment size on erosion rate by supplying debris flows having unsaturated sediment concentration over erodible beds. Experimental results show that the erosion rate decreases monotonically with increase of sediment size, although erosion rate changes with sediment concentration of debris flow body. In order to evaluate critical condition of bed sediment entrainment, a length scale which measures an effective bed shear stress is introduced. The effective bed shear stress is defined as total shear stress minus yield...
A solid physical understanding of debris-flow erosion is needed for both hazard prediction and under...
A solid physical understanding of debris-flow erosion is needed for both hazard prediction and under...
Debris flow simulations are useful for predicting the sediment supplied to watersheds from upstream ...
The present study describes entrainment characteristics of bed material into debris flow, based on ...
The present study describes entrainment characteristics of bed material into debris flow, based on ...
International audienceThe present study describes entrainment characteristics of bed material into d...
The present study describes entrainment characteristics of bed material into debris flow, based on ...
The present study describes entrainment characteristics of bed material into debris flow, based on ...
Debris flows typically increase in scale by entraining soil, fluid, and boulders along the flow chan...
Debris flows have proved to be a major worldwide hazard for more than 100 years owing to the destruc...
Debris flows can grow greatly in size by entrainment of bed material, enhancing their runout and haz...
[1] Analyses of mass and momentum exchange between a debris flow or avalanche and an underlying sedi...
Debris flows can grow greatly in size and hazardous potential by eroding bed and bank materials. How...
Debris flows can grow greatly in size and hazardous potential by eroding bed and bank materials. How...
Debris flows can grow greatly in size and hazardous potential by eroding bed and bank materials. How...
A solid physical understanding of debris-flow erosion is needed for both hazard prediction and under...
A solid physical understanding of debris-flow erosion is needed for both hazard prediction and under...
Debris flow simulations are useful for predicting the sediment supplied to watersheds from upstream ...
The present study describes entrainment characteristics of bed material into debris flow, based on ...
The present study describes entrainment characteristics of bed material into debris flow, based on ...
International audienceThe present study describes entrainment characteristics of bed material into d...
The present study describes entrainment characteristics of bed material into debris flow, based on ...
The present study describes entrainment characteristics of bed material into debris flow, based on ...
Debris flows typically increase in scale by entraining soil, fluid, and boulders along the flow chan...
Debris flows have proved to be a major worldwide hazard for more than 100 years owing to the destruc...
Debris flows can grow greatly in size by entrainment of bed material, enhancing their runout and haz...
[1] Analyses of mass and momentum exchange between a debris flow or avalanche and an underlying sedi...
Debris flows can grow greatly in size and hazardous potential by eroding bed and bank materials. How...
Debris flows can grow greatly in size and hazardous potential by eroding bed and bank materials. How...
Debris flows can grow greatly in size and hazardous potential by eroding bed and bank materials. How...
A solid physical understanding of debris-flow erosion is needed for both hazard prediction and under...
A solid physical understanding of debris-flow erosion is needed for both hazard prediction and under...
Debris flow simulations are useful for predicting the sediment supplied to watersheds from upstream ...