Efficacies of the newly devised methods to control debris flow once under wayare discussed experimentally and numerically. These methods are retarding andstoring the debris flow by the series of alternately projecting groynes, stopping thedebris flow front by removing water from it through the grating layed on the bedor on the channel wall, and changing the flow regime from inertial to macro-viscousrange, I. E., slow down the velocity by adding a kind of chemicals.First, a numerical simulation method which is useful to discuss the behaviour ofdebris flow around such structures is presented. Then, the processes of retardation, deformation and stoppage of debris flow by the structures are examined by both theflume experiments and the numerica...
Debris-flows are very destructive phenomena which can cause material damages and victims: many effor...
This report describes methods for determining the depths, velocities, and flow rates...
This report describes methods for determining the depths, velocities, and flow rates...
Debris flows typically increase in scale by entraining soil, fluid, and boulders along the flow chan...
Channelized debris-flows are a type of mass movements that involve water-charged, predominantly coar...
Channelized debris-flows are a type of mass movements that involve water-charged, predominantly coar...
As it is known, debris flows are characterized by extreme propagation rapidity and by the ability to...
As it is known, debris flows are characterized by extreme propagation rapidity and by the ability to...
Debris flows have proved to be a major worldwide hazard for more than 100 years owing to the destruc...
The principal objectives of this research are to investigate the flow mechanisms of debris flows. Th...
Debris flows are very to extremely rapid flows of saturated granular soils. Two main types of debri...
Debris flows are the naturally occurring phenomena. It is occur when poorly sediments, shaken and mi...
The mechanisms of debris flows and their interaction with mitigation structures are still not well u...
The mechanisms of debris flows and their interaction with mitigation structures are still not well u...
Debris-flow is one of the major natural hazards in Norway. The mountainous terrains of Norway are ex...
Debris-flows are very destructive phenomena which can cause material damages and victims: many effor...
This report describes methods for determining the depths, velocities, and flow rates...
This report describes methods for determining the depths, velocities, and flow rates...
Debris flows typically increase in scale by entraining soil, fluid, and boulders along the flow chan...
Channelized debris-flows are a type of mass movements that involve water-charged, predominantly coar...
Channelized debris-flows are a type of mass movements that involve water-charged, predominantly coar...
As it is known, debris flows are characterized by extreme propagation rapidity and by the ability to...
As it is known, debris flows are characterized by extreme propagation rapidity and by the ability to...
Debris flows have proved to be a major worldwide hazard for more than 100 years owing to the destruc...
The principal objectives of this research are to investigate the flow mechanisms of debris flows. Th...
Debris flows are very to extremely rapid flows of saturated granular soils. Two main types of debri...
Debris flows are the naturally occurring phenomena. It is occur when poorly sediments, shaken and mi...
The mechanisms of debris flows and their interaction with mitigation structures are still not well u...
The mechanisms of debris flows and their interaction with mitigation structures are still not well u...
Debris-flow is one of the major natural hazards in Norway. The mountainous terrains of Norway are ex...
Debris-flows are very destructive phenomena which can cause material damages and victims: many effor...
This report describes methods for determining the depths, velocities, and flow rates...
This report describes methods for determining the depths, velocities, and flow rates...