Abstract
In debris flows over erodible beds, kinematic bed conditions such as velocity and velocity gradient are determined from the dynamic condition that the driving force must be equal to the yield stress at the bed surface. On the other hand, debris flows over rigid beds depend on the conditions; bed slope, sediment discharge rate, static friction angle of sediment and friction angle of grain to the bed surface. In present study, the differences between debris flows over erodible beds and ones over rigid beds, and their transitions are clarified theoretically by solving velocity profile, sediment concentration profile and flow resistance and experimentally by using flume data.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
