Abstract
The statistical properties of the downstream propagation speed of the alluvial bedforms and the associated progression speeds of the individual sediments were evaluated on the basis of a series of radio-active tracer sxperiments conducted in a laboratory flume over a fairly broad range of flow conditions in which dunes were observed. The probability density functions for the progression speeds of the sediment motion were derived and found to fit well with the tracer results.
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.
