Abstract

Natural rivers and streams are observed to maintain stable banks while transporting sediment over a central bed region. The development of a numerical model that accounts for this essential feature of natural rivers and streams is discussed in this paper. The model considers the concept of momentum diffusion, and assumes a channel comprising a flat-bed region and two curving bank regions. The resulting boundary stress distribution is such that boundary particles in the flat-bed region are subjected to stresses great enough to put them in motion, while particles in the bank regions are only in a state of incipient motion. It is the combination of this channel geometry and the phenomenon of momentum diffusion that allows for the successful simulation of the “stable bank, mobile bed” condition experienced by rivers. While this paper emphasizes the theoretical and numerical aspects of the problem, a companion paper deals with the application and verification of the model. It presents design equations and grap...

Full Text
Paper version not known

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 call

Disclaimer: 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.