Abstract
This work deals with the development of a morphological model, suitable for computing the morphological changes in mountain rivers during a flood event. In most of the morphological river bed models developed earlier, the granulometric compo-sition of the sediment transport assumed to be uniform or represented by a material of some characteristic diameter, i.e. D50, The granulometric composition of the river bed and, particularly in the mountain rivers, is characterised by a variety of dimension of particles, which vary from fine sand to boulders. It is obvious that the uniform material assumption is far from reality and more detailed approaches must be made.
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.
