Abstract
An analytical solution for the characteristic parameters of the nonequilibrium processes of aggradation due to sediment augmentation and degradation due to sediment diminution in alluvial channels of finite length is presented. The analytical solution for small time agrees with that for a semi‐infinite channel. The analytical solution is compared with the available experimental data. The limitations of the analytical model are explained.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
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
