scholarly journals Dynamics of channel bifurcations in noncohesive sediments

2003 ◽  
Vol 39 (6) ◽  
Author(s):  
Bianca Federici ◽  
Chris Paola
2021 ◽  
Vol 147 (5) ◽  
pp. 05021002
Author(s):  
Shaimaa A. Theol ◽  
Bert Jagers ◽  
F. X. Suryadi ◽  
Charlotte de Fraiture

2011 ◽  
Vol 58 (10) ◽  
pp. 986-991 ◽  
Author(s):  
Ulrich C.E. Zanke ◽  
Tai-Wen Hsu ◽  
Aron Roland ◽  
Oscar Link ◽  
Reda Diab

Author(s):  
Valeria S. Rego ◽  
Claudia M. P. M. Santos

Assessment of scour below pipelines and gravity based structures in a submarine system is revisited with evaluation of data from two inspections and results for semi-empirical simplified models. Usually semi-empirical models are based on small scale experimental data that normally consider uniform and noncohesive sediments and have been questioned as to their practical applications. Recent local metocean data is used to revisit predictions of onset of scour and scour depth for the system, which are compared to survey statistics.


1992 ◽  
Vol 25 (8) ◽  
pp. 151-164 ◽  
Author(s):  
C. Nalluri ◽  
E. M. Alvarez

This paper describes the results of a laboratory study financed by the Science and Engineering Research Council (SERC), UK. The work was carried out at the University of Newcastle upon Tyne in collaboration with the Water Research Centre's (WRc) River Basin Management Project during the period 1987-90. The present study has covered hydraulics, deposition, erosion and sediment transport, all with deposited bed. Noncohesive sands and sewer sediment analogues (with cohesive additives to sand) have been used and throughout the study comparisons between cohesive and noncohesive sediments were made. The noncohesive sediment studies suggested that the initiation of erosion and transport rates criteria in channels of circular cross-section using bed shear stress are comparable to those of wide channels. The sewer sediment analogues corresponding to type A needed a maximum mean shear stress of around 6-7 N/m2 whereas a weaker sediment (type C) needed only around 2.5 N/m2. The chosen cohesive analogues behaved as noncohesive sediments once they started moving, perhaps a phenomenon close to reality.


Sign in / Sign up

Export Citation Format

Share Document