Incipient Motion of Non-Cohesive Sediment under Ice Cover — An Experimental Study

2008 ◽  
Vol 20 (1) ◽  
pp. 117-124 ◽  
Author(s):  
Jun Wang ◽  
Jue-yi Sui ◽  
Bryan W. Karney
2014 ◽  
Vol 41 (10) ◽  
pp. 892-899 ◽  
Author(s):  
Peng Wu ◽  
Faye Hirshfield ◽  
Jueyi Sui

An experimental study was conducted to investigate the scour development around bridge abutments under ice cover with non-uniform natural sands. Two abutments and three non-uniform sediments were used in the research. The mechanism of incipient motion for non-uniform sediments under ice cover was analyzed. By introducing scour angles around two abutments, a relationship between maximum scour depth and velocity was established for clear-water scour under ice cover. Dimensionless shear stress was also calculated and compared with shear Reynolds number for non-uniform sediments. The maximum scour depth and dimensionless shear stress were investigated under both open channel, smooth cover and rough covered conditions. Results show that around the square abutment, the scour angle is smaller than that of the semi-circular abutment. For clear water scour, the maximum scour depth increases due to the presence of ice cover.


2010 ◽  
Vol 22 (1) ◽  
pp. 51-57 ◽  
Author(s):  
Guang-ming Tan ◽  
Lei Jiang ◽  
Cai-wen Shu ◽  
Ping Lv ◽  
Jun Wang

1988 ◽  
Vol 24 (7) ◽  
pp. 1137-1151 ◽  
Author(s):  
Peter R. Wilcock ◽  
John B. Southard

2020 ◽  
Vol 13 (18) ◽  
Author(s):  
Caiwen Shu ◽  
Guangming Tan ◽  
Peng Chen ◽  
Jun Wang ◽  
Ping Lv

Abstract This paper analyzes the incipient motion mechanism of consolidated cohesive sediment. An experimental device based on previous studies was designed to investigate the influencing factors of the incipient shear stress, including the consolidation time, the density of dry bulk, cohesive particles content, and the composition of sediment mixtures. The experimental results indicated that the incipient shear stress of cohesive sediment increased with the increase of consolidation time, dry bulk density, and content of cohesive particles. The incipient motion mechanism of cohesive particles was further investigated using experimental data and theoretical analysis. A formula of the incipient shear stress for cohesive sediment was proposed herein, which is related to both the content of cohesive particles and the relative dry bulk density. The proposed formula was validated by the experimental data, and the calculated values of incipient shear stress using the formula were in good agreement with the experimental results.


2001 ◽  
Vol 45 ◽  
pp. 667-672
Author(s):  
Masato SEKINE ◽  
Nobuaki IIZUKA ◽  
Kenta FUJIO

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