scholarly journals Dynamic hydraulic jump and retrograde sedimentation in an open channel induced by sediment supply: experimental study and SPH simulation

2019 ◽  
Vol 16 (8) ◽  
pp. 1913-1927 ◽  
Author(s):  
Xiao-gang Zheng ◽  
Ri-dong Chen ◽  
Min Luo ◽  
Ehsan Kazemi ◽  
Xing-nian Liu
1995 ◽  
Vol 39 ◽  
pp. 391-396
Author(s):  
Kouki ONITSUKA ◽  
Masaru URA ◽  
Juichiro AKIYAMA ◽  
Sadakatsu MATSUOKA

2021 ◽  
pp. 104097
Author(s):  
Diana De Padova ◽  
Mouldi Ben Meftah ◽  
Michele Mossa ◽  
Stefano Sibilla

2020 ◽  
Vol 173 (6) ◽  
pp. 317-324
Author(s):  
Saber Ebrahimiyan ◽  
Hooman Hajikandi ◽  
Mahmood Shafai Bejestan ◽  
Saeed Jamali ◽  
Ebrahim Asadi

2016 ◽  
Vol 78 (5-3) ◽  
Author(s):  
Duratul Ain Tholibon ◽  
Junaidah Ariffin ◽  
Jazuri Abdullah ◽  
Juliana Idrus

A large number of studies both theoretical and experimental have been devoted to understand the physical mechanisms underlying the bar formation. This can be investigated by carrying out an experimental work in an erodible sand bed channel using a large-scale physical river model. The study included the various hydraulic characteristics with steady flow rates and sediment supply. An experimental work consists of four matrices of flow rate and channel width with other variables namely grains size and bed slope were kept constant. Details of bar profile development that generated using Surfer, a software used for 3D elevation plots are included.


1993 ◽  
Vol 20 (3) ◽  
pp. 536-539 ◽  
Author(s):  
Willi H. Hager

Based on a large number of experiments, a simple formula is developed for the time-averaged free surface profile of a classical hydraulic jump. This novel approach is based on the length of the roller. The resulting surface profile fits the data well for usual inflow Froude numbers in the range of 2 to 10. Key words: backwater, channel flow, hydraulics, open channel, surface profile.


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