Local scour around a bridge pier under ice-jammed flow condition – an experimental study

Abstract The appearance of an ice jam in a river crucially distorts local hydrodynamic conditions including water level, flow velocity, riverbed form and local scour processes. Laboratory experiments are used for the first time here to study ice-induced scour processes near a bridge pier. Results sh...

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Bibliographic Details
Published in:Journal of Hydrology and Hydromechanics
Main Authors: Wang, Jun, Hou, Zhixing, Sun, Hongjian, Fang, Bihe, Sui, Jueyi, Karney, Bryan
Format: Article in Journal/Newspaper
Language:English
Published: Walter de Gruyter GmbH 2021
Subjects:
Online Access:http://dx.doi.org/10.2478/johh-2021-0014
https://www.sciendo.com/pdf/10.2478/johh-2021-0014
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Summary:Abstract The appearance of an ice jam in a river crucially distorts local hydrodynamic conditions including water level, flow velocity, riverbed form and local scour processes. Laboratory experiments are used for the first time here to study ice-induced scour processes near a bridge pier. Results show that with an ice sheet cover the scour hole depth around a bridge is increased by about 10% compared to under equivalent open flow conditions. More dramatically, ice-jammed flows induce both greater scour depths and scour variability, with the maximum scour depth under an ice-jammed flow as much as 200% greater than under equivalent open flow conditions. Under an ice-jammed condition, both the maximum depth and length of scour holes around a bridge pier increase with the flow velocity while the maximum scour hole depth increases with ice-jam thickness. Also, quite naturally, the height of the resulting deposition dune downstream of a scour hole responds to flow velocity and ice jam thickness. Using the laboratory data under ice-jammed conditions, predictive relationships are derived between the flow’s Froude number and both the dimensionless maximum scour depth and the dimensionless maximum scour length.