Abstract
In cold-region rivers, the formation of ice cover during winter markedly modifies the hydraulic conditions, leading to enhanced local scour around in-stream infrastructures such as bridge piers. To analyze the flow characteristics and maximum local scour depth around the pier under both open-channel and ice-covered conditions with varying roughness, both experimental methods and numerical simulations were employed in this study. The findings reveal that, under rough ice-covered flow conditions, the interaction of elevated bed shear stress and intensified turbulent kinetic energy contributes to an increased maximum scour depth around the pier. Under identical approaching flow conditions, when the ratio of ice cover roughness to bed roughness increases to 1.9, the increase in maximum local scour depth around the pier becomes less pronounced owing to the enhanced energy dissipation caused by the rough ice cover. A numerical model for local scour around the pier under open-channel flow and ice-covered flow conditions was developed by integrating the RNG k − ε turbulence model with the Meyer-Peter sediment transport equation. A new formula was developed to estimate the maximum local scour depth around bridge piers considering various ice cover roughness conditions. Comparison with existing formulas demonstrates that the proposed formula achieves the highest accuracy, offering a useful reference for the design of bridge foundations in ice-affected regions.
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The datasets used and/or analyzed during the current study are available from the corresponding author on request.
Abbreviations
- B :
-
Flume width
- B/D :
-
Flume width to pier diameter ratio
- D :
-
Pier diameter
- d 50 :
-
Median particle diameter
- d s :
-
Maximum local scour depth
- Fr :
-
Froude number
- G :
-
Gravitational acceleration
- H :
-
Approaching flow depth
- k s :
-
Roughness coefficient
- κ:
-
Von Kármán constan
- n i :
-
Manning roughness coefficient of the ice cover
- n b :
-
Manning roughness coefficient of the riverbed
- n i/n b :
-
Ratio of ice cover roughness to riverbed roughness
- ρ s :
-
Sand mass density
- Q :
-
Flow rate
- TKE:
-
Turbulent kinetic energy
- \(\it \it {\text{u}}\text{*}\) :
-
Shear velocity
- U :
-
Approaching flow velocity
- U a :
-
Average velocity
- U c :
-
Incipient sediment motion in open channel flow
- U/U c :
-
Flow intensity
- y :
-
Distance of the bottom ice cover surface
- Z :
-
Distance from the riverbed
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Acknowledgements
The authors are grateful for the Joint Funds of the National Natural Science Foundation of China.
Funding
This study was supported by the Joint Funds of the National Natural Science Foundation of China (NSFC) under grant numbers U2443221 and U2243239.
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S.D.: laboratory works, data curation, formal analysis, methodology, and writing—original draft preparation; Z.Z.: conceptualization, laboratory supervision, and methodology; J.S.: conceptualization, methodology, and writing—review and editing; J.W.: conceptualization, laboratory supervision, methodology, and writing—review and editing.
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Dong, S., Zhang, Z., Wang, J. et al. Effect of ice cover roughness on local scour around bridge piers. Sci Rep (2026). https://doi.org/10.1038/s41598-025-34352-1
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DOI: https://doi.org/10.1038/s41598-025-34352-1


