4.2 Article

A Large Bridge Pier in an Alluvial Channel: Local Scour versus Morphological Effects and the Role of Physical Models

期刊

JOURNAL OF HYDRAULIC ENGINEERING
卷 148, 期 8, 页码 -

出版社

ASCE-AMER SOC CIVIL ENGINEERS
DOI: 10.1061/(ASCE)HY.1943-7900.0001993

关键词

Local scour; Large pier; Physical model; Model-prototype comparison; Scour and fill; Live-bed tests; Clear-water tests; Riprap; Secondary currents; Bifurcation

资金

  1. Portuguese funds (Foundation for Science and Technology, IP) [PTDC/ECI-EGS/29835/2017-POCI-01-0145-FEDER-029835]
  2. FEDER-COMPETE2020 (POCI)

向作者/读者索取更多资源

This study investigates the effects of large piers on river morphology and fluvial processes during floods using scale model experiments and a case study. The results show that the large piers cause an imbalance in the spanwise bedload distribution, leading to changes in the river bed. Thus, it is important to consider the effects of large piers on river morphology during the bridge planning phase.
The large pier of an emblematic bridge built in 2008 in the Ebro River (Zaragoza, Spain) obstructs the flow in high floods. Clear-water scour experiments in a scale model were conducted to anticipate maximum local scour depths and design riprap protections. These proved to be effective during a large flood event in 2015, but bed aggradation under the left bridge span and deep scour under the right one, not mirroring the bed deformation observed in the model, raised concerns about the bridge safety. The effects of the protected pier on the changes in the aftermath of the 2015 flood are discussed. It is shown that a large meander upstream generated an imbalance in the spanwise bedload distribution, leading to sedimentation on the left and contraction scour on the right. The paper argues for the need to take into account the effects of large piers on river morphology at the bridge planning phase. The case study shows that using a clear-water model to design the riprap protection is adequate, but more importantly, that the fluvial processes during a flood could only be studied with a live-bed model with geometrical detail of the full river reach, namely, the upstream meander.

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