Hydro-morphological effects of bridge-crossings on large braided/anabranched sand-bed rivers

Muhammad Rizwan Akram*, Muzaffar Khan, Alessandra Crosato

*Corresponding author for this work

Research output: Contribution to journalArticleScientificpeer-review

19 Downloads (Pure)

Abstract

In large rivers, most bridge crossings locally reduce the transverse floodplain width. This leads to adverse hydro-morphological effects, such as river bed and bank erosion, as well as increased upstream flood levels. In this study, we used a 2D morphodynamic model developed in Delft 3D to investigate the hydro-morphological impact of bridge span. The tool was applied to the Talibwala Bridge across the Chenab River in Pakistan. Our findings indicate that not only the length but also the location of the bridge span across the floodplain and bridge orientation influence the river hydro-morphodynamics. Smaller bridge spans exert more pronounced impacts, particularly during high flood events. We highlight that bridge span enlargement can serve as an effective intervention to reduce the adverse effects of existing bridges. These results emphasize the importance of considering the morphological river response during the design phase of bridges and of using morphodynamic instead of hydrodynamic models for flood level assessments.
Original languageEnglish
Pages (from-to)59-80
Number of pages22
JournalJournal of Applied Water Engineering and Research
Volume13
Issue number1
DOIs
Publication statusPublished - 2024

Bibliographical note

Green Open Access added to TU Delft Institutional Repository 'You share, we take care!' - Taverne project https://www.openaccess.nl/en/you-share-we-take-care
Otherwise as indicated in the copyright section: the publisher is the copyright holder of this work and the author uses the Dutch legislation to make this work public.

Keywords

  • Bridge crossing
  • Bridge span
  • Chenab river
  • Delft3D
  • Talibwala Bridge

Fingerprint

Dive into the research topics of 'Hydro-morphological effects of bridge-crossings on large braided/anabranched sand-bed rivers'. Together they form a unique fingerprint.

Cite this