Local Scour at Complex Bridge Piers in Bangladesh Rivers: Reflections from a Large Study

Abstract

Many small-scale experimental, field, and empirical studies on bridge scour are available, however a large-scale study on local scour at a complex pier with wide variation in design parameters is still lacking. In this study, a country-wide assessment of local scour at complex piers of 239 bridges in Bangladesh is made. The hydrologic, hydraulic, and sediment data required in the assessment are obtained from secondary sources, primary measurements and samples, and numerical model simulations. An incredible number of 239 field visits are made, 1434 km of bathymetric surveys are carried out, and 478 samples of bed soils are collected and analyzed. The local scour depth is estimated using a complex pier configuration with pier, pile, and pile cap dimensions selected in consultation with structural and geotechnical engineers of bridge design. Flood frequency analysis and the HEC-RAS model simulation are used to estimate the hydrologic and hydrodynamic parameters needed in the assessment. A number of empirical formulations are used to estimate and compare the design local scours. The formulae of Melville and Coleman, Jain and Fischer, and Richardson are found to be dominant when deciding the design local scour depth at the bridge piers. Suggestions are provided to include a few additional equations in scour estimation and to develop a unified Bangladesh standard for scour depth estimation. The findings and recommendations of the study would be useful in planning and designing bridges in alluvial deltaic settings, particularly in the selection of empirical methods and mainstreaming of complex pier configuration in bridge scour assessment.

Fluvio-Geomorphic Change of the Padma-Meghna River Course Using the NDWI and MNDWI Techniques

“…The Padma transports 900 Mt of sediment annually, whereas, the Upper Meghna transports 13 Mt. (Mondal et al, 2020). The Padma is a very large alluvial river that has a 5 cm/km average slope and the Meghna River is a low-energy, multi-channel fluvial system with a system of linking channels and inter-channel zones (Alam, 1991;Chowdhury et al, 2021).…”

“…The Padma is a very large alluvial river that has a 5 cm/km average slope and the Meghna River is a low-energy, multi-channel fluvial system with a system of linking channels and inter-channel zones (Alam, 1991;Chowdhury et al, 2021). Furthermore, the Upper Meghna has a 2 cm/km average slope, and the Lower Meghna has a 5 cm/km average slope (Mondal et al, 2020;Gazi et al, 2020). Some recent research suggests that both the Padma and Meghna substantially changes in the last fifty years due to erosion, bar development and migration of the riverbank.…”