Skip to main content

Research Repository

Advanced Search

Low-angle dunes in the Changjiang (Yangtze) Estuary: Flow and sediment dynamics under tidal influence

Hackney, Christopher R.; Hu, Hao; Wei, Taoyuan; Yang, Zhongyong; Hackney, Christopher; Parsons, Daniel R.

Authors

Christopher R. Hackney

Hao Hu

Taoyuan Wei

Zhongyong Yang

Christopher Hackney

Daniel R. Parsons



Abstract

It has long been highlighted that important feedbacks exist between river bed morphology, sediment transport and the turbulent flow field and that these feedbacks change in response to forcing mechanisms. However, our current understanding of bedform dynamics is largely based on studies of steady flow environments and cohesionless bed conditions. Few investigations have been made under rapidly changing flows. Here, we examine flow and sediment dynamics over low-angle dunes in unsteady flows in the Changjiang (Yangtze) Estuary, China. Topography, flow and sediment data were collected over a reach ca 1.8 km long through a semi-diurnal tidal cycle in a moderate tide of flood season. The results show that: (1) roughness length derived from the upper flow changes little with the flow reversing and displays the same value on both the ebb and flood tide. Moreover, the variability of individual bedform features plays an important role in roughness length variation. (2) Shear stress over the crest of low-angle dunes roughly represents the total spatially averaged stress over dunes in this study area, which has significant implications for advancing numerical models. (3) Changes in morphology, flow and sediment dynamics over dunes through time reveal how low-angle dunes evolve within a tidal cycle. (4) The clockwise hysteresis loops between flow dynamics and bedform features (height and aspect ratio) are also observed. The combination of suspended sediment transport and bedload transport on dune transformation and migration attributes to the clockwise hysteresis. The specific sediment composition of the riverbed, in some extent, affects the mechanism of sediment transport related to the exchange between suspended sediment and riverbed, but further investigation is needed to figure out the mechanism behind this for extended series of tides, such as spring/neap tide and tides in flooding and dry season.

Citation

Hackney, C. R., Hu, H., Wei, T., Yang, Z., Hackney, C., & Parsons, D. R. (2018). Low-angle dunes in the Changjiang (Yangtze) Estuary: Flow and sediment dynamics under tidal influence. Estuarine, coastal and shelf science, 205, 110-122. https://doi.org/10.1016/j.ecss.2018.03.009

Journal Article Type Article
Acceptance Date Mar 6, 2018
Online Publication Date Mar 10, 2018
Publication Date Mar 10, 2018
Deposit Date Mar 16, 2018
Publicly Available Date Mar 11, 2019
Journal Estuarine, Coastal and Shelf Science
Print ISSN 0272-7714
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 205
Pages 110-122
DOI https://doi.org/10.1016/j.ecss.2018.03.009
Keywords Aquatic Science; Oceanography
Public URL https://hull-repository.worktribe.com/output/742213
Publisher URL https://www.sciencedirect.com/science/article/pii/S0272771417306881

Files





You might also like



Downloadable Citations