Extended Engelund–Hansen type sediment transport relation for mixtures based on the sand-silt-bed Lower Yellow River, China

ABSTRACT

While the grain-sorting morphodynamics of gravel- and sand-bed rivers has been intensively studied, sand-silt bed rivers such as the Lower Yellow River (LYR), China and the Pilcomayo River, Paraguay/Argentina have received much less attention. As a first step, we use a database from the LYR in the 1980s to develop a grain size specific extended Engelund–Hansen total bed material load relation. We then use this relation in two morphodynamic calculations. First, we “spin-up” the calculation from an arbitrary bed slope over 600 years to reproduce the downstream fining observed before the closing of Xiaolangdi Dam in 2000. We then cut off the sediment supply, and reproduce the observed pattern of bed coarsening as the bed armours in response to degradation. We argue that our model is likely not site-specific, but applies to other sand-silt bed rivers, basic data for which is as yet lacking.

Keywords:

• Fluvial geomorphology
• morphodynamics and channel form
• river channels
• sediment transport
• suspended sediment

Acknowledgements

We very gratefully acknowledge the students in Parker’s course, “River Morphodynamics” in the spring of 2015 for their help with data extraction, organization and analysis: C-G An, D.S. Ancalle Reyes, Z.D. Barnaal, Q-T Gao, J. Geldmeyer, A.M. Hamed, T-Y He, E. Lacunza, F.P. Maciel Yo, M.J. Reed, F.A. Neira Ruiz, J.E. San Juan Blanco, R.H. Takahashi, D-C Wang, H. Wu, R-J Zeng and R-S. Zhou.

Supplemental data

Supplemental data for this article can be accessed doi:10.1080/00221686.2018.1555554.

ORCID

Kensuke Naito http://orcid.org/0000-0001-8683-0846

Additional information

Funding

Kensuke Naito, Hongbo Ma, Jeffrey Nittrouer and Gary Parker gratefully acknowledge the National Science Foundation [EAR grants 1427262; 1209402]. Yuanfeng Zhang acknowledges the National Natural Science Foundation of China [grant 51379087]. Yuanjian Wang also acknowledges support from the National Nature Science Foundation of China [grants 51509102; 51679104; 5153000441]; Division of Earth Sciences.