4.7 Article

A field study of near-junction-apex flow at a large river confluence and its response to the effects of floodplain flow

Journal

JOURNAL OF HYDROLOGY
Volume 610, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.jhydrol.2022.127983

Keywords

River confluence; Yangtze River; Poyang Lake; Compound channels; Hydrodynamics; Kinetic energy; Momentum correction coefficients

Funding

  1. National Natural Science Founda-tion of China [U2040205, 51779080, 52079044]
  2. Fundamental Research Funds for the Central Universities [20195025712, B200202237]
  3. 111 Project [B17015]
  4. Fok Ying Tung Edu-cation Foundation [520013312]

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A field investigation was conducted at the confluence between the Yangtze River and the outflow channel of Poyang Lake to study the confluence dynamics. The results showed that the alternate flow mechanism and momentum flux ratio had significant impacts on the characteristics of the stagnation zone, mixing interface, and secondary flow at the confluence.
A field investigation was carried out in March 2019 at the large river confluence between the Yangtze River and the outflow channel with a large inner-side floodplain of Poyang Lake using acoustic Doppler current profiling (ADCP) and water quality sampling. The study was intended to complement previous field studies carried out under different flow conditions in August and December 2018 and to investigate the effects of the alternate flow mechanism (compound channel vs single channel) of the Poyang Lake outflow channel on confluence dynamics. The main hydrodynamics and morphodynamics features were identified and comparatively discussed with those from the previous field studies. The kinetic energy and momentum correction coefficients were found to peak near the confluence apex and decay farther downstream reflecting the gradual flow recovering process in the post-confluence channel. The alternate flow mechanism (compound channel vs single channel) of the Poyang Lake outflow channel and the change in momentum flux ratio MR were found to significantly impact on the characteristics of the stagnation zone, mixing interface and secondary flow at the confluence. The smallest and the largest stagnation zone were observed at the lowest MR and as the outflow channel acted as single channel, respectively, while also the location of the mixing interface was impacted. Furthermore, secondary flow consisting of dual counter-rotating helical cells and channel scale circulation were observed as the Poyang Lake outflow channel acted as compound channel and a single channel, respectively. These results provide novel information about confluence dynamics in large river systems where one tributary may have a floodplain flow in flooding conditions.

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