No Cover Image

Journal article 432 views 28 downloads

Vertically layered flow structure at confluence of a reservoir and tributary carrying high sediment loads

Yining Sun, Ji Li Orcid Logo, Zhixian Cao, Alistair G.L. Borthwick

Frontiers in Earth Science, Volume: 10

Swansea University Author: Ji Li Orcid Logo

  • 61370_VoR.pdf

    PDF | Version of Record

    © 2022 Sun, Li, Cao and Borthwick. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY)

    Download (3.65MB)

Abstract

Enhanced understanding of flow structure at a river confluence is essential for predictions of sediment transport and morphological evolution. To date, however, the confluent flow structure of a reservoir and tributary carrying high sediment loads has remained poorly understood, and may be verticall...

Full description

Published in: Frontiers in Earth Science
ISSN: 2296-6463
Published: Frontiers Media SA 2022
Online Access: Check full text

URI: https://cronfa.swan.ac.uk/Record/cronfa61370
Tags: Add Tag
No Tags, Be the first to tag this record!
Abstract: Enhanced understanding of flow structure at a river confluence is essential for predictions of sediment transport and morphological evolution. To date, however, the confluent flow structure of a reservoir and tributary carrying high sediment loads has remained poorly understood, and may be vertically layered sharply, featuring subaqueous sediment-laden flow, i.e., turbidity currents underneath subaerial clear water. Here a recently established 2D double layer-averaged model, able to resolve the formation, propagation, and recession of turbidity currents, is used to investigate a series of idealized laboratory-scale cases and a prototype case study of the Guxian Reservoir on the Yellow River, China. Four primary patterns of the stable, vertically layered flow structure at a reservoir-tributary confluence are identified: 1) single layers of sediment-laden inflow in both the main channel and tributary, sustained by sufficient vertical mixing; 2) a double layer in the main channel and a single layer of sediment-laden inflow in the tributary, when the sediment-laden flow in the tributary suffices to block intrusion of flow in the main channel; 3) a single layer of sediment-laden inflow in the main channel and a double layer in the tributary, induced by the intrusion of sediment-laden flow from the main channel into clear-water flow with small discharge in the tributary; and 4) double layers in both the main channel and tributary, which may be further divided into three subpatterns, as turbidity current exists in both the main channel and tributary, or in the main channel (tributary) intruding into the tributary (main channel). In response to unsteady discharge and sediment inputs from upstream, the vertically layered flow structure evolves in time, and may fall into one of the patterns identified above. Although bed deformation in the long term may modify the confluent flow, the vertically layered flow pattern remains so far as the present cases are concerned. The findings have implications for sediment transport and morphological evolution at a reservoir–tributary confluence, for which further studies are suggested to inform the optimization of reservoir operation schemes to mitigate capacity loss caused by sedimentation.
Keywords: reservoir, river confluence, turbidity current, vertically layered flow structure, Yellow River
College: Faculty of Science and Engineering
Funders: This work has been funded by the National Natural Science Foundation of China under Grant No. 12072244.