Length Scales, Rates, and Variability of Mixing Downstream of River Confluences

Abstract Past work on lateral mixing downstream of river confluences has focused on mixing at individual confluences, limiting general knowledge of this process. This study evaluates the average length scales, rates, and variability of lateral mixing downstream at 43 confluences for 150 events based on contrasts in gray‐scale intensity of confluent flows captured by aerial images. Only 45% of the events exhibit complete mixing over the length of the imaged downstream reach. The average dimensionless length scale ( s d ) of complete mixing is 7.4 times the downstream flow width and varies from s d = 1.1–26.3, but not all flows completely mix. A nonlinear spatial pattern of mixing, consistent with relations derived from shallow flow theory, reveals that mixing rates are substantially higher immediately downstream of confluences with most mixing occurring over s d < 15. The findings confirm that confluences are important locations of accelerated mixing in river networks.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-04-23
DOI
https://doi.org/10.1029/2025gl114640
Citations
3
Primary Topic
Hydrology and Sediment Transport Processes
Type
article
Field-Weighted Citation Impact
5.15

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article

Length Scales, Rates, and Variability of Mixing Downstream of River Confluences

Bruce L. Rhoads, Quinn W. Lewis, Alexander Sukhodolov, Muhammad Umar et al.
3 citations
Geophysical Research Letters
Hydrology and Sediment Transport Processes
5.15
article

Length Scales, Rates, and Variability of Mixing Downstream of River Confluences

Bruce L. Rhoads, Quinn W. Lewis, Alexander Sukhodolov, Muhammad Umar, Tasneem Haq Meem
article en
3 citations

Abstract

Abstract Past work on lateral mixing downstream of river confluences has focused on mixing at individual confluences, limiting general knowledge of this process. This study evaluates the average length scales, rates, and variability of lateral mixing downstream at 43 confluences for 150 events based on contrasts in gray‐scale intensity of confluent flows captured by aerial images. Only 45% of the events exhibit complete mixing over the length of the imaged downstream reach. The average dimensionless length scale ( s d ) of complete mixing is 7.4 times the downstream flow width and varies from s d = 1.1–26.3, but not all flows completely mix. A nonlinear spatial pattern of mixing, consistent with relations derived from shallow flow theory, reveals that mixing rates are substantially higher immediately downstream of confluences with most mixing occurring over s d < 15. The findings confirm that confluences are important locations of accelerated mixing in river networks.

Geophysical Research LettersVol. 52(8)
University of Illinois Urbana-Champaign (US), Leibniz Institute of Freshwater Ecology and Inland Fisheries (DE)
National Science Foundation, Deutsche Forschungsgemeinschaft
Openalex Percentile: Top 6%
Hydrology and Sediment Transport Processes
5.15
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