1. Predicting Transverse Mixing Efficiency Downstream of a River Confluence
- Author
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Emmanuel Mignot, S. Pouchoulin, L. Gond, Nicolas Riviere, J. Le Coz, Institut National des Sciences Appliquées de Lyon (INSA Lyon), Université de Lyon-Institut National des Sciences Appliquées (INSA), Laboratoire de Mecanique des Fluides et d'Acoustique (LMFA), École Centrale de Lyon (ECL), Université de Lyon-Université de Lyon-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Institut National des Sciences Appliquées de Lyon (INSA Lyon), Université de Lyon-Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)-Centre National de la Recherche Scientifique (CNRS), RiverLy - Fonctionnement des hydrosystèmes (RiverLy), Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Region Auvergne-Rhone-Alpes-European Commission :CNRS-144140-Agence de l'eau Rhone-Mediterranee-Corse (France) : 2018 1063-Consiglio Nazionale delle Ricerche (CNR)-EDF -Region Provence-Alpes-Cote d'Azur-Region Occitanie, ANR-17-EURE-0018,H2O'LYON,School of Integrated Watershed Sciences(2017), ANR-11-LABX-0010,DRIIHM / IRDHEI,Dispositif de recherche interdisciplinaire sur les Interactions Hommes-Milieux(2011), Institut National des Sciences Appliquées (INSA)-Université de Lyon, and Riverly (Riverly)
- Subjects
010504 meteorology & atmospheric sciences ,[SDE.IE]Environmental Sciences/Environmental Engineering ,transverse mixing ,0207 environmental engineering ,River confluence ,ADCP ,02 engineering and technology ,Mechanics ,tracer ,01 natural sciences ,Transverse plane ,Downstream (manufacturing) ,13. Climate action ,TRACER ,Dispersion (optics) ,river confluence ,dispersion ,020701 environmental engineering ,Mixing (physics) ,Geology ,0105 earth and related environmental sciences ,Water Science and Technology - Abstract
International audience; Predicting mixing processes, especially transverse mixing, downstream of river confluences, is necessary for assessing and modeling the fate of pollutants transported in river networks, but it is still challenging. Typically, there is a lack of transverse mixing solutions implemented in 1-D hydrodynamical models widely used in river engineering applications. To investigate the mixing processes developing downstream of a medium-sized river confluence, three high-resolution in situ surveys are conducted at the Rhône-Saône confluence in France, based on geolocated specific conductivity and hydroacoustic measurements. Contrasting mixing situations are observed depending on hydrological conditions. In some cases, the two flows mix slowly due to turbulent shear at their vertical interface. This can be modeled by an analytical solution of the advection-diffusion equation. In other cases, the waters from one of the two tributaries move under the waters of the other tributary. The induced local circulation enhances transverse mixing but not vertical mixing and the flow remains stratified vertically, which may be missed when surface or satellite images are analyzed qualitatively. Stratification may be predicted by comparing the time scales for shear and density-driven adjustment. Shear-dominated transverse mixing of depth-averaged concentrations can be predicted analytically and implemented in 1-D hydrodynamical models. However, the initiation of apparently rapid transverse mixing due to density-driven circulation remains to be better understood and quantified. Plain Language Summary Predicting how waters mix downstream of river confluences is necessary for assessing and modeling the fate of pollutants transported in river networks, but it is still challenging. Typically, there is a lack of transverse mixing solutions implemented in models widely used in river engineering applications. To investigate the mixing processes developing downstream of a medium-sized river confluence, three high-resolution in situ surveys are conducted at the Rhône-Saône confluence in France. Contrasting slow or rapid mixing situations are observed depending on hydrological conditions. The transverse mixing of depth-averaged concentrations can be predicted analytically and implemented in 1-D hydrodynamical models. However, the initiation of rapid transverse mixing due to difference in fluid density remains to be better understood and quantified.
- Published
- 2020
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