2019
DOI: 10.1016/j.scitotenv.2019.02.015
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Numerical modelling of the suspended particulate matter dynamics in a regulated river network

Abstract: Understanding and predicting the propagation, deposition and re-suspension of suspended particulate matter (SPM) in river networks is important for managing water resources, ecological habitat, pollution, navigation, hydropower generation, reservoir sedimentation, etc. Observational data are scarce and costly, and there is little feedback on the efficiency of numerical simulation tools for compensating the lack of data on a river scale of several hundreds of kilometres.

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Cited by 21 publications
(21 citation statements)
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“…The Rhône accounts for the highest mean annual discharge (ca. 1700 m 3 s -1 ) into the Western Mediterranean basin (Launay et al, 2019), including 95% of suspended particulate matter (SPM) fluxes to the French Mediterranean coast (Sadaoui et al, 2016) and 50% of GoL primary production (Lochet and Leveau, 1990). The Mediterranean Se ' very low tidal range allows the Rhône riverine plume to expand westwards into the GoL (Boudet et al, 2017;Many et al, 2018).…”
Section: Study Areamentioning
confidence: 99%
“…The Rhône accounts for the highest mean annual discharge (ca. 1700 m 3 s -1 ) into the Western Mediterranean basin (Launay et al, 2019), including 95% of suspended particulate matter (SPM) fluxes to the French Mediterranean coast (Sadaoui et al, 2016) and 50% of GoL primary production (Lochet and Leveau, 1990). The Mediterranean Se ' very low tidal range allows the Rhône riverine plume to expand westwards into the GoL (Boudet et al, 2017;Many et al, 2018).…”
Section: Study Areamentioning
confidence: 99%
“…As shown in Figure 1, 3.5 km downstream of the confluence the Rhône River 10.1029/2019WR026367 splits into two channels, the dammed, bypassed Old Rhône and the navigation canal with a hydropower plant. More than 15 similar bifurcations exist along the Rhône River between Lake Geneva and the Mediterranean Sea (Dugué et al, 2015;Launay et al, 2019). A traditional 1-D model would compute different discharges, Q right and Q left , for the two downstream branches but both concentrations would be equal to each other and equal to the cross-sectional average concentration upstream of the bifurcation.…”
Section: Application To the Improvement Of 1-d Modelsmentioning
confidence: 99%
“…In river engineering applications, 1‐D or 2‐D hydrodynamic models are commonly used to predict pollutant fate and dynamics by solving the shallow water equations coupled with the advection‐diffusion equation for solutes or suspended particulate matter (SPM; e.g., Beltaos & Arora, 1988; Launay et al, 2019). One‐dimensional models are especially useful for simulations over large river domains (e.g., El Kadi Abderrezzak et al, 2015; Launay et al, 2019). However, 1‐D hydrodynamic models coupled with the 1‐D advection‐diffusion equation consider only cross‐section averaged concentrations and assume complete mixing to occur instantaneously at each confluence.…”
Section: Introductionmentioning
confidence: 99%
“…In addition, other codes such as GSTARS3 have been successfully used to simulate the long-term longitudinal profile by Nohani and Afrous [36]. Launay et al [37] simulated the spatial and temporal dynamics of suspended particulate matter during floods. For this long-term simulation, they used the Rhone 1-D model.…”
Section: Simulation Of Longitudinal Sediment Profile In Reservoirsmentioning
confidence: 99%
“…The SRH-2D code was also used to simulate the bypass tunnel for the Yellowstone river intake by Sixta et al [22]. Amini et al [32] HEC-RAS Mohammad et al [33] HEC-RAS Castillo et al [34] HEC-RAS Nohani and Afrous [36] GSTARS3 Launay et al [37] RS3Rhône 1-D…”
Section: Route Sediments To Maintain Transport and Minimize Depositionmentioning
confidence: 99%