Numerical modelling of the suspended particulate matter dynamics in a regulated river network

被引:15
作者
Launay, M. [1 ,2 ]
Dugue, V. [1 ,3 ]
Faure, J. -B. [1 ]
Coquery, M. [1 ]
Camenen, B. [1 ]
Le Coz, J. [1 ]
机构
[1] Irstea, UR RiverLy, 5 Rue Doua CS 20244, F-69625 Villeurbanne, France
[2] Stucky SA, Rue Lac 33, CH-1020 Renens, VD, Switzerland
[3] CNR, 2 Rue Andre Bonin, F-69004 Lyon, France
关键词
Suspended sediment; Suspended solids; 1-D hydrodynamical model; Numerical simulation; Rhone River; Flood; SEDIMENT TRANSPORT; RHONE RIVER; TRACE-ELEMENT; SOLID FLUXES; GRAIN-SIZE; CONSEQUENCES; CONTAMINANTS; NUTRIENTS; DELIVERY; CHANNEL;
D O I
10.1016/j.scitotenv.2019.02.015
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Understanding and predicting the propagation, deposition and resuspension 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 kilometers. This paper aims at exploring the use of a one-dimensional (1-D) hydrodynamical model for understanding the source and fate of SPM during complex events. The numerical model was applied to the May-June 2008 flood in the Lower Rhone River, France. This event was a combination of floods of the Isere (including dam flushing operations in the Lower Isere River) and Durance tributaries over a two-week period. The simulation code was used to model the SPM fluxes at a high spatial and temporal resolution using a multi-class approach. Approximately half of the 4.9 Mt of SPM measured at the outlet at Beaucaire were found to come from the Isere River and the other half from the Durance River, whereas previous studies estimated that most of the SPM flux at the outlet came from the Durance River. The amount of SPM trapped within the river network, mainly behind the first hydropower structure downstream of the Isere confluence, was estimated to be 3.7 Mt due to the deposition of the coarsest particles. Such a model proved to be able to compute the interaction of various grain size classes with dams and other structures. In turn, the quality of the results of SPM fluxes and deposition is highly sensitive to particle parameters, especially grain size distribution, and to the operational rules of reservoirs. (c) 2019 Elsevier B.V. All rights reserved.
引用
收藏
页码:591 / 605
页数:15
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