Abstract
Channel confluences at which two channels merge have an important effect on momentum exchange and contaminant diffusion in both natural rivers and artificial canals. In this study, a three-dimensional numerical model, which is based on the Reynolds Averaged Navier–Stokes equations and Reynolds Stress Turbulence model, is applied to simulate and compare flow patterns and contaminant transport processes for different bed morphologies. The results clearly show that the distribution of contaminant concentrations is mainly controlled by the shear layer and two counter-rotating helical cells, which in turn are affected by the discharge ratio and the bed morphology. As the discharge ratio increases, the shear flow moves to the outer bank and the counter-clockwise tributary helical cell caused by flow deflection is enlarged, leading the mixing happens near the outer bank and the mixing layer distorted. The bed morphology can induce shrinkage of the separation zone and increase of the clockwise main channel helical cell, which is initiated by the interaction between the tributary helical cell and the main channel flow and strengthened by the deep scour hole. The bed morphology can also affect the distortion direction of the mixing layer. Both a large discharge ratio and the bed morphology could lead to an increase in mixing intensity.
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Schindfessel L, Creëlle S, Mulder TD (2015) Flow patterns in an open channel confluence with increasingly dominant tributary inflow. Water 7(9):4724–4751
Best, JL (1985) Flow dynamics and sediment transport at river channel confluences. Ph.D. Thesis, University of London
Best JL (1987) Flow dynamics at river channel confluences: Implications for sediment transport and bed morphology. In: Ethridge FG, Flores RM, Harvey MD (eds) Recent developments in fluvial sedimentology, vol 39. SPEM Publication, Tulsa, pp 27–35
Best JL (1988) Sediment transport and bed morphology at river channel confluences. Sedimentology 35:481–498
Biron P, Best JL, Roy AG (1996) Effects of bed discordance on flow dynamics at open channel confluences. J Hydraul Eng 122(12):676–682
Best JL, Reid I (1984) Separation zone at open-channel junctions. J Hydraul Eng 110(11):1588–1594
Yang QY, Wang XY, Lu WZ, Wang XK (2009) Experimental study on characteristics of separation zone in confluence zones in rivers. J Hydrol Eng 14(2):166–171
Constantinescu G, Miyawaki S, Rhoads B, Sukhodolov A, Kirkil G (2011) Structure of turbulent flow at a river confluence with momentum and velocity ratios close to 1: insight provided by an eddy-resolving numerical simulation. Water Resour Res 47:W05507. https://doi.org/10.1029/2010WR010018
Constantinescu G, Miyawaki S, Rhoads B, Sukhodolov A (2012) Numerical analysis of the effect of momentum ratio on the dynamics and sediment-entrainment capacity of coherent flow structures at a stream confluence. J Geophys Res 117:F04028. https://doi.org/10.1029/2012JF002452
Leite Ribeiro M, Blanckaert K, Roy AG, Schleiss AJ (2012) Flow and sediment dynamics in channel confluences. J Geophys Res 117:F01035. https://doi.org/10.1029/2011JF002171
Biron P, De Serres B, Roy AG, Best JL (1993) Shear layer turbulence at an unequal depth channel confluence. In: Clifford NJ, French JR, Hardisty J (eds) Turbulence: Perspectives on Flow and Sediment Transport. Wiley, Chichester, pp 197–213
Rhoads BL, Sukhodolov AN (2004) Spatial and temporal structure of shear layer turbulence at a stream confluence. Water Resour Res 40:W06304. https://doi.org/10.1029/2003WR002811
Yuan SY, Tang HW, Xiao Y, Qiu XH, Zhang HM, Yu DD (2016) Turbulent flow structure at a 90-degree open channel confluence: accounting for the distortion of the shear layer. J Hydro-Environ Res 12:130–147
Shakibainia A, Tabatabai MRM, Zarrati AR (2010) Three-dimensional numerical study of flow structure in channel confluences. Can J Civ Eng 37:772–781
De Serres B, Roy AG, Biron PM, Best JL (1999) Three-dimensional structure of flow at a confluence of river channels with discordant beds. Geomorphology 26:313–335
Bradbrook KF, Lane SN, Richards KS, Biron PM, Roy AG (2001) Role of bed discordance at asymmetrical river confluences. J Hydraul Eng 127:351–368
Wang XG, Yan ZM (2007) Three-dimensional simulation for effects of bed discordance on flow dynamics at Y-shaped open channel confluences. J Hydrodyn 19(5):587–593
Boyer C, Roy AG, Best JL (2006) Dynamics of a river channel confluence with discordant beds: flow turbulence, bed load sediment transport, and bed morphology. J Geophys Res 111:F04007. https://doi.org/10.1029/2005JF000458
Jirka GH (2004) Mixing and dispersion in rivers. In: Greco M, Carravetta A, Della Morte R (eds) River Flow. Taylor & Francis Group, London, pp 13–27
Gaudet JM, Roy AG (1995) Effect of bed morphology on flow mixing length at river confluences. Nature 373:138–139
Best JL, Roy AG (1991) Mixing-layer distortion at the confluence of channels of different depth. Nature 350:411–413
Mignot E, Vinkovic I, Doppler D, Riviere N (2014) Mixing layer in open-channel junction flows. Environ Fluid Mech 14(5):1027–1041
Mcguirk JJ, Rodi W (1978) A depth-averaged mathematical model for the near field of side discharges into open-channel flow. J Fluid Mech 86(4):761–781
Weerakoon SB, Tamai N (1989) Three dimensional calculation of flow structure in channel confluences using boundary-fitted coordinates. J Hydrosci Hydraul Eng 7:51–62
Weerakoon SB, Tamai N, Kawahara Y (2003) Depth-averaged flow computation at a river confluence. J Water Marit Eng 156(1):73–83
Bradbrook KF, Biron PM, Lane SN, Richards KS, Roy AG (1998) Investigation of controls on secondary circulation in a simple confluence geometry using a three-dimensional numerical model. Hydrol Process 12:1371–1396
Bradbrook KF, Lane SN, Richards KS, Biron PM, Roy AG (2000) Large eddy simulation of periodic flow characteristics at river channel confluences. J Hydraul Res 38(3):207–215
Ferguson R, Hoey T (2008) Effects of tributaries on main-channel geomorphology. In: Rice SP, Roy AG, Rhoads BL (eds) River confluences, tributaries and the fluvial network. Wiley, England, pp 183–208
Yuan SY, Li L, Amini F, Tang HW (2014) Turbulence measurement of combined wave and surge overtopping over a full scale HPTRM strengthened levee. J Waterw Port C 4:04014014
ANSYS-FLUENT® (2011) User’s Guide Release 14.0 (online). FLUENT Documentation. ANSYS Inc. http://www.ansys.com
Mohammadiun S, Neyshabouri SAAS, Naser G, Vahabi H (2016) Numerical investigation of submerged vane effects on flow pattern in a 90° junction of straight and bend open channels. Iran J Sci Technol Trans Civ Eng 40(4):349–365
Wei J, Li R, Kang P, Liu SY (2012) Study on transportation and diffusion characteristics of contaminants at flow confluence. Adv Water Sci 23(6):822–828 (In Chinese)
Rhoads BL, Sukhodolov AN (2008) Lateral momentum flux and the spatial evolution of flow within a confluence mixing interface. Water Resour Res 44:W08440. https://doi.org/10.1029/2007WR006634
Weerakoon SB, Kawahara Y, Tamai N (1991) Three dimensional flow structure in channel confluence of rectangular section. In: Proceeding X XIV congress, international association for hydraulic research, Part A, 373–380
Rhoads BL, Sukhodolov AN (2001) Field investigation of three-dimensional flow structure at stream confluences: 1. Thermal mixing and time-averaged velocities. Water Resour Res 37:2393–2410. https://doi.org/10.1029/2001WR000316
Sukhodolov AN, Rhoads BL (2001) Field investigation of three-dimensional flow structure at stream confluences: 2. Turbulence. Water Resour Res 37:2411–2424. https://doi.org/10.1029/2001WR000317
Bradbrook KF, Lane SN, Richards KS (2000) Numerical simulation of three-dimensional time-averaged flow structure at river channel confluences. Water Resour Res 36:2731–2746. https://doi.org/10.1029/2000WR900011
Biron PM, Ramamurthy AS, Han S (2004) Three-dimensional numerical modeling of mixing at river confluences. J Hydraul Eng 130(3):243–253
Lane SN, Parsons DR, Best JL, Orfeo O, Kostaschuk RA, Hardy RJ (2008) Causes of rapid mixing at a junction of two large rivers: Río Paraná and Río Paraguay, Argentina. J Geophys Res 113:F02019. https://doi.org/10.1029/2006JF000745
Acknowledgements
This research was funded by National Science Foundation of China (Grand Nos. 51239003, 51509073 and 51779080), the Research Innovation Program for Graduate Students of Jiangsu Province (Grand No. B1504703), and the Program of Introducing Talents of Discipline to Universities (111 Project, Grand No. B17015). The opinions and conclusions described in this paper are solely those of the authors and do not necessarily reflect the opinions or policies of the sponsors. Thanks are also extended to Huaihe River Basin Water Resources Protection Bureau for their support during the experiments. The authors are grateful to the anonymous reviewers for comments that helped improve the paper.
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Tang, H., Zhang, H. & Yuan, S. Hydrodynamics and contaminant transport on a degraded bed at a 90-degree channel confluence. Environ Fluid Mech 18, 443–463 (2018). https://doi.org/10.1007/s10652-017-9562-8
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DOI: https://doi.org/10.1007/s10652-017-9562-8