TY - GEN
T1 - 3D CFD modeling of bed changes at a laboratory channel confluence
AU - Balouchi, B.
AU - Mirzaahmad, A.
AU - Bihs, H.
AU - Ruther, N.
N1 - Publisher Copyright:
© 2024 The Author(s).
PY - 2024
Y1 - 2024
N2 - The complex three-dimensional flow at river confluence is causing river bed to react with scouring and deposition zones, which in man-made channels can cause problems for navigation, and in natural channels causes lateral movement which might be a threat to riverine structures. Although several studies have studied the sediment pattern of river confluences, a numerical method will be practical in improving the investigation of it in complex zones. In the present study, REEF3D::CFD model, solving the Reynolds-averaged NavierStokes equations with k-ω turbulence model, and sediment transport model is applied to evaluate bed changes in the river confluence. The applicability of this 3D modeling is shown by validating the results with data from laboratory. For the calculation of the free-surface, the model uses the level-set method and 5th-order weighted essentially non-oscillatory discretization scheme. The numerical setup leads to promising results and the representation of the characteristic morphodynamic features at river confluences.
AB - The complex three-dimensional flow at river confluence is causing river bed to react with scouring and deposition zones, which in man-made channels can cause problems for navigation, and in natural channels causes lateral movement which might be a threat to riverine structures. Although several studies have studied the sediment pattern of river confluences, a numerical method will be practical in improving the investigation of it in complex zones. In the present study, REEF3D::CFD model, solving the Reynolds-averaged NavierStokes equations with k-ω turbulence model, and sediment transport model is applied to evaluate bed changes in the river confluence. The applicability of this 3D modeling is shown by validating the results with data from laboratory. For the calculation of the free-surface, the model uses the level-set method and 5th-order weighted essentially non-oscillatory discretization scheme. The numerical setup leads to promising results and the representation of the characteristic morphodynamic features at river confluences.
UR - http://www.scopus.com/inward/record.url?scp=85202437272&partnerID=8YFLogxK
U2 - 10.1201/9781003323037-46
DO - 10.1201/9781003323037-46
M3 - Conference contribution
AN - SCOPUS:85202437272
SN - 9781032346137
T3 - River Flow - Proceedings of the 11th Conference on Fluvial Hydraulics, 2022
SP - 340
EP - 344
BT - River Flow - Proceedings of the 11th Conference on Fluvial Hydraulics, 2022
A2 - da Silva, Ana Maria Ferreira
A2 - Rennie, Colin
A2 - Gaskin, Susan
A2 - Lacey, Jay
A2 - MacVicar, Bruce
PB - CRC Press/Balkema
T2 - 11th International Conference on Fluvial Hydraulics, River Flow 2022
Y2 - 8 November 2022 through 10 November 2022
ER -