Multiphase mesh-free particle modeling of local sediment scouring with μ(I) rheology
Author(s) -
Ehsan Jafari Nodoushan,
Ahmad Shakibaeinia
Publication year - 2018
Publication title -
journal of hydroinformatics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.654
H-Index - 50
eISSN - 1465-1734
pISSN - 1464-7141
DOI - 10.2166/hydro.2018.068
Subject(s) - viscoplasticity , hagen–poiseuille equation , mechanics , geology , geotechnical engineering , rheology , compressibility , viscosity , sediment , multiphase flow , particle (ecology) , non newtonian fluid , flow (mathematics) , materials science , finite element method , engineering , geomorphology , constitutive equation , physics , structural engineering , composite material , oceanography
Sediment scouring is a common example of highly dynamic sediment transport. Considering its complexities, the accurate prediction of such a highly dynamic multiphase granular flow system is a challenge for the traditional numerical techniques that rely on a mesh system. The mesh-free particle methods are a newer generation of numerical techniques with an inherent ability to deal with the deformations and fragmentations of a multiphase continuum. This study aims at developing and evaluating a multiphase mesh-free particle model based on the weakly compressible moving particle semi-implicit (WC-MPS) formulation for simulation of sediment scouring. The sediment material is considered as a non-Newtonian viscoplastic fluid, whose behavior is predicted using a regularized μ(I) rheological model in combination with pressure-dependent yield criteria. The model is first validated for a benchmark problem of viscoplastic Poiseuille flow. It is then applied and evaluated for the study of two classical sediment scouring cases. The results show that the high-velocity flow currents and the circulations can create a low-viscosity region on the surface of the sediment continuum. Comparing the numerical results with the experimental measurements shows a good accuracy in prediction of the sediment profile, especially the shape and dimensions of the scour hole.
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