2018
DOI: 10.1016/j.compgeo.2018.04.004
|View full text |Cite
|
Sign up to set email alerts
|

A semi-resolved CFD-DEM model for seepage-induced fine particle migration in gap-graded soils

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
42
0

Year Published

2019
2019
2023
2023

Publication Types

Select...
9

Relationship

0
9

Authors

Journals

citations
Cited by 136 publications
(42 citation statements)
references
References 60 publications
0
42
0
Order By: Relevance
“…The internal erosion rate is proportional to the flow velocity for both spherical and non-spherical particles, and a critical velocity exists for angular particles owing to grain interlocking which is not observed for the spherical particles (Guo et al, 2018). As shown in Figure 14, the seepage field is distributed uniformly in the fine-grained dam material which results in a global seepage failure (flowing soil), whereas it is gradually deflected with the increase in the hydraulic gradient and local seepage failure (piping) occurs in the coarse-grained dam material (Cheng et al, 2018;Shi et al, 2018).…”
Section: Discontinuous Medium Methodsmentioning
confidence: 95%
“…The internal erosion rate is proportional to the flow velocity for both spherical and non-spherical particles, and a critical velocity exists for angular particles owing to grain interlocking which is not observed for the spherical particles (Guo et al, 2018). As shown in Figure 14, the seepage field is distributed uniformly in the fine-grained dam material which results in a global seepage failure (flowing soil), whereas it is gradually deflected with the increase in the hydraulic gradient and local seepage failure (piping) occurs in the coarse-grained dam material (Cheng et al, 2018;Shi et al, 2018).…”
Section: Discontinuous Medium Methodsmentioning
confidence: 95%
“…30 For the simulation of FSI-D problems with large movement of the solids, the optimal choice is combining the computational fluid dynamics (CFD) with the discontinuous methods, for instance, the discrete element method (DEM). 31 A significant attempt is the establishment of the CFD-DEM (CFDEM) methods, [32][33][34][35] in which the simulation of the coupling between the fluid and the discontinuous solids with arbitrary large movement is accomplished. However, the FSI force in the CFDEM methods is simplified as the drag force determined by the void fraction, and the common empirical formulas were provided by Ergun 36 or Di Felice.…”
Section: Discussionmentioning
confidence: 99%
“…The coupling scheme of DEM with CFD involves two sets of discrete equations to be solved: the flow rule defined in Equations (19) and (20) for all VPs and the law of motion in DEM for all discrete elements (Section 2). The two-way coupling scheme is based on a transfer of pressure and shear stress forces from CFD to DEM and the time derivative of VP volumes from DEM to CFD.…”
Section: Two-phase Fluid Flow Modelmentioning
confidence: 99%
“…Hu et al 13 applied FVM (OpenFOAM) for investigating both the kinetics of fines' removal and the micromechanisms of suffusioninduced deformation of soils. Intensive research works have also been carried out by applying LBM in coupling with DEM [14][15][16][17][18] To model a seepage-induced fine particle migration through the skeleton formed of coarse particles, Cheng et al 19 proposed a semi-resolved CFD-DEM model, wherein a resolved fictitious domain method was used to resolve the fluid flow around coarse particles and an unresolved method based on a locally averaging theory was adopted to describe interactions between fine particles and fluid flow. To study the complicated impacts of debris flow on flexible barriers, Li and Jidong 20 proposed a discrete-based approach to couple CFD with DEM, wherein they solved the continuity equation and the locally averaged Navier-Stokes equation in a discretized fluid domain.…”
Section: Introductionmentioning
confidence: 99%