Improved Boundary Conditions for a 3D DEM Simple Shear Model

In this study, a 3D simple shear model using DEM is built based on the boundary condition of an NGI-type bidirectional simple shear apparatus. Stack of rings used as lateral constraints in a bidirectional simple shear test is modelled by layers of clumps which is possible to be moved by particles; d...

Full description

Saved in:
Bibliographic Details
Main Authors: Yao Li, Peifeng Su, Zhe Wang
Format: Article
Language:English
Published: Wiley 2020-01-01
Series:Advances in Civil Engineering
Online Access:http://dx.doi.org/10.1155/2020/5420793
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1832554092708233216
author Yao Li
Peifeng Su
Zhe Wang
author_facet Yao Li
Peifeng Su
Zhe Wang
author_sort Yao Li
collection DOAJ
description In this study, a 3D simple shear model using DEM is built based on the boundary condition of an NGI-type bidirectional simple shear apparatus. Stack of rings used as lateral constraints in a bidirectional simple shear test is modelled by layers of clumps which is possible to be moved by particles; different contact types and parameters are used to model the sand-loading caps, sand-latex membrane, and sand-sand contacts. A simple shear test using the bidirectional simple shear apparatus is performed for the calibration of the 3D DEM simple shear model. By analyzing the simulation results, the following can be concluded. (1) Rings generated by clumps can provide an accurate boundary condition, effective in computation since no contact force is needed for a clump. (2) In the simulation, the orientation of average contact force changed dramatically during shear. It is in the vertical direction (90°) before shear and changes to 45° at 40% shear strain. No shear band is observed which is consistent with the test, and particles move uniformly. (3) In the simulation, the degree of noncoaxiality is the greatest at the beginning of shear, and it is decreased during shear. However, the degree of noncoaxiality is still large at 20% shear strain where there is a 10° difference between the rotation angle of principal stress and principal strain increment.
format Article
id doaj-art-7745ca648932460e80343bf71f5b3c4b
institution Kabale University
issn 1687-8086
1687-8094
language English
publishDate 2020-01-01
publisher Wiley
record_format Article
series Advances in Civil Engineering
spelling doaj-art-7745ca648932460e80343bf71f5b3c4b2025-02-03T05:52:28ZengWileyAdvances in Civil Engineering1687-80861687-80942020-01-01202010.1155/2020/54207935420793Improved Boundary Conditions for a 3D DEM Simple Shear ModelYao Li0Peifeng Su1Zhe Wang2School of Highway, Chang’an University, Xi’an 710064, ChinaSchool of Highway, Chang’an University, Xi’an 710064, ChinaFaculty of Engineering, The University of Lishui, Lishui, ChinaIn this study, a 3D simple shear model using DEM is built based on the boundary condition of an NGI-type bidirectional simple shear apparatus. Stack of rings used as lateral constraints in a bidirectional simple shear test is modelled by layers of clumps which is possible to be moved by particles; different contact types and parameters are used to model the sand-loading caps, sand-latex membrane, and sand-sand contacts. A simple shear test using the bidirectional simple shear apparatus is performed for the calibration of the 3D DEM simple shear model. By analyzing the simulation results, the following can be concluded. (1) Rings generated by clumps can provide an accurate boundary condition, effective in computation since no contact force is needed for a clump. (2) In the simulation, the orientation of average contact force changed dramatically during shear. It is in the vertical direction (90°) before shear and changes to 45° at 40% shear strain. No shear band is observed which is consistent with the test, and particles move uniformly. (3) In the simulation, the degree of noncoaxiality is the greatest at the beginning of shear, and it is decreased during shear. However, the degree of noncoaxiality is still large at 20% shear strain where there is a 10° difference between the rotation angle of principal stress and principal strain increment.http://dx.doi.org/10.1155/2020/5420793
spellingShingle Yao Li
Peifeng Su
Zhe Wang
Improved Boundary Conditions for a 3D DEM Simple Shear Model
Advances in Civil Engineering
title Improved Boundary Conditions for a 3D DEM Simple Shear Model
title_full Improved Boundary Conditions for a 3D DEM Simple Shear Model
title_fullStr Improved Boundary Conditions for a 3D DEM Simple Shear Model
title_full_unstemmed Improved Boundary Conditions for a 3D DEM Simple Shear Model
title_short Improved Boundary Conditions for a 3D DEM Simple Shear Model
title_sort improved boundary conditions for a 3d dem simple shear model
url http://dx.doi.org/10.1155/2020/5420793
work_keys_str_mv AT yaoli improvedboundaryconditionsfora3ddemsimpleshearmodel
AT peifengsu improvedboundaryconditionsfora3ddemsimpleshearmodel
AT zhewang improvedboundaryconditionsfora3ddemsimpleshearmodel