Abstract
In this paper, the application of the distinct element method (DEM) to frictional cohesive (c,) geomaterials
is described. A new contact bond model based on the Mohr-Coulomb failure criterion has been
implemented in PFC2D. According to this model, the bond strength can be clearly divided into two distinct
micromechanical contributions: an intergranular friction angle and a cohesive bond force. A parametric
analysis, based on several biaxial tests, has been run to validate the proposed model and to calibrate
the micromechanical parameters. Simple relationships between the macromechanical strength parameters
(c,) and the corresponding micromechanical quantities have been obtained so that they can be used to
model boundary value problems with the DEM without need of further calibration.
As an example application, the evolution of natural cliffs subject to weathering has been studied.
Different weathering scenarios have been considered for an initially vertical cliff. Firstly, the case of uniform
weathering has been studied. Although unrealistic, this case has been considered in order to validate the
DEM approach by comparison against analytical predictions available from limit analysis. Secondly, nonuniform
weathering has been studied. The results obtained clearly show that with the DEM it is possible
to realistically model boundary value problems of bonded geomaterials, which would be overwhelmingly
difficult to do with other numerical techniques.
Original language | English |
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Pages (from-to) | 1997-2031 |
Number of pages | 35 |
Journal | International Journal for Numerical and Analytical Methods in Geomechanics |
Volume | 32 |
Issue number | 17 |
DOIs | |
Publication status | Published - 10 Dec 2008 |
Keywords
- distinct element method
- bonded geomaterials
- cohesive frictional materials
- slope stability