1.15.5 Finite deformation of an elastic-plastic granular material

Products: Abaqus/Standard  Abaqus/Explicit  

Problem description

This example develops the homogeneous, finite-strain inelastic response of a granular material subject to uniform extension or compression in plane strain.

Results given by Carter et al. (1977) for these cases are used for comparison.

The specimen is initially stress-free and is made of an elastic, perfectly plastic material. The elasticity is linear, with a Young's modulus of 30 MPa and a Poisson's ratio of 0.3. Carter et al. assume that the inelastic response is governed by a Mohr-Coulomb failure surface, defined by the friction angle of the Coulomb line ( 30°) and the material's cohesion (c). They also assume that the cohesion is twice the Young's modulus for the extension test and 10% of the Young's modulus in the compression test. The above problem is solved using the Mohr-Coulomb plasticity model in Abaqus with the friction angle and the dilation angle equal to 30°. However, note that this Abaqus Mohr-Coulomb model is not identical to the classical Mohr-Coulomb model used by Carter because it uses a smooth flow potential.

An alternative solution is to use the associated linear Drucker-Prager surface in place of the Mohr-Coulomb surface. In this case it is necessary to relate and c to the material constants and that are used in the Drucker-Prager model. Matching procedures are discussed in Extended Drucker-Prager models, Section 23.3.1 of the Abaqus Analysis User's Guide. In this case we select a match appropriate for plane strain conditions:

The first equation gives  40°. Using the assumptions of Carter et al., the second equation gives d as 86.47 MPa ( = 120 MPa) for the extension case and d as 4.323 MPa ( = 6 MPa) for the compression case.

Uniform extension or compression of the soil sample is specified by displacement boundary conditions since the load-displacement response will be unstable for the extension case.

Results and discussion

The results are shown in Figure 1.15.5–1 for extension and in Figure 1.15.5–2 for compression. The solutions for Abaqus/Standard and Abaqus/Explicit are the same. The Drucker-Prager solutions agree well with the results given by Carter et al.; this is to be expected since the Drucker-Prager parameters are matched to the classical Mohr-Coulomb parameters under plane strain conditions. The differences between the Abaqus Mohr-Coulomb solutions and Carter's solutions are due to the fact that the Abaqus Mohr-Coulomb model uses a different flow potential. The Abaqus Mohr-Coulomb model uses a smooth flow potential that matches the classical Mohr-Coulomb surface only at the triaxial extension and compression meridians (not in plane strain).

However, one can also obtain Abaqus Mohr-Coulomb solutions that match Carter's plane strain solutions exactly. As discussed earlier, the classical Mohr-Coloumb model can be matched under plane strain conditions to an associated linear Drucker-Prager model with the flow potential

This match implies that under plane strain conditions the flow direction of the classical Mohr-Coulomb model can be alternatively calculated by the corresponding flow direction of the Drucker-Prager model with the dilation angle as computed before. Therefore, we can match the flow potential of the Abaqus Mohr-Coulomb model to that of the Drucker-Prager model. Matching between these two forms of flow potential assumes  1 and results in

which gives  22° in the Abaqus Mohr-Coulomb model. These Abaqus Mohr-Coulomb solutions are shown in Figure 1.15.5–1 and Figure 1.15.5–2 and match Carter's solutions exactly.

Input files

Abaqus/Standard input files

deformgranularmat_mc3030.inp

Extension case with the Mohr-Coulomb plasticity model ( 30° and  30°) and CPE4 elements.

deformgranularmat_dp.inp

Extension and compression cases with the linear Drucker-Prager plasticity model and CPE4 elements.

deformgranularmat_cpe4i_dp.inp

Extension case with the linear Drucker-Prager plasticity model and CPE4I incompatible mode elements.

deformgranularmat_mc3030_comp.inp

Compression case with the Mohr-Coulomb plasticity model ( 30° and  30°) and CPE4 elements.

deformgranularmat_dp_comp.inp

Compression case with the linear Drucker-Prager plasticity model and CPE4 elements.

deformgranularmat_mc3022.inp

Extension case with the Mohr-Coulomb plasticity model ( 30° and  22°) and CPE4 elements.

deformgranularmat_mc3022_comp.inp

Compression case with the Mohr-Coulomb plasticity model ( 30° and  22°) and CPE4 elements.

Abaqus/Explicit input files

granular.inp

Extension and compression cases with the linear Drucker-Prager plasticity model and CPE4R elements.

deformgranularmat_mc3030_xpl.inp

Extension case with the Mohr-Coulomb plasticity model ( 30° and  30°) and CPE4R elements.

deformgranularmat_mc3030_comp_xpl.inp

Compression case with the Mohr-Coulomb plasticity model ( 30° and  30°) and CPE4R elements.

deformgranularmat_mc3022_xpl.inp

Extension case with the Mohr-Coulomb plasticity model ( 30° and  22°) and CPE4R elements.

deformgranularmat_mc3022_comp_xpl.inp

Compression case with the Mohr-Coulomb plasticity model ( 30° and  22°) and CPE4R elements.

Reference

  • Carter,  J. P., J. R. Booker, and E. H. Davis, Finite Deformation of an Elasto-Plastic Soil,International Journal for Numerical and Analytical Methods in Geomechanics, vol. 1, pp. 25–43, 1977.

  • Figures

    Figure 1.15.5–1 Load-displacement results for uniform extension.

    Figure 1.15.5–2 Load-displacement results for uniform compression.