Computer Methods in Applied Mechanics and Engineering
Deformation and localization analysis of partially saturated soil
Introduction
In geotechnical engineering, there is a rapidly growing interest in the coupled analysis of the soil deformation and the pore-fluid flow. To set an example, it is evident that dykes or embankments, which are built to protect the environment from the elements of water, are generally loaded by gravitation and by a water table on one side. As a consequence, one observes both the deformation of the porous embankment structure and a flow process of the pore-content, water and air, cf. Fig. 1. Furthermore, if the water table rises or decreases rapidly driven, e.g., by natural hazards, stability problems occur, which are initiated by the localization of plastic solid deformations in narrow bands (shear bands). In order to correctly predict the overall behavior of such constructions, it is necessary to carefully investigate the coupled solid–fluid behavior of a biphasic material (solid matrix and pore-liquid) or of a triphasic material (solid matrix, pore-liquid and pore-gas). In the triphasic case, which is of course more general and contains the “saturated” material (solid matrix and pore-liquid) or the “empty” material (solid matrix and pore-gas) as special cases, a partially saturated porous solid material is considered and described within the well-founded Theory of Porous Media (TPM). Concerning the general TPM approach, the reader is referred, e.g., to the work by Truesdell and Toupin [1], Bowen [2], de Boer [3] or Ehlers [4], [5]. In the present contribution, the triphasic material under consideration is assumed to consist of a materially incompressible, elasto-plastic or elasto-viscoplastic, cohesive-frictional solid skeleton saturated by two viscous fluids, a materially incompressible pore-liquid (water) and a materially compressible pore-gas (air).
Concerning the localization analysis of solids as well as of multiphasic materials, it is well known that the computation of shear band localizations generally leads to a mathematically ill-posed problem that has to be regularized by means of additional assumptions as, e.g., the consideration of additional kinematical degrees of freedom in the sense of a micropolar continuum [6], [7], [8], [9], by the assumption of viscoplastic skeleton behavior [10], [11], [12] or by proceeding from further techniques like the consideration of gradient plasticity models [13] or of non-local approaches [14].
With regard to the organization of the following contribution, there is firstly the triphasic material for the description of partially saturated soil presented in Section 2. Therein, proceeding from a geometrically linear framework of the solid deformation, the soil matrix is considered as a cohesive-frictional material governed by a general elasto-viscoplastic description of the solid stresses based on a Hookean type elasticity law and a single-surface yield criterion [15] together with an additional plastic potential function in order to catch the non-associativity of the plastic behavior of geomaterials. Viscoplasticity is not only a convenient tool for the regularization of the shear band problem, but it also represents the basic matrix behavior of typical embankment materials like clayey silt. Furthermore, it additionally allows for a simple transfer to geomaterials plasticity. Concerning the pore-fluids, the effective pressure of the materially incompressible liquid acts as a Lagrangean, whereas the effective gas pressure is assumed to be governed by the ideal gas law. The interaction between the constituents, solid matrix, liquid and gas, is taken into consideration by additional constitutive relations for the momentum production terms, thus leading to Darcy-like relations for the seepage velocities. Finally, the fluids interact by a capillary-pressure-saturation relation based on relative permeabilities to consider the mutually interacting pore-fluid mobilities. In Section 3, the numerical treatment of the strongly coupled solid–fluid problem is described. Based on quasi-static initial boundary-value problems, the numerical computations proceed from weak formulations of the momentum balance of the overall triphasic material together with the volume and mass balance equations of the pore-fluids. As a result, a system of strongly coupled differential-algebraic equations (DAE) occurs, which can be solved by use of the FE tool PANDAS.1 This tool [16] is designed for the solution of volumetrically coupled initial boundary-value problems, where, if necessary, time- and space-adaptive methods [12], [17], [18] can be taken into consideration. Numerical examples are presented in Section 4, thus demonstrating the efficiency of the overall formulation. In particular, the draining of a soil column shows the differences of the triphasic in comparison to a biphasic formulation based on the Reynolds assumption, whereas the two-dimensional computation of diverse embankment problems together with the fully three-dimensional investigation of a slope failure situation demonstrate the full capability of the model by exhibiting the coupled behavior of the water and gas flow with the solid deformation ranging from very small strains to shear band localizations.
Section snippets
Preliminaries and basic concepts
Based on the fundamental concepts of the Theory of Porous Media, one proceeds from the hypothesis that the individual constituents, solid, liquid and gas, composing the triphasic material under consideration are in a state of ideal disarrangement, i.e., they are statistically distributed over the control space. This assumption together with the prescription of a real or of a virtual averaging process leads to a model ϕ of superimposed and interacting continua ϕα:Therein, α is the
Weak formulations of the governing field equations
The numerical treatment of initial boundary-value problems of the triphasic material under study is based on the weak formulations of the governing field equations together with discretization methods in the space and time domains. As was mentioned above, the isothermal problem is basically governed by five independent fields: the solid displacement , the seepage velocities and and the effective fluid pressures pLR and pGR. However, under quasi-static conditions, Darcy-like relations
Numerical examples
The numerical examples presented in this article exhibit typical problems in the framework of the deformation and localization analysis of unsaturated soil. As was described above, the computations proceed from a triphasic TPM formulation together with the numerical tools presented in the preceding section and implemented in the FE code PANDAS. In particular, the examples concern the draining of a soil column following the Liakopoulos test and the deformation and localization behavior of a
Conclusion
In the present contribution, a triphasic model for the description of partially saturated soil has been considered on the basis of the Theory of Porous Media. In particular, a thermodynamically consistent framework of an elasto-plastic or an elasto-viscoplastic cohesive-frictional soil skeleton saturated by the pore-fluids water and air has been presented. In order to describe the volumetrically fully coupled triphasic material with individual states of motion driven by external loads,
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