دانلود مقاله ISI انگلیسی شماره 21937
عنوان فارسی مقاله

تغییر شکل و تجزیه و تحلیل محل خاک نیمه اشباع

کد مقاله سال انتشار مقاله انگلیسی ترجمه فارسی تعداد کلمات
21937 2004 26 صفحه PDF سفارش دهید 9260 کلمه
خرید مقاله
پس از پرداخت، فوراً می توانید مقاله را دانلود فرمایید.
عنوان انگلیسی
Deformation and localization analysis of partially saturated soil
منبع

Publisher : Elsevier - Science Direct (الزویر - ساینس دایرکت)

Journal : Computer Methods in Applied Mechanics and Engineering, Volume 193, Issues 27–29, 9 July 2004, Pages 2885–2910

کلمات کلیدی
() نظریه محیط متخلخل - مواد تریفازیک طبیعی - جامد الاستو پلاستیک - منافذ - مایعات چسبناک - تغییر شکل و تجزیه و تحلیل محلی سازی - محاسبات تطبیقی​​ -
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پیش نمایش مقاله تغییر شکل و تجزیه و تحلیل محل خاک نیمه اشباع

چکیده انگلیسی

Deformation and localization analysis is a crucial issue and has thus been intensively investigated in the last decades. However, in contrast to solid mechanical problems, geotechnical applications do not only concern a single solid material, the soil, but they also affect the pore-fluids, water and air, and, consequently, the coupling of the solid deformation with the pore-fluid flow. As a result, both the deformation and the localization analysis must be applied to a triphasic material consisting of the soil skeleton, the pore-water and the pore-gas, which, in geotechnical engineering, is known as unsaturated or partially saturated soil. Based on a continuum mechanical approach, unsaturated soil can be described within the well-founded framework of the Theory of Porous Media (TPM), thus including saturated soil (solid matrix and pore-water) as well as empty soil (solid matrix and pore-gas) as special cases. It is the goal of the present contribution to investigate the deformation and the localization behavior of unsaturated soil and to exhibit the influence of the solid–fluid coupling on the localization analysis. In the framework of a triphasic formulation, unsaturated soil is considered as a materially incompressible elasto-plastic or elasto-viscoplastic skeleton saturated by two viscous pore-fluids, a materially incompressible pore-liquid and a materially compressible pore-gas. Assuming quasi-static situations, the numerical computations proceed from weak formulations of the momentum balance of the overall triphasic material together with the mass balance equations of the pore-fluids and Darcy-like relations for the seepage velocities. As a result, a system of strongly coupled differential-algebraic equations (DAE) occurs, which is solved by use of the FE tool PANDAS. In particular, various initial boundary-value problems are treated on the basis of time- and space-adaptive methods, thus demonstrating the efficiency of the overall formulation. Furthermore, the influence of the pore-gas constituent on the material behavior of partially saturated soil is studied with respect to fluid-flow simulations or embankment and slope failure problems.

مقدمه انگلیسی

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] and [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). Fig. 1. Pore-liquid distribution in an embankment. Figure options 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] and [9], by the assumption of viscoplastic skeleton behavior [10], [11] and [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] and [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.

نتیجه گیری انگلیسی

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, pressures, displacements and saturations in combination with mutual interactions between the individual constituents, it has been assumed that the solid skeleton and the pore-water are materially incompressible, whereas the pore-gas follows the ideal gas law. Furthermore, the interaction between the solid and the fluid materials has been based on the capillarypressure- saturation relation together with the relative-permeabilities-saturation relation by van Genuchten [26] and constitutive equations for the momentum supply terms leading to Darcy-like filter laws. Based on an elasto-plastic or an elasto-viscoplastic deformation behavior of the cohesive-frictional skeleton materials, a realistic model of partially saturated soil was obtained. On the numerical side, the triphasic model was implemented in the FE tool PANDAS such that time- and space-adaptive computations of a variety of initial boundary-value problems could be carried out. In particular, the 1-dimensional computation of a leaking soil column exhibited the difference of the fully triphasic approach in comparison to the biphasic analysis based on Reynolds’ assumption of a static gasphase. This example clearly pointed out that the gas phase in a partially saturated soil is not generally negligible. The following numerical examples additionally demonstrated the wide range of useful applications of the coupled solid–fluid behavior in the framework of the triphasic formulation. In particular, it could be shown how close the fluid saturation is coupled to the solid deformation up to the onset and the development of localization phenomena prior to a possible destruction of embankments and slopes.

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