| 020 | $a9781461200796 |
| 082 | $a620.1160 |
| 099 | $aOnline resource: Birkhäuser |
| 245 | $aModeling and Mechanics of Granular and Porous Materials$h[EBook]$cedited by Gianfranco Capriz, Vito N. Ghionna, Pasquale Giovine. |
| 260 | $aBoston, MA$bBirkhäuser$c2002. |
| 300 | $aXIII, 369 pages.$bonline resource. |
| 336 | $atext |
| 338 | $aonline resource |
| 440 | $aModeling and Simulation in Science, Engineering and Technology,$x2164-3679 |
| 505 | $aI Mechanics of Porous Media -- 1 Constitutive Equations and Instabilities of Granular Materials -- 2 Micromechanical Modeling of Granular Materials -- 3 Thermodynamic Modeling of Granular Continua Exhibiting Quasi-Static Frictional Behaviour with Abrasion -- 4 Modeling of Soil Behaviour: from Micro-Mechanical Analysis to Macroscopic Description -- 5 Dynamic Thermo-Poro-Mechanical Stability Analysis of Simple Shear on Frictional Materials -- II Flow and Transport Phenomena in Particulate Materials -- 6 Mathematical Models for Soil Consolidation Problems: a State of the Art Report -- 7 Flow of Water in Rigid and Non-Rigid, Saturated and Unsaturated Soils -- 8 Mass Exchange, Diffusion and Large Deformations of Poroelastic Materials -- III Numerical Simulations -- 9 Continuum and Numerical Simulation of Porous Materials in Science and Technology -- 10 A Mathematical and Numerical Model for Finite Elastoplastic Deformations in Fluid Saturated Porous Media -- 11 Numerical Modeling of Initiation and Propagation Phases of Landslides. |
| 520 | $aSoils are complex materials: they have a particulate structure and fluids can seep through pores, mechanically interacting with the solid skeleton. Moreover, at a microscopic level, the behaviour of the solid skeleton is highly unstable. External loadings are in fact taken by grain chains which are continuously destroyed and rebuilt. Many issues of modeling, even of the physical details of the phenomena, remain open, even obscure; de Gennes listed them not long ago in a critical review. However, despite physical complexities, soil mechanics has developed on the assumption that a soil can be seen as a continuum, or better yet as a medium obtained by the superposition of two and sometimes three con and the other fluids, which occupy the same portion of tinua, one solid space. Furthermore, relatively simple and robust constitutive laws were adopted to describe the stress-strain behaviour and the interaction between the solid and the fluid continua. The contrast between the intrinsic nature of soil and the simplistic engi neering approach is self-evident. When trying to describe more and more sophisticated phenomena (static liquefaction, strain localisation, cyclic mo bility, effects of diagenesis and weathering, ..... ), the nalve description of soil must be abandoned or, at least, improved. Higher order continua, incrementally non-linear laws, micromechanical considerations must be taken into account. A new world was opened, where basic mathematical questions (such as the choice of the best tools to model phenomena and the proof of the well-posedness of the consequent problems) could be addressed. |
| 538 | $aOnline access to this digital book is restricted to subscription institutions through IP address (only for SISSA internal users) |
| 700 | $aCapriz, Gianfranco.$eeditor. |
| 700 | $aGhionna, Vito N.$eeditor. |
| 700 | $aGiovine, Pasquale.$eeditor. |
| 710 | $aSpringerLink (Online service) |
| 830 | $aModeling and Simulation in Science, Engineering and Technology, |
| 856 | $uhttp://dx.doi.org/10.1007/978-1-4612-0079-6 |
