Reactive plasticity for clays: Application to a natural analog of longterm geomechanical effects of nuclear waste disposal

Engineering Geology

Volumn 64, Issue 2-3, 2002, Pages 195-215

  Hueckel, Tomasz ^a   Pellegrini, Rita ^b  

^a Duke University   (United States)

^b ISMES Istituto Sperimentale Modelli e Strutture   (Italy)

Author keywords

Chemo plasticity; Clays; Natural analog; Nuclear waste disposal; Re smectitization

Indexed keywords

BOREHOLES; CLAY; HEATING; MINERALOGY; RADIOACTIVE WASTES; THERMAL EFFECTS;

ILLITIZATION;

GEOLOGY;

CAM-CLAY MODEL; CHEMICAL ALTERATION; CLAY; CONTAINMENT BARRIER; LONG-TERM CHANGE; MECHANICAL PROPERTY; PLASTICITY; RADIOACTIVE WASTE; TIME DEPENDENT BEHAVIOR;

EID: 0036572636     PISSN: 00137952     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0013-7952(01)00114-4     Document Type: Article

References (41)

1. Pilot field experiment with canister embedding clay under simulated repository conditions
2. Thermal volume changes of the mineral-water system in low porosity clay soil
3. Developments in modelling of thermo-hydro-geomechanical behaviour of Boom clay and clay based buffer materials
4. Natural analogues and evidence of long term isolation capacity of clays occuring in Italy
5. Variational-Lagrangian irreversible thermodynamics of initially-stressed solids with thermomolecular diffusion and chemical reactions
6. Influence of temperature variations on soil behavior
7. Thermo-mechanical properties of deep argillaceous formations
8. Contact metamorphism /hydrothermal alteration of Tertiary basalts from the Isle of Skye, Northwest Scotland
9. Critical issues in modelling of the long-term hydro-thermal performance of natural clay barriers
10. The buffer/container experiment: Results, synthesis, issues
11. + smectites: The importance of particle geometry on dehydration and rehydration
12. Dehydration and rehydration of montmorillonite at elevated pressures and temperatures monitored using synchrotron radiation
13. Water-mineral interaction in hygro-mechanics of clays exposed to environmental loads: A mixture approach
14. Chemo-plasticity of clays subjected to flow of a single contaminant and stress
15. Reactive plasticity for clays during dehydration and rehydration: Part I. Concepts and options
16. Thermoplastic behavior of saturated clays: An experimental constitutive study
17. Thermoplasticity of saturated soils and shales: Constitutive equations
18. A note on thermo-mechanical anisotropy of clays
19. Constitutive properties of thermo-elasto-plastic behavior of deep carbonatic clays
20. Reactive plasticity for geological materials with a double structure evolving during aging
21. Estimation of illitization rate of smectite from the thermal history of Murakami deposit
22. Differentiation in rock strength in the weathered zone due to softening, swelling and shrinkage
23. Nuclear repositories in clays: The Orciatico metamorphic aureole analogy
24. Structural component of the swelling pressure of clay
25. Intrinsic failure and cracking of clay
26. The conversion of smectite to illite during diagnesis: Evidence from some illitic clays, from bentonites and sandstones
27. Physical and chemical properties of rocks and fluids for chemical mass transport calculations
28. Long-term effects of heating in clay rocks: Lessons learnt from the study of thermomechanical natural analogues
29. Essai thermo-hydromanique dans une argile profonde-Essai "Cactus"
30. Physico/chemical stability of smectite clays
31. Aspect of illitization of Kinnekulle bentonites
32. The thermal transformation of smectite to illite
33. Hydrothermal clay minerals in granodiorite of the Main Terrace, Steamboat Springs, Nevada
34. Clay minerals in hydro-thermally altered rocks at Wairakei, New Zealand
35. Mass transfer studies in sorbing porous media: I. Analytical solutions
36. Possible use of clay minerals in the search for oil
37. Illite-mica
38. Notes on determination of illite crystallinity
39. Changes in particle morphology during illitization: An experimental study
40. 2O pressure: Stability of hydrate phases, rehydration hysteresis, and the effect of interlayer cations