An insight into the unloading/reloading loops on the compression curve of natural stiff clays
Source abstract
Abstract
Abstract Oedometer tests were carried out with loading/unloading/reloading on natural stiff clays, Ypresian clays (YPClay), taken from several depths. Common unloading/reloading loops were identified. Further examination of the unloading or reloading curves shows that each path can be satisfactorily considered as bi-linear with a small and a larger slope separated by a threshold vertical stress. This threshold stress can be considered as the swelling pressure corresponding to the void ratio just before the unloading or reloading. Indeed, upon unloading, when the applied stress is higher than the threshold stress or swelling pressure, the mechanical effect is dominant and only small mechanical rebound is observed, corresponding to a small microstructure change; by contrast, when the applied stress is lower than the swelling pressure, physico-chemical effect becomes prevailing and soil swelling occurs with a larger microstructure change. Upon reloading, when the applied stress is lower than the swelling pressure, the microstructure is not significantly affected thanks to the contribution of the physico-chemical repulsive force, leading to a small volume change; on the contrary, beyond the swelling pressure, the mechanical effect becomes dominant giving rise to larger volume changes corresponding to the microstructure collapse. Like unsaturated expansive soils, it is found that there is a good relationship between the swelling pressure (threshold stress) and the void ratio just before the unloading or reloading. This is confirmed by the results from the data reported in the literature about other stiff clays such as Boom and London clays. It can be then deduced that the unloading/reloading loop is rather due to the competition between the mechanical and physico-chemical effects on the microstructure changes than the viscosity effect as commonly admitted.
Source: openaire · Quality: candidate unverified · Source record ↗
Research context
OpenAlex topics: Soil and Unsaturated Flow · Geotechnical Engineering and Soil Mechanics · Landslides and related hazards
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
References (37)
Show source-provided references
1. AFNOR · 1995
2. AFNOR · 2005
3. Agus · 2005
4. Changes in clay swelling and shear strength properties with different sample preparation techniques10.1520/GTJ11335J ↗
5. Laboratory assessment of swelling pressure of expansive soils10.1016/0169-1317(94)00032-L ↗
6. Modelling of the physical behaviour of clay barriers close to water saturation10.1016/0013-7952(95)00030-5 ↗
7. The form and function of microfabric features in a variety of natural soils10.1680/geot.1974.24.2.223 ↗
8. The behaviour of granular soils at elevated stresses
9. Investigating the time dependent behaviour of Boom clay under thermo-mechanical loading10.1680/geot.2009.59.4.319 ↗
10. Study of the structure of a sensitive Champlain clay and of its evolution during consolidation10.1139/t84-003 ↗
11. Suction and in-situ stresses of deep Boom clay samples10.1680/geot.2007.57.2.239 ↗
12. Laboratory hydro-mechanical characterisation of Boom clay at Essen and Mol10.1016/j.pce.2011.10.002 ↗
13. A study on the hydraulic conductivity of Boom clay10.1139/t11-048 ↗
14. Investigating the pore-water chemistry effects on the volume change behaviour of Boom clay10.1016/j.pce.2011.07.016 ↗
15. Volume change behaviour of clays: the influence of mineral composition, pore fluid composition and stress state10.1016/S0167-6636(03)00070-X ↗
16. Quantification of the effects of structure on the compression of a stiff clay10.1139/T08-052 ↗
17. Lessons from oedometer tests on high quality samples10.1061/(ASCE)0733-9410(1986)112:8(768) ↗
18. Geotechnical characterization of Boom clay in relation to the disposal of radioactive waste
19. The stratigraphy of the London Basin and associated deposits
20. Studying the stress–suction coupling in soils using an oedometer equipped with a high capacity tensiometer10.1007/s11709-011-0106-x ↗
21. Mitchell · 2005
22. Oedometer compression and swelling behaviour of the Callovo-Oxfordian argillite10.1016/j.ijrmms.2011.02.016 ↗
23. Critical evaluation of determining swelling pressure by swell-load method and constant volume method10.1520/GTJ102051 ↗
24. Nasreddine · 2004
25. Viscous behaviour of soil under oedometric conditions10.1139/t96-031 ↗
26. Mechanisms controlling compressibility of clays
27. The microstructure of dispersed and flocculated samples of kaolinite, illite and montmorillonite10.1139/t71-041 ↗
28. Evaluation of the influence of boundary confinement on the behaviour of unsaturated swelling clay soils10.1139/T08-125 ↗
29. Some new aspects of time effects on the stress–strain behaviour of stiff geomaterials
30. Time-dependent deformation characteristics of stiff geomaterials in engineering practice
31. Time-dependent shear deformation characteristics of geomaterials and their simulation10.3208/sandf.42.2_103 ↗
32. Nonlinear creep and swelling behavior of bentonite mixed with different sand contents under oedometric condition10.1080/1064119X.2011.560824 ↗
33. The Ypresian clays as possible host rock for radioactive waste disposal: an evaluation
34. van Olphen · 1977
35. Qualitative & quantitative mineralogical analyses on the Ypresian clay
36. Influence of dry density and water content on the swelling of a compacted bentonite10.1016/j.clay.2007.04.007 ↗
37. Experimental study on the swelling behaviour of bentonite/claystone mixture10.1016/j.enggeo.2011.10.003 ↗