Investigation of the evolution of clay microstructure under different loading paths and impact on constitutive modelling
Part of a research programme concerning the investigation of the evolution of clay microstructure under different loading paths is presented. The material is a stiff over consolidated natural clay, strongly bonded by diagenetic processes. Its one-dimensional compression and consequential microstruct...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2020 |
| País: | España |
| Institución: | Universitat Politècnica de Catalunya (UPC) |
| Repositorio: | UPCommons. Portal del coneixement obert de la UPC |
| Idioma: | inglés |
| OAI Identifier: | oai:upcommons.upc.edu:2117/336048 |
| Acceso en línea: | https://hdl.handle.net/2117/336048 https://dx.doi.org/10.33552/GJES.2019.05.000603 |
| Access Level: | acceso abierto |
| Palabra clave: | Clay soils Clays Clay microstructure Micro to macro Microscopy SEM Sòls argilosos Àrees temàtiques de la UPC::Enginyeria civil::Geotècnia::Mecànica de sòls |
| Sumario: | Part of a research programme concerning the investigation of the evolution of clay microstructure under different loading paths is presented. The material is a stiff over consolidated natural clay, strongly bonded by diagenetic processes. Its one-dimensional compression and consequential microstructural changes are compared with those of the same clay when reconstituted. The microstructural changes are evaluated using scanning electron microscopy. The results of oedometer tests are discussed, some carried out in a purpose-built constant-rate-of- strain oedometer which enables the behaviour of the natural clay to be studied well beyond yield. The variations in swelling index, stiffness and coefficients of consolidation and permeability are compared pre- and post-yield for the two clays. Both clays are found to have significantly different states and fabrics at all stages of compression. Post-yield the structural changes in the natural clay are initially a destruction of the original fabric, and then a rearrangement of the clay particles into a systematic packing of honeycomb and perfectly oriented fabrics. The same fabric architecture is recognized at medium magnification in the reconstituted clay compressed to high pressures. Despite the different states and structures of the two clays, the trends of compression and consolidation behaviour are found to be similar. |
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