Both osmotic and matric suction changes have a significant influence on the mechanical behaviour of clays. Despite the different types of interactions at the microstructural level, both suctions havea relevant effect on the fabric of non-expansive clays. Starting from experimental observations at the laboratory scale, it is possible to identify some common features characterizing the mechanical response of non-expansive clays to salinity and degree of saturation changes. This paper presents an elastoplasticframework to reproduce the behaviour of unsaturated clayey soils upon changes in the salt concentration of the pore fluid. In particular, it presents a strategy to include osmotic suction induced by pore fluid salinity in BBM-like models [1]. The model was implemented in the Thebes code and it was calibrated on experimental data performed on Boom clay [2] and remoulded loess [3].
A constitutive framework for the chemo-mechanical behaviour of unsaturated non-expansive clays / Gramegna, L.; Abed, A. A.; Solowski, W. T.; Musso, G.; Vecchia, G. D.. - In: E3S WEB OF CONFERENCES. - ISSN 2267-1242. - ELETTRONICO. - 382:(2023), pp. 1-6. (Intervento presentato al convegno 8th International Conference on Unsaturated Soils, UNSAT 2023 tenutosi a Milos (Grecia) nel 2 May 2023 through 5 May 2023) [10.1051/e3sconf/202338215004].
A constitutive framework for the chemo-mechanical behaviour of unsaturated non-expansive clays
Musso G.;
2023
Abstract
Both osmotic and matric suction changes have a significant influence on the mechanical behaviour of clays. Despite the different types of interactions at the microstructural level, both suctions havea relevant effect on the fabric of non-expansive clays. Starting from experimental observations at the laboratory scale, it is possible to identify some common features characterizing the mechanical response of non-expansive clays to salinity and degree of saturation changes. This paper presents an elastoplasticframework to reproduce the behaviour of unsaturated clayey soils upon changes in the salt concentration of the pore fluid. In particular, it presents a strategy to include osmotic suction induced by pore fluid salinity in BBM-like models [1]. The model was implemented in the Thebes code and it was calibrated on experimental data performed on Boom clay [2] and remoulded loess [3].File | Dimensione | Formato | |
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https://hdl.handle.net/11583/2988364