Modeling the homogenization of a heterogeneous granular bentonite mixture

A hydro-mechanical model of a heterogeneous granular bentonite mixture is presented based on discretization into a finite number of “bentonite units”, systems in which “megapores” are considered between bentonite grains, which, in turn, contain micro- and macropores. A macroscopic approach is used,...

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Detalles Bibliográficos
Autores: Navarro Gámir, Vicente, Torres Serra, Joel|||0000-0002-2267-4570, Romero Morales, Enrique Edgar|||0000-0002-4105-8941, Asensio Sánchez, Laura
Tipo de recurso: artículo
Fecha de publicación:2023
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:2117/390629
Acceso en línea:https://hdl.handle.net/2117/390629
https://dx.doi.org/10.1016/j.compgeo.2023.105572
Access Level:acceso abierto
Palabra clave:Bentonite
Granular bentonite mixtures
Grain
Clay aggregate
Macroscopic approach
Megaporosity
Macroporosity
Microporosity
Bentonita
Àrees temàtiques de la UPC::Enginyeria civil::Geotècnia::Mecànica de sòls
Descripción
Sumario:A hydro-mechanical model of a heterogeneous granular bentonite mixture is presented based on discretization into a finite number of “bentonite units”, systems in which “megapores” are considered between bentonite grains, which, in turn, contain micro- and macropores. A macroscopic approach is used, where pore levels are associated with superposed homogeneous continua. Mixture heterogeneity is incorporated into the model considering the potentially very different percentage of megapores and grains in adjacent bentonite unit pairs. Mechanical contact is therefore affected, so a strategy is proposed based on porosity values, controlling deformability by the most deformable of the two units in contact. The constitutive formulation was implemented on a numerical solver to simulate a confined hydration test on a granular bentonite mixture with a notable initial local heterogeneity. The reproduced experimental evolution of the swelling pressure, relative humidity distribution, and water inflow was satisfactory. Porosity variation data were synthesized through histograms, describing not only the variation of the maximum and minimum porosity values but also the evolution of the porosity distribution in the mixture. This provides a quantitative description of the homogenization process, allowing an assessment of its scope and technological interest.