4.7 Article

Multi-scale description of hydro-mechanical coupling in swelling clays. Part I: Nonlinear poroelasticity

Journal

MECHANICS OF MATERIALS
Volume 171, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.mechmat.2022.104354

Keywords

Clay; Multiscale modeling; Homogenization Swelling stress; Capillary stress; Nonlinear poroelasticity

Funding

  1. Natural Sciences and Engineering Research Council of Canada (NSERC)
  2. University Research Award from the Imperial Oil Limited, Canada

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This paper presents a micromechanical description of the swelling behavior of partially saturated clays. The representative elementary volume (REV) of clay at the nano-scale consists of idealized parallel clay platelets and oblate spheroidal pores saturated with an electrolyte solution. Swelling forces at all spacing ranges are considered, and the description at the macroscopic level takes into account the couplings of mechanical, hydraulic, and electrochemical forces. The paper focuses on reversible deformation mechanisms in clay and obtains a generalized nonlinear form of Biot's poroelasticity relation with additional terms for capillary and swelling stresses. The stress description of clays is embedded with microstructural information, and a localization procedure is utilized to track microstructural changes. Material point simulations of clay swelling tests are used to investigate the baseline features of the model.
This paper presents a micromechanical description of the swelling behavior of partially saturated clays following a two-stage homogenization procedure on a three-dimensional Representative Elementary Volume (REV) of clay. At the nano-scale, the REV of clay particles includes idealized parallel clay platelets and oblate spheroidal pores in between them that are saturated with an electrolyte solution. Swelling forces at all spacing ranges, including the crystalline and osmotic regimes, are considered. At the micro-scale, the REV of clay is comprised of dispersed clay aggregates and partially saturated (variably-sized) spherical pores in between them. At issue, is reconstructing the couplings of mechanical, hydraulic and electrochemical forces at the macroscopic level and their effect on the overall behavior of clay. In Part I, we focus on reversible deformation mechanisms in clay. A generalized nonlinear form of the classical Biot's poroelasticity relation is obtained with additional terms accounting for capillary and swelling stresses. Capillary stress emerges from interaction of fluid phases at different scales, and takes into account the surface tension effects. The swelling part on the other hand, correlates with the net disjoining hydration and electrochemical forces at the nano-scale. As a result, the stress description of clays is embedded with microstructural information. In addition, a robust localization procedure is utilized to track the microstructural changes associated to micro-porosity and clay platelet spacing. The nonlinearity of the stress-strain description is shown to originate from the dependency of the particles' elasticity on spacing with electrochemical origins. Finally, base-line features of the model are investigated through material point simulations of a clay swelling test. The discrepancies between the model predictions and experimental measurements are resolved in Part II of this paper by considering also the plastic deformations within the framework developed in Part I.

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