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A nonlinear, transient finite element method for coupled solvent diffusion and large deformation of hydrogels

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TLDR
In this article, a nonlinear, transient finite element formulation is presented for initial boundary value problems associated with swelling and deformation of hydrogels, based on the nonlinear continuum theory that is consistent with classical theory of linear poroelasticity.
Abstract
Hydrogels are capable of coupled mass transport and large deformation in response to external stimuli. In this paper, a nonlinear, transient finite element formulation is presented for initial boundary value problems associated with swelling and deformation of hydrogels, based on a nonlinear continuum theory that is consistent with classical theory of linear poroelasticity. A mixed finite element method is implemented with implicit time integration. The incompressible or nearly incompressible behavior at the initial stage imposes a constraint to the finite element discretization in order to satisfy the Ladyzhenskaya–Babuska–Brezzi (LBB) condition for stability of the mixed method, similar to linear poroelasticity as well as incompressible elasticity and Stokes flow; failure to choose an appropriate discretization would result in locking and numerical oscillations in transient analysis. To demonstrate the numerical method, two problems of practical interests are considered: constrained swelling and flat-punch indentation of hydrogel layers. Constrained swelling may lead to instantaneous surface instability for a soft hydrogel in a good solvent, which can be regulated by assuming a stiff surface layer. Indentation relaxation of hydrogels is simulated beyond the linear regime under plane strain conditions, in comparison with two elastic limits for the instantaneous and equilibrium states. The effects of Poisson’s ratio and loading rate are discussed. It is concluded that the present finite element method is robust and can be extended to study other transient phenomena in hydrogels.

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Minimization principles for the coupled problem of Darcy–Biot-type fluid transport in porous media linked to phase field modeling of fracture

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Molecular Characterization of Polymer Networks.

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Physics-informed neural networks for solving nonlinear diffusivity and Biot's equations.

TL;DR: In this article, the authors investigate how to extend the methodology of physics-informed neural networks to solve both the forward and inverse problems in relation to the nonlinear diffusivity and Biot's equations.
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Effect of Solvent Diffusion on Crack-Tip Fields and Driving Force for Fracture of Hydrogels

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A variational phase-field model for brittle fracture in polydisperse elastomer networks

TL;DR: In this paper, a phase-field model for brittle fracture in polydisperse elastomer networks is proposed, where the authors employ a mixed displacement-pressure formulation for the discretization of the incompressible large deformation elastic problem.
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TL;DR: In this article, the number of physical constants necessary to determine the properties of the soil is derived along with the general equations for the prediction of settlements and stresses in three-dimensional problems.
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On the existence, uniqueness and approximation of saddle-point problems arising from lagrangian multipliers

Franco Brezzi
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Some basic stress diffusion solutions for fluid-saturated elastic porous media with compressible constituents

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Journal ArticleDOI

A new finite element formulation for computational fluid dynamics: V. Circumventing the Babuscka-Brezzi condition: A stable Petrov-Galerkin formulation of

TL;DR: A new Petrov-Galerkin formulation of the Stokes problem is proposed in this paper, which possesses better stability properties than the classical Galerkin/variational method.
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