Adaptive asynchronous time-stepping, stopping criteria, and a posteriori error estimates for fixed-stress iterative schemes for coupled poromechanics problems (original) (raw)

Adaptive poromechanics computations based on a posteriori error estimates for fully mixed formulations of Biot’s consolidation model

Computer Methods in Applied Mechanics and Engineering, 2018

This paper is concerned with the analysis of coupled mixed finite element methods applied to the Biot's consolidation model. We consider two mixed formulations that use the stress tensor and Darcy velocity as primary variables as well as the displacement and pressure. The first formulation is with a symmetric stress tensor while the other enforces the symmetry of the stress weakly through the introduction of a Lagrange multiplier. The well-posedness of the two formulations is shown through Galerkin's method and suitable a priori estimates. The two formulations are then discretized with the backward Euler scheme in time and with two mixed finite elements in space. We present next a general and unified a posteriori error analysis which is applicable for any flux-and stress-conforming discretization. Our estimates are based on H 1 (Ω)-conforming reconstruction of the pressure and a suitable H 1 (Ω) d-conforming reconstruction of the displacement; both are continuous and piecewise affine in time. These reconstructions are used to infer a guaranteed and fully computable upper bound on the energy-type error measuring the differences between the exact and the approximate pressure and displacement. The error components resulting from the spatial and the temporal discretization are distinguished. They are then used to design an adaptive space-time algorithm. Numerical experiments illustrate the efficiency of our estimates and the performance of the adaptive algorithm.

Robust iterative schemes for non-linear poromechanics

Computational Geosciences, 2018

We consider a non-linear extension of Biot's model for poromechanics, wherein both the fluid flow and mechanical deformation are allowed to be non-linear. We perform an implicit discretization in time (backward Euler) and propose two iterative schemes for solving the non-linear problems appearing within each time step: a splitting algorithm extending the undrained split and fixed stress methods to non-linear problems, and a monolithic L-scheme. The convergence of both schemes is shown rigorously. Illustrative numerical examples are presented to confirm the applicability of the schemes and validate the theoretical results. Index terms-Biot's model L-schemes MFEM convergence analysis coupled problems poromechanics

A coupling of mixed and continuous Galerkin finite element methods for poroelasticity I: the continuous in time case

Computational Geosciences, 2007

In this paper, we formulate a finite element procedure for approximating the coupled fluid and mechanics in Biot's consolidation model of poroelasticity. Here, we approximate the pressure by a mixed finite element method and the displacements by a Galerkin method. Theoretical convergence error estimates are derived in a continuous in-time setting for a strictly positive constrained specific storage coefficient. Of particular interest is the case when the lowest-order Raviart-Thomas approximating space or cell-centered finite differences are used in the mixed formulation, and continuous piecewise linear approximations are used for displacements. This approach appears to be the one most frequently applied to existing reservoir engineering simulators.

A stabilized assumed deformation gradient finite element formulation for strongly coupled poromechanical simulations at finite strain

2013

An adaptively stabilized finite element scheme is proposed for a strongly coupled hydro-mechanical problem in fluid-infiltrating porous solids at finite strain. We first present the derivation of the poromechanics model via mixture theory in large deformation. By exploiting assumed deformation gradient techniques, we develop a numerical procedure capable of simultaneously curing the multiple locking phenomena related to shear failure, incompressibility imposed by pore-fluid and/or incompressible solid skeleton, and yet produce solutions that satisfy the inf-sup condition. The template based generic programming and automatic differentiation techniques used to implement the stabilized model are also highlighted. Finally, numerical examples are given to show the versatility and efficiency of this model.

A novel iterative method based on fixed stress rates for hydromechanical problems with nonlinear constitutive relationships

Computers and Geotechnics, 2021

This paper focuses on the development of alternative coupling strategies for hydromechanical applications considering highly nonlinear constitutive models to represent the behavior of porous media. We present a novel consistent iterative coupling formulation based on fixed stress rates to define the coupling terms between mass balance and equilibrium equations. We show that controlling stress rates allows the application of an adaptive iterative coupling scheme with single or multi-rate solutions. The proposed methodology has been implemented in a framework that manages sequential simulations, exchanges of information between models, and checks the convergence of the iterative process. We present several numerical tests in which we evaluate the stability, accuracy, and performance of the proposed coupling technique. From the results, we confirm that the rate form of the fixed stress split guarantees solution stability and yields results as accurate as those obtained through fully implicit solutions, even for highly nonlinear constitutive behavior.

Parallel Solution Methods for Porous Media Models in Biomechanics

PAMM, 2005

We present a biomechanical application of our parallel finite element model for coupled problems in solid mechanics. This programming framework provides a very lean and flexible interface, which allows to realize time-dependent nonlinear simulations. In this context, a special variant of a stabilized local Gauß-Seidel preconditioner is introduced, which can be successfully employed to large scale computations. Finally, the efficiency of the implemented algorithm is shown by a numerical example considering the axial compression of a L4-L5 motion segment of the spine. *

A coupling of mixed and discontinuous Galerkin finite-element methods for poroelasticity

Computational Geosciences, 2008

In this paper, we formulate a finite-element procedure for approximating the coupled fluid and mechanics in Biot's consolidation model of poroelasticity. We approximate the flow variables by a mixed finiteelement space and the displacement by a family of discontinuous Galerkin methods. Theoretical convergence error estimates are derived and, in particular, are shown to be independent of the constrained specific storage coefficient, c o . This suggests that our proposed algorithm is a potentially effective way to combat locking, or the nonphysical pressure oscillations, which sometimes arise in numerical algorithms for poroelasticity.

Guaranteed and computable error bounds for approximations constructed by an iterative decoupling of the Biot problem

Computers & Mathematics with Applications, 2020

The paper is concerned with guaranteed a posteriori error estimates for a class of evolutionary problems related to poroelastic media governed by the quasi-static linear Biot equations. The system is decoupled employing the fixed-stress split scheme, which leads to a semi-discrete system solved iteratively. The error bounds are derived by combining a posteriori estimates for contractive mappings with those of the functional type for elliptic partial differential equations. The estimates are applicable for any approximation in the admissible functional space and are independent of the discretization method. They are fully computable, do not contain mesh dependent constants, and provide reliable global estimates of the error measured in the energy norm. Moreover, they suggest efficient error indicators for the distribution of local errors, which can be used in adaptive procedures.

Robust a posteriori error estimation for mixed finite element approximation of linear poroelasticity

IMA Journal of Numerical Analysis, 2020

This work is dedicated to the memory of John W. Barrett, who introduced the concept of inf–sup stability to the corresponding author in the bar at the MAFELAP conference in 1981. We analyze a posteriori error estimators for locking-free mixed finite element approximation of Biot’s consolidation model. Three estimators are described. The simplest of these is a conventional residual-based estimator. We establish bounds relating the estimated and true errors, and show that these are independent of the physical parameters. The other two estimators require the solution of local problems. These local problem estimators are also shown to be reliable, efficient and robust. Numerical results are presented that validate the theoretical estimates, and illustrate the effectiveness of the estimators in guiding adaptive solution algorithms. The IFISS and T-IFISS software packages used for the computational experiments are available online.

A Fully-Conservative Finite Volume Formulation for Coupled Poro- Elastic Problems

2018

Solid mechanics is a research field that deals with the mechanical behavior of a wide variety of materials undergoing external loads. Among the various types of solids, porous materials, for instance, can be found in applications such as soil and rock mechanics, biomechanics, ceramics, etc. These applications are studied in the field of poromechanics, which is a specific branch of the solid mechanics that considers all types of porous materials. An important characteristic of such materials is that they contain a network of interconnected pore channels saturated with a fluid. In most situations the mechanical behavior of the porous matrix and the fluid flow through the pore channels are two tightly coupled phenomena interfering with each other. When the fluid moves from one region to another in the porous matrix it changes the pressure field inside the pore channels, which is perceived by the porous matrix as a force imbalance. As a consequence, the porous matrix tends to deform in ...