This article considers the iterative solution of a finite element discretization of the magma dynamics equations. In simplified form, the magma dynamics equations share some features of the Stokes equations. We therefore formulate, analyze, and numerically test an Elman, Silvester, and Wathen-type block preconditioner for magma dynamics. We prove analytically and demonstrate numerically the optimality of the preconditioner. The presented analysis highlights the dependence of the preconditioner on parameters in the magma dynamics equations that can affect convergence of iterative linear solvers. The analysis is verified through a range of two- and three-dimensional numerical examples on unstructured grids, from simple illustrative problems ...
We present a numerical code for the simulation of the dynamics of compressible to incompressible, mu...
The Finite Element modelling of geological faults by penalty contact elements may give rise to illco...
A convection–diffusion model for the averaged flow of a viscous, incompressible magma through an ela...
This article considers the iterative solution of a finite element discretization of the magma dynam...
This article considers the iterative solution of a finite element discretisation of the magma dynami...
This article considers the iterative solution of a finite element discretization of the magma dynami...
For a prescribed porosity, the coupled magma/mantle flow equations can be formulated as a two-field ...
For a prescribed porosity, the coupled magma/mantle flow equations can be formulated as a two-field ...
Included programs build on the FEniCS and PETSc libraries.Supporting computer code for the paper: Rh...
Abstract. Finite element discretizations of multiphysics problems frequently give rise to block-stru...
We study robust, preconditioned, iterative solution methods for large-scale linear systems of equati...
The finite element (FE) integration of the coupled consolidation equations requires the solution of ...
A high-order discretization consisting of a tensor product of the Fourier collocation and discontinu...
Robust preconditioners on block-triangular and block-factorized form for three types of linear syste...
summary:This paper discusses finite element discretization and preconditioning strategies for the it...
We present a numerical code for the simulation of the dynamics of compressible to incompressible, mu...
The Finite Element modelling of geological faults by penalty contact elements may give rise to illco...
A convection–diffusion model for the averaged flow of a viscous, incompressible magma through an ela...
This article considers the iterative solution of a finite element discretization of the magma dynam...
This article considers the iterative solution of a finite element discretisation of the magma dynami...
This article considers the iterative solution of a finite element discretization of the magma dynami...
For a prescribed porosity, the coupled magma/mantle flow equations can be formulated as a two-field ...
For a prescribed porosity, the coupled magma/mantle flow equations can be formulated as a two-field ...
Included programs build on the FEniCS and PETSc libraries.Supporting computer code for the paper: Rh...
Abstract. Finite element discretizations of multiphysics problems frequently give rise to block-stru...
We study robust, preconditioned, iterative solution methods for large-scale linear systems of equati...
The finite element (FE) integration of the coupled consolidation equations requires the solution of ...
A high-order discretization consisting of a tensor product of the Fourier collocation and discontinu...
Robust preconditioners on block-triangular and block-factorized form for three types of linear syste...
summary:This paper discusses finite element discretization and preconditioning strategies for the it...
We present a numerical code for the simulation of the dynamics of compressible to incompressible, mu...
The Finite Element modelling of geological faults by penalty contact elements may give rise to illco...
A convection–diffusion model for the averaged flow of a viscous, incompressible magma through an ela...