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Gradient discretisation method

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Gradient discretisation method

In numerical mathematics, the gradient discretisation method (GDM) is a framework which contains classical and recent numerical schemes for diffusion problems of various kinds: linear or non-linear, steady-state or time-dependent. The schemes may be conforming or non-conforming, and may rely on very general polygonal or polyhedral meshes (or may even be meshless).

Contents

Some core properties are required to prove the convergence of a GDM. These core properties enable complete proofs of convergence of the GDM for elliptic and parabolic problems, linear or non-linear. For linear problems, stationary or transient, error estimates can be established based on three indicators specific to the GDM (the quantities C D , S D and W D , see below). For non-linear problems, the proofs are based on compactness techniques and do not require any non-physical strong regularity assumption on the solution or the model data. Non-linear models for which such convergence proof of the GDM have been carried out comprise: the Stefan model of a melting material, two-phase flows in porous media, the Richards equation of underground water flow, the fully non-linear Leray—Lions equations.

Any scheme entering the GDM framework is then known to converge on all these problems. This applies in particular to conforming Finite Elements, Raviart—Thomas Mixed Finite Elements, the P 1 non-conforming Finite Elements, and, in the case of more recent schemes, the Hybrid Mixed Mimetic method, the Nodal Mimetic Finite Difference method, some Discrete Duality Finite Volume schemes, and some Multi-Point Flux Approximation schemes.

The example of a linear diffusion problem

Let us consider Poisson's equation in a bounded open domain Ω R d , with homogeneous Dirichlet boundary condition

( 1 ) Δ u ¯ = f ,

where f L 2 ( Ω ) . The usual sense of weak solution to this model is:

( 2 ) Find  u ¯ H 0 1 ( Ω )  such that, for all  v ¯ H 0 1 ( Ω ) , Ω u ¯ ( x ) v ¯ ( x ) d x = Ω f ( x ) v ¯ ( x ) d x .

In a nutshell, the GDM for such a model consists in selecting a finite-dimensional space and two reconstruction operators (one for the functions, one for the gradients) and to substitute these discrete elements in lieu of the continuous elements in (2). More precisely, the GDM starts by defining a Gradient Discretization (GD), which is a triplet D = ( X D , 0 , Π D , D ) , where:

  • the set of discrete unknowns X D , 0 is a finite dimensional real vector space,
  • the function reconstruction Π D   :   X D , 0 L 2 ( Ω ) is a linear mapping that reconstructs, from an element of X D , 0 , a function over Ω ,
  • the gradient reconstruction D   :   X D , 0 L 2 ( Ω ) d is a linear mapping which reconstructs, from an element of X D , 0 , a "gradient" (vector-valued function) over Ω . This gradient reconstruction must be chosen such that D L 2 ( Ω ) d is a norm on X D , 0 .
  • The related Gradient Scheme for the approximation of (2) is given by: find u X D , 0 such that

    ( 3 ) v X D , 0 , Ω D u ( x ) D v ( x ) d x = Ω f ( x ) Π D v ( x ) d x .

    The GDM is then in this case a nonconforming method for the approximation of (2), which includes the nonconforming finite element method. Note that the reciprocal is not true, in the sense that the GDM framework includes methods such that the function D u cannot be computed from the function Π D u .

    The following error estimate, inspired by [Strang,1972], holds

    ( 4 ) u ¯ D u D L 2 ( Ω ) d W D ( u ¯ ) + 2 S D ( u ¯ ) ,

    and

    ( 5 ) u ¯ Π D u D L 2 ( Ω ) C D W D ( u ¯ ) + ( C D + 1 ) S D ( u ¯ ) ,

    defining:

    ( 6 ) C D = max v X D , 0 { 0 } Π D v L 2 ( Ω ) D v L 2 ( Ω ) d ,

    which measures the coercivity (discrete Poincaré constant),

    ( 7 ) φ H 0 1 ( Ω ) , S D ( φ ) = min v X D , 0 ( Π D v φ L 2 ( Ω ) + D v φ L 2 ( Ω ) d ) ,

    which measures the interpolation error,

    ( 8 ) φ H div ( Ω ) , W D ( φ ) = max v X D , 0 { 0 } | Ω ( D v ( x ) φ ( x ) + Π D v ( x ) div φ ( x ) ) d x | D v L 2 ( Ω ) d ,

    which measures the defect of conformity.

    Then the core properties which are sufficient for the convergence of the method are, for a family of GDs, the coercivity, the GD-consistency and the limit-conformity properties, as defined in the next section. These three core properties are sufficient to prove the convergence of the GDM for linear problems. For nonlinear problems (nonlinear diffusion, degenerate parabolic problems...), we add in the next section two other core properties which may be required.

    The core properties allowing for the convergence of a GDM

    Let ( D m ) m N be a family of GDs, defined as above (generally associated with a sequence of regular meshes whose size tends to 0).

    Coercivity

    The sequence ( C D m ) m N (defined by (6)) remains bounded.

    GD-consistency

    For all φ H 0 1 ( Ω ) , lim m S D m ( φ ) = 0 (defined by (7)).

    Limit-conformity

    For all φ H div ( Ω ) , lim m W D m ( φ ) = 0 (defined by (8)).

    Compactness (needed for some nonlinear problems)

    For all sequence ( u m ) m N such that u m X D m , 0 for all m N and ( u m D m ) m N is bounded, then the sequence ( Π D m u m ) m N is relatively compact in L 2 ( Ω ) (this property implies the coercivity property).

    Piecewise constant reconstruction (needed for some nonlinear problems)

    Let D = ( X D , 0 , Π D , D ) be a gradient discretisation as defined above. The operator Π D is a piecewise constant reconstruction if there exists a basis ( e i ) i B of X D , 0 and a family of disjoint subsets ( Ω i ) i B of Ω such that Π D u = i B u i χ Ω i for all u = i B u i e i X D , 0 , where χ Ω i is the characteristic function of Ω i .

    Some non-linear problems with complete convergence proofs of the GDM

    We review some problems for which the GDM can be proved to converge when the above core properties are satisfied.

    Nonlinear stationary diffusion problems

    div ( Λ ( u ¯ ) u ¯ ) = f

    In this case, the GDM converges under the coercivity, GD-consistency, limit-conformity and compactness properties.

    p-Laplace problem for p > 1

    div ( | u ¯ | p 2 u ¯ ) = f

    In this case, the core properties must be written, replacing L 2 ( Ω ) by L p ( Ω ) , H 0 1 ( Ω ) by W 0 1 , p ( Ω ) and H div ( Ω ) by W div p ( Ω ) with 1 p + 1 p = 1 , and the GDM converges only under the coercivity, GD-consistency and limit-conformity properties.

    Linear and nonlinear heat equation

    t u ¯ div ( Λ ( u ¯ ) u ¯ ) = f

    In this case, the GDM converges under the coercivity, GD-consistency (adapted to space-time problems), limit-conformity and compactness (for the nonlinear case) properties.

    Degenerate parabolic problems

    Assume that β and ζ are nondecreasing Lipschitz continuous functions:

    t β ( u ¯ ) Δ ζ ( u ¯ ) = f

    Note that, for this problem, the piecewise constant reconstruction property is needed, in addition to the coercivity, GD-consistency (adapted to space-time problems), limit-conformity and compactness properties.

    Review of some numerical methods which are GDM

    All the methods below satisfy the first four core properties of GDM (coercivity, GD-consistency, limit-conformity, compactness), and in some cases the fifth one (piecewise constant reconstruction).

    Galerkin methods and conforming finite element methods

    Let V h H 0 1 ( Ω ) be spanned by the finite basis ( ψ i ) i I . The Galerkin method in V h is identical to the GDM where one defines

  • X D , 0 = { u = ( u i ) i I } = R I ,
  • Π D u = i I u i ψ i
  • D u = i I u i ψ i .
  • In this case, C D is the constant involved in the continuous Poincaré inequality, and, for all φ H div ( Ω ) , W D ( φ ) = 0 (defined by (8)). Then (4) and (5) are implied by Céa's lemma.

    The "mass-lumped" P 1 finite element case enters the framework of the GDM, replacing Π D u by Π ~ D u = i I u i χ Ω i , where Ω i is a dual cell centred on the vertex indexed by i I . Using mass lumping allows to get the piecewise constant reconstruction property.

    Nonconforming P1 finite element

    On a mesh T which is a conforming set of simplices of R d , the nonconforming P 1 finite elements are defined by the basis ( ψ i ) i I of the functions which are affine in any K T , and whose value at the centre of gravity of one given face of the mesh is 1 and 0 at all the others. Then the method enters the GDM framework with the same definition as in the case of the Galerkin method, except for the fact that ψ i must be understood as the "broken gradient" of ψ i , in the sense that it is the piecewise constant function equal in each simplex to the gradient of the affine function in the simplex.

    Mixed finite element

    The mixed finite element method consists in defining two discrete spaces, one for the approximation of u ¯ and another one for u ¯ . It suffices to use the discrete relations between these approximations to define a GDM. Using the low degree Raviart–Thomas basis functions allows to get the piecewise constant reconstruction property.

    Mimetic finite difference method and nodal mimetic finite difference method

    This family of methods is introduced by [Brezzi et al, 2005] and completed in [Lipnikov et al, 2014]. It allows the approximation of elliptic problems using a large class of polyhedral meshes. The proof that it enters the GDM framework is done in [Droniou et al, 2013].

    References

    Gradient discretisation method Wikipedia


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