Abstract

Integral representations for the solution of linear elliptic partial differential equations (PDEs) can be obtained using Green's theorem. However, these representations involve both the Dirichlet and the Neumann values on the boundary, and for a well-posed boundary-value problem (BVPs) one of these functions is unknown. A new transform method for solving BVPs for linear and integrable nonlinear PDEs usually referred to as the unified transform (or the Fokas transform) was introduced by the second author in the late Nineties. For linear elliptic PDEs, this method can be considered as the analogue of Green's function approach but now it is formulated in the complex Fourier plane instead of the physical plane. It employs two global relations also formulated in the Fourier plane which couple the Dirichlet and the Neumann boundary values. These relations can be used to characterize the unknown boundary values in terms of the given boundary data, yielding an elegant approach for determining the Dirichlet to Neumann map. The numerical implementation of the unified transform can be considered as the counterpart in the Fourier plane of the well-known boundary integral method which is formulated in the physical plane. For this implementation, one must choose (i) a suitable basis for expanding the unknown functions and (ii) an appropriate set of complex values, which we refer to as collocation points, at which to evaluate the global relations. Here, by employing a variety of examples we present simple guidelines of how the above choices can be made. Furthermore, we provide concrete rules for choosing the collocation points so that the condition number of the matrix of the associated linear system remains low.

Highlights

  • A new method for analysing boundary-value problems (BVP) for linear and for integrable nonlinear partial differential equations (PDEs) was introduced by the second author in the late Nineties [1,2,3]

  • These integral formulae provide the analogue of the classical Green’s representations, but the formulation takes place in the complex Fourier plane instead of the physical plane. (ii) The above transforms of the Dirichlet and of the Neumann boundary values are related via two simple algebraic equations called global relations. These relations provide a characterization of the generalized Dirichlet to Neumann map. (iii) By employing the integral representation and global relations mentioned in (i) and (ii), respectively, it has been possible to obtain exact solutions for a variety of problems for which apparently the usual approaches fail, see e.g. [4,5]. (iv) Ashton [6,7] has developed a rigorous approach for deriving well posedness results for linear elliptic PDEs using the new formalism. This includes the analysis of BVPs with distributional data and with corner singularities [8]. (v) The new method can be applied to linear PDEs with nonlinear boundary conditions, see e.g. [9,10,11]. (vi) The first steps have been taken towards extending the unified transform to three dimensions, see e.g. [9,12]

  • This paper is organized as follows: in §2, we review the concept of global relations and obtain these relations for the Laplace, modified Helmholtz and Helmholtz equations in the interior of a polygonal domain

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Summary

Introduction

A new method for analysing boundary-value problems (BVP) for linear and for integrable nonlinear partial differential equations (PDEs) was introduced by the second author in the late Nineties [1,2,3]. This method, which is usually referred to as the unified transform (or the Fokas transform), has been applied to a variety of linear elliptic PDEs formulated in the interior of a polygon Important results in this direction include the following: (i) for the Laplace, modified Helmholtz and Helmholtz equations, it is possible to express the solution in terms of integrals in the complex λ-plane (complex Fourier plane). These integrals contain certain integral transforms of the Dirichlet and of the Neumann values on the boundary of the polygon.

Global relations
The approximate global relation
Collocation points
Numerical results
Conclusion
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