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1.2 Boundary Potentials and Calder´on’s Projector  3

                                                                               c
                           Here v p denotes a particular solution of (1.1.1) in Ω or Ω and f has been
                                                                 n
                                                 c
                           extended from Ω (or Ω ) to the entire R . Moreover, for the extended f
                                                                                            c
                           we assume that the integral defined in (1.1.5) exists for all x ∈ Ω (or Ω ).
                           Clearly, with this particular solution, the boundary conditions for u are to
                           be modified accordingly.
                              Now, without loss of generality, we restrict our considerations to the so-
                           lution u of the Laplacian (1.1.6) which now can be represented in the form:
                                                        ∂u             ∂E(x, y)

                                       u(x)=     E(x, y)  (y) −    u(y)       ds y .    (1.1.7)
                                                        ∂n               ∂n y
                                             y∈Γ               y∈Γ
                              For given boundary data u| Γ and  ∂u  |
                                                            ∂n Γ , the representation formula (1.1.7)
                           defines the solution of (1.1.6) everywhere in Ω. Therefore, the pair of bound-
                           ary functions belonging to a solution u of (1.1.6) is called the Cauchy data,
                           namely

                                                                    u| Γ
                                                Cauchy data of u :=      .              (1.1.8)
                                                                   ∂u
                                                                     |
                                                                   ∂n Γ
                           In solid mechanics, the representation formula (1.1.7) can also be derived
                           by the principle of virtual work in terms of the so–called weighted resid-
                           ual formulation. The Laplacian (1.1.6) corresponds to the equation of the
                           equilibrium state of the membrane without external body forces and vertical
                           displacement u. Then, for fixed x ∈ Ω, the terms

                                                              ∂E(x, y)
                                                u(x)+     u(y)        ds y
                                                                ∂n y
                                                      y∈Γ
                           correspond to the virtual work of the point force at x and of the resulting
                           boundary forces ∂E(x, y)/∂n y against the displacement field u, which are
                           equal to the virtual work of the resulting boundary forces  ∂u  |
                                                                             ∂n Γ acting against
                           the displacement E(x, y), i.e.

                                                             ∂u
                                                       E(x, y)  (y)ds y .
                                                             ∂n
                                                   y∈Γ
                           This equality is known as Betti’s principle (see e.g. Ciarlet [42], Fichera [75]
                           and Hartmann [121, p. 159]). Corresponding formulas can also be obtained
                           for more general elliptic partial differential equations than (1.1.6), as will be
                           discussed in Chapter 2.


                           1.2 Boundary Potentials and Calder´on’s Projector

                           The representation formula (1.1.7) contains two boundary potentials, the
                           simple layer potential
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