Mathematical Foundations for the Boundary- Field Equation Methods in Acoustic and Electromagnetic Scattering

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Mathematical Foundations for the Boundary- Field Equation Methods in Acoustic and Electromagnetic Scattering George C. Hsiao Abstract The essence of the boundary-field equation method is the reduction of the boundary value problem under consideration to an equivalent nonlocal boundary value problem in a bounded domain by using boundary integral equations. The latter can then be treated by the standard variational method including its numerical approximations. In this paper, various formulations of the nonlocal boundary value problems will be given for the Helmholtz equation as well as for the time- harmonic Maxwell equations. Emphasis will be placed upon the variational formulation for the method and mathematical foundations for the solution procedure. Some numerical experiments are included for a model problem in electromagnetic scattering. 1 Introduction basic concepts The idea of combining the boundary integral equation method with other techniques had already been introduced in a paper by Greenspan and Werner [6] in the study of an exterior Dirichlet problem for the Helmholtz equation in 2-D. Specially, they employed a combined boundary integral equation and the finite difference methods in a bounded domain in order to obtain sufficiently accurate approximate solutions at points near the boundary. Alternatively, one may also consider combining the boundary integral equation method with other methods such as the finite element method as in the paper by MacCamy and Marin [11] for exterior interface problems. In general we refer to a variational method for treating boundary value problems for partial differential equations in a bounded domain together with some nonlocal boundary conditions in the form of boundary integral equations as the boundary-field equation method (see, e.g., the monograph by Gatica and Hsiao [5]). For the exterior boundary value problem (BVP), the general solution procedure for the method is shown in Figure 1. Of course for the scattering problem we may Department of Mathematical Sciences, University of Delaware, Newark, Delaware 19716. 1

start directly with the transmission problem. In this paper we will confine to the steps concerning the various nonlocal BVPs and their corresponding weak formulations in acoustics as well as in electromagnetics. BVP Transmission Prob. Nonlocal BVP Weak Formulation Numerical Implementation & Error Analysis Figure 1: A flow chart for the general solution procedure. As will be seen, for the transmission problem, the nonlocal boundary condition will be derived from boundary integral equation methods and it will give the relation among the Cauchy data of the solution on the interface boundary. It is important to point out that in general the process of the reduction from a BVP to boundary integral equation formulations is not unique; hence one may arrive at various different forms of nonlocal boundary value problems. However, in all the cases, one tries to obtain an equivalent nonlocal boundary value problem whose weak formulation will provide a bilinear form to satisfy a Gårding inequality in appropriate function space. In fact, the Gårding inequality is one of the main mathematical ingredients for the variational methods. It is well known that Gårding s inequality implies the validity of the Fredholm alternatives for the variational equations under consideration. If in addition the finite-dimensional approximate subspaces approximate the solution space in the energy norm, then the Babǔska-Brezzi-Ladzenskaya condition (the so-called BBL-condition) follows also from Gårding s inequality together with the uniqueness of the solution (see, e.g., [13]). This BBL-condition is a crucial stability condition for the Galerkin method. As a consequence, one has the celebrated Ceá s lemma which implies that the Galerkin solution is the best approximation for the variational solution in the energy norm. In fact, from Ceá s lemma, one reduces the problem of error estimates to a problem in approximation theory. Together with approximation and inverse properties of the corresponding finite dimensional approximate function space, qusioptimal error estimates for the Galerkin solution can be established by using standard arguments in functional analysis (see, e.g., [15]). 2

2 Acoustic Scattering Through out the paper, let Ω be a bounded domain in IR 3 with smooth boundary Γ. We consider the exterior BVP for the Helmholtz equation u + k 2 u = 0 in Ω c := IR 3 \ Ω, u = 0 on Γ, (1) u s r ikus = o(r 1 ) as r = x, (2) where u = u s + u i denotes the total field, u s the unknown scattered field, and u i the given incident field. For simplicity, we assume that the wave number k is a constant and that Im k 0 in order to avoid resonance states. The Dirichlet problem (1), (2) is one of the basic problems in classical scattering theory. It represents the scattering of time-harmonic acoustic waves by a bounded impenetrable obstacle Ω and the homogeneous Dirichlet boundary condition in (1) corresponds to a soundsoft obstacle. The Sommerfeld radiation condition (2) guarantees the scattered wave u s is outgoing and will ensure uniqueness for the solutions to the scattering problem. We now reformulate the BVP as a transmission problem. We divide the domain Ω c into two subdomains Ω F and Ω B = Ω c \ Ω F by introducing an artificial common boundary so that Ω is completely contained in. Then (1), (2) may be reformulated as a transmission problem u + k 2 u = 0 in Ω F ; u = 0 on Γ, (3) u = u s+ + u i, u n = us+ n + ui n on, (4) u s + k 2 u s = 0 in Ω B u s r ikus = o(r 1 ) as r = x. (5) In the formulation, it is understood that the given incident field u i is required also to satisfy the Helmholtz equation in Ω B. Here and in the sequel, we have adapted the notation v and v + for the limits of v on from Ω F and Ω B, respectively, and / n for the normal derivative with respect to the unit outward normal n to. To reduce the transmission problem (3),(4),(5) to a nonlocal boundary value problem, we begin with the Green representation for u s in Ω B, u s (x) = u s (y) + γ(x, y)ds y u s (y) + γ(x, y)ds y, x Ω B, (6) n y n y where γ(x, y) := e ik x y /4π x y, is the fundamental solution for the Helmholtz equation. In the representation, the functions u s (y) + and n y u s (y) + are unknown 3

on the interface. These are the Cauchy data of the solution u s to the Helmholtz equation in Ω B and they are related by the two boundary integral equations (BIEs) 1 us+ u s+ = 2 I + K V n W 1 2 I K us+ u s+ on. (7) n Here V, K, K, W are the four basic boundary integral operators defined by V σ(x) := γ(x, y)σ(y)ds y, Kµ(x) := µ(y)γ(x, y)ds y, n y K σ(x) := σ(y)γ(x, y)ds y, W µ(x) := µ(y)γ(x, y)ds y, n x n x n y while the matrix of boundary integral operators ( 1 C ΩB := I + K V ) 2 W 1I K 2 is referred to as the Calderon projector which maps the Cauchy data into itself. We note that the solution u s in the exterior domain Ω B is completely determined from the representation (6), provided one knows its Cauchy data on the interface. This leads us to the consideration of various nonlocal boundary value problems which all will reduce the transmission problem (3),(4),(5) to an equivalent problem in the bounded domain Ω F. If we denote σ = u s+ / n, and use the first BIE in (7), we arrive at the simplest nonlocal boundary value problem: Find (u, σ) such that u + k 2 u = 0 Ω F ; u = 0 on Γ, (8) u n = σ + ui n on, (9) V σ + ( 1 2 I K)(u u i ) = 0 on. (10) The boundary condition (10) is nonlocal in the sense that to find σ at a single point on, one needs the values of u at every point on. In some sense (10) serves as a boundary integral equation of the first kind for the unknown σ by considering u as well as u i as the given data. We note that if σ is given on, then (8) and (9) will be sufficient for determining u in Ω F. Alternatively, we may use both BIEs in (7) to formulate the nonlocal boundary value problem. More precisely, one may replace (9) by u n = W (u u i ) + ( 1 2 I K )σ + ui on. (9a) n 4

Then the problem consisting of (8),(9a),(10) is an another version of nonlocal boundary value problem for (u, σ). This is the symmetric version as can be seen from its variational formulation [4], and it does not depend on the compactness of the operator K as in the one BIE formulation, (8),(9),(10). For the variational formulation, we need the energy spaces: H 1 Γ(Ω F ) := {v H 1 (Ω F ) : v Γ = 0}, H 1 2 (Γ0 ) = dual of H 1 2 (Γ0 ). Now the variational formulation for the nonolocal boundary value problem (8),(9),(10) reads: Find (u, σ) H 1 Γ (Ω F ) H 1 2 ( ) such that a(u, v) < σ, v >=< ui n, v >, (11) < χ, V σ > + < χ, ( 1 2 I K)u >=< χ, ( 1 2 I K)ui > (12) for all (v, χ) HΓ 1(Ω F ) H 1 2 ( ), where a(u, v) := { u v k 2 uv}dx, Ω F and <, > denotes the duality pairing between H 1/2 ( ) and H 1/2 ( ). For the problem (8),(9a),(10), the variational equational (11) will be replaced by a(u, v)+ < W u ( 1 2 I K )σ, v >=< ui n + W ui, v >, because of (9a), but (12) remains unchanged. The following results can now be established (see, e.g. [7]). (11a) Theorem 2.1 The sesquilinear form A k (, ), k = 1, 2, from the variational problems (11),(12), and (11a), (12) defined by A 1 ((u, σ), (v, χ)) := a(u, σ) < σ, v > +2{< χ, V σ > + < χ, ( 1 2 I K)u >}, A 2 ((u, σ), (v, χ)) := a(u, σ)+ < W u, v > < ( 1 2 I K )σ, v > + < χ, V σ > + < χ, ( 1 2 I K)u > respectively, satisfies a Gårding inequality in the form: ReA k ((v, χ), (v, χ)) α k (v, χ) 2 E C k ((v, χ), (v, χ)) for all (v, χ) E, where α k > 0 is a constant, C k is a compact form on E := H 1 Γ (Ω F ) H 1 2 ( ), and (v, χ) 2 E := v 2 H 1 Γ (Ω F ) + χ 2 H 1 2 ( ). 5

3 Electromagnetic Scattering We now consider the scattering of time-harmonic electromagnetic waves by an obstacle surrounded by a homogeneous medium with constant electric permittivity ɛ and magnetic permeability µ. This leads us to the exterior BVP for the reduced Maxwell equations: E = iωµh; H = iωɛe in Ω c := IR 3 \ Ω, (13) n E = 0 on Γ, (14) lim ( µ H s x x x ɛ E s ) = 0, (15) E = E s + E i ; H = H s + H i. (16) In the formulation, E and H are, respectively, the electric and magnetic fields of the total electromagnetic wave with frequency ω > 0. We assume again that Im k 0, where the wave number k is a constant given by k 2 = ɛµω 2. The boundary condition (14) simply implies that we have a perfectly conducting obstacle Ω, where n is the unit outward normal to the boundary Γ. The Silver-Müller radiation condition (15) is the counterpart of the Sommerfeld radiation condition (2) for elctromagnetic waves. Let be the artificial boundary as in the acoustic scattering. In the same manner, we may convert the BVP (13)-(16) to a transmission problem of the form, E = iωµ; H = iωɛe in Ω F, (17) n E = 0 on Γ, (18) n E = n E s + n E i ; H n = H s n + H i n on, (19) E s = iωµh s ; H s = iωɛe s in Ω B, (20) lim ( µ H s x x x ɛ E s ) = 0. (21) Now in order to reduce the transmission (17)-(21) to a nonlocal boundary value problem, we begin with the well known Stratton-Chu formulas for E s and H s in [14], E s (x) = iωµ γ(x, y)(h s n)ds y + (n E s ) y γ(x, y)ds y y γ(x, y) (n E s )ds y, x Ω B, H s (x) = iωɛ γ(x, y)(n E s ) + (n H s ) y γ(x, y)ds y + y γ(x, y) (H s n)ds y, x Ω B, where γ(x, y) is again the fundamental solution for the Helmholtz equation (see (6)). In some way, the Stratton-Chu formulas are misleading from the mathematical point 6

of view. We see that the representation formulas require more Cauchy data on interface than those appeared in (19). This is due to the fact that the formulas were derived by using only the fundamental solution of the Helmholtz equation. In fact, from the Maxwell equations, one can easily show that the additional boundary data can be eliminated (see, e.g., [8]), and we will obtain a modified version of the Stratton-Chu formulas for E s and H s, E s (x) = iωµ {γ(x, y) 1 k yγ(x, y)div 2 Γ0 }(H s n)ds y (22) y γ(x, y) (n E s )ds y, x Ω B, H s (x) = iωɛ {γ(x, y) 1 k yγ(x, y)div 2 Γ0 }(n E s )ds y (23) + y γ(x, y) (H s n)ds y, x Ω B. Here H s n and n E s are the appropriate Cauchy data. They are related by the BIEs n E s 1 I R iωµt n E s 2 = on, (24) H s 1 n iωɛt I R H s n, 2 where the boundary integral operators are defined by T (ϕ)(x) := n {γ(x, y) 1 k yγ(x, y)div 2 Γ0 }ϕ(y)ds y, R(ϕ)(x) := n y γ(x, y) ϕ(y)ds y. In an analogue to (7), the Calderon projector defined by (24) maps the Cauchy data j := H s n, m := n E s into itself. These are the electric current of density j, and the magnetic current of density m. We refer to the first and the second BIEs in (24) as the EFIE and MFIE respectively, since from these equations, we may recover the conventional electric and magnetic field integral equations, if Ω F is a perfect conductor. We may now formulate the nonlocal BVP by using the BIEs from (24). For one BIE formulation based on the EFIE, we have the formulation: Find (E, H, j) such that E = iωµh; H = iωɛe in Ω F, (25) n E = 0 on Γ, (26) H n = j + H i n on, (27) 7

iωµt j ( 1 2 I + R)(n E n Ei ) = 0 on. (28) We remark that in principle one may also replace the nonlocal boundary condition (28) by using the MFIE (see Section 4 ). Moreover, we may apply the to the Maxwell equations in order to eliminate one of the unknowns. This leads to the formulation: Find (E, j) such that E k 2 E = 0 in Ω F, (25a) n E = 0 on Γ, (26) (1/iωµ) n ( E) = (j + H i n) on (27a) together with (28), where in (27a), j is replaced by j = ( 1 2 I R)j + iωɛt (n E n Ei ) on. (27b) We note that (27a) is the same as (27) in view of (25) and that (27b) is the MFIE in (24). This formulation based on the second order partial differential equation (25a) together with (26), (27a) with (27b), and (28) is in some sense closest to the formulations for the elliptic BVPs as in the acoustic scattering. It has been analysesed recently by Ammari and Nédélec in [1]. In the following, we will confine ourselves to the variational formulation for this nonlocal boundary value problem. We remark that one may also replace (25) by (25a) in the previous formulation which will be resemble to the one BIE formulation in the acoustic scattering. To consider the variational formulation for the two BIE nonlocal boundary value problem, we need the appropriate Sobolev spaces. In fact, as well be seen, in contrast to the acoustic case, the mathematical analysis here is not so transparent. To motive our observation, let us begin with the weak form of (25a) subject to the conditions (26) and (27a), b(e, Γ Ẽ) iω j Ẽds = iω (H i n) Ẽds, (29) 0 where b(e, Ẽ) is the sesqulinear form associated with (25a) defined by b(e, Ẽ) := 1 ( E) ( Ẽ)dx ω2 ɛ E Ẽdx. (30) Ω F µ Ω F The latter suggests that the proper solution space for E (also the test function space for Ẽ) should be a subspace of H(curl, Ω F ) := {v (L 2 (Ω F )) 3 : v (L 2 (Ω F )) 3 }, that is, H 0 (curl, Ω F ) := {v H(curl, Ω F ) : n v Γ = 0}. 8

Then from (29), we see that if the magnetic field H is also in H(curl, Ω F ), then j must be in the trace space, H 1/2 div ( ) := {v T H 1/2 ( ) : div Γ0 v H 1/2 ( )}. The latter can be naturally identified with the dual of the trace space H 1/2 curl ( ) := {v T H 1/2 ( ) : curl v H 1/2 ( )}. Here we denote the tangential space by T H s ( ) := {v (H s ( )) 3 : v n Γ0 = 0}. We denote by Γ0 the surface gradient, and define div Γ0 := Γ0, curl Γ0 := n Γ0, and curlγ 0 := the transpose of curl Γ0. We now have the variational formulation for the nonlocal BVP consisting of (25a),(26),(27a),(27b) and (28): Find (E, j) H 0 (curl, Ω F ) H 1/2 div ( ) satisfying b(e, Γ Ẽ) iω j Ẽds = iω (H inc n) Ẽds, and (31) 0 iωµ T j jds ( 1 2 I R)(n E) jds = ( 1 2 I R)(n Ei ) jds (32) for all (Ẽ, j) H 0 (curl, Ω F ) H 1/2 div ( ), where in (31) j := ( 1 2 I R)j + iωɛt (n E n Einc ). (33) We note that in the above variational formulation, the sesqulinear form (30) contains the L 2 -term. However, in contrast to the case for the Helmholtz equation, it is known that the embedding from H(curl, Ω F ) to L 2 (Ω F ) is not compact. This means that we are not able to establish a Gårding inequality on the energy space H 0 (curl, Ω F ) H 1/2 div ( ) directly without any modifications. To overcome this difficulty, we need the following result for the decomposition of function spaces which is known as the Helmholtz or Hodge decomposition [3],[10]. Lemma 3.1 (1) Let M(Ω F ) and P (Ω F ) be the spaces defined by M(Ω F ) := {v H 0 (curl, Ω F ) : ɛ v q = 0, q P (Ω F )}, Ω F P (Ω F ) := {p H 1 (Ω F ) : p Γ = 0}. Then the decomposition and H 0 (curl, Ω F ) = M(Ω F ) P (Ω F ) is orthogonal with respect to the inner product ((u, v)) := u v + Ω F ɛ u v. Ω F 9

(2) The decomposition H 1/2 div ( ) = Γ0 H 3/2 ( )/C curl Γ0 H 1/2 ( )/C is orthogonal with respect to the duality product between T H 1/2 ( ) and T H 1/2 ( ). We note that the integral condition in the space M(Ω F ) is equivalent to require that div(ɛv) = 0 in Ω F and that v n = 0 on. Hence the embedding from M(Ω F ) to L 2 (Ω F ) is compact. With the Hodge decomposition available, we are now in a position to discuss the Gårding inequality. The following theorem has been recently established in [1]. Theorem 3.2 In the variational formulation for (31),(32),(33), let E = u + p, u M(Ω F ), p P (Ω), j = Γ0 ϕ + curl Γ0 ψ H 1/2 dvi ( ) and denote the corresponding sesquiliear form by A((u, p, ϕ, ψ), (v, q, σ, λ)), where (v, q, σ, λ) are the test functions in H := M(Ω F ) P (Ω F ) H 3/2 ( )/C H 1/2 ( )/C. Then A satisfies the Gårding inequality: ReA((v, q, σ, λ), ((v, q, σ, λ)) α (v, q, σ, λ) 2 H C((v, q, σ, λ), (v, q, σ, λ)) for all (v, q, σ, λ) H, where C is compact on H. Here the norm H is defined by (v, q, σ, λ) 2 H := v 2 M(Ω F ) + q 2 P (Ω F ) + σ 2 H 3/2 ( )/C + λ 2 H 1/2 ( )/C. 4 Some computational results To conclude the paper, we present here some preliminary numerical results for a model problem in electromagnetic scattering by using a boundary-field equation method consisting of the Maxwell equations in the computational domain and one boundary integral equation, the MFIE on the artificial boundary. We consider the electric scattering by a perfect conductor occupying a unit ball {(x, y, z) : x 2 + y 2 + z 2 1}. The incident wave propagates in the positive direction of z-axis ɛ E i (x, y, z) = µ eikzˆx, H i (x, y, z) = e ikz ŷ, 10

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