Let D be a bounded domain in R3 with a closed, smooth, connected boundary S, N be the outer unit normal to S, k>0 be a constant, uN± are the limiting values of the normal derivative of u on S from D, respectively D′:=R3∖ˉD; g(x,y)=eik|x−y|4π|x−y|, w:=w(x,μ):=∫SgN(x,s)μ(s)ds be the double-layer potential, u:=u(x,σ):=∫Sg(x,s)σ(s)ds be the single-layer potential.
In this paper it is proved that for every w there is a unique u, such that w=u in D and vice versa. This result is new, although the potential theory has more than 150 years of history.
Necessary and sufficient conditions are given for the existence of u and the relation w=u in D′, given w in D′, and for the existence of w and the relation w=u in D′, given u in D′.
Citation: Alexander G. Ramm. When does a double-layer potential equal to a single-layer one?[J]. AIMS Mathematics, 2022, 7(10): 19287-19291. doi: 10.3934/math.20221058
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Let D be a bounded domain in R3 with a closed, smooth, connected boundary S, N be the outer unit normal to S, k>0 be a constant, uN± are the limiting values of the normal derivative of u on S from D, respectively D′:=R3∖ˉD; g(x,y)=eik|x−y|4π|x−y|, w:=w(x,μ):=∫SgN(x,s)μ(s)ds be the double-layer potential, u:=u(x,σ):=∫Sg(x,s)σ(s)ds be the single-layer potential.
In this paper it is proved that for every w there is a unique u, such that w=u in D and vice versa. This result is new, although the potential theory has more than 150 years of history.
Necessary and sufficient conditions are given for the existence of u and the relation w=u in D′, given w in D′, and for the existence of w and the relation w=u in D′, given u in D′.
Let D be a bounded domain in R3 with a closed, smooth, connected boundary S, N=Ns be the outer unit normal to S at the point s∈S, k>0 be a constant, g(x,y)=eik|x−y|4π|x−y|, w:=w(x,μ):=∫SgN(x,s)μ(s)ds be the double-layer potential, w± are the limiting values of w on S from D, respectively, from D′, u:=u(x,σ):=∫Sg(x,s)σ(s)ds be the single-layer potential, uN± are the limiting values of the normal derivative of u on S from D, respectively D′:=R3∖ˉD, ˉD is the closure of D, ˉσ, denotes the complex conjugate of σ, H0:=L2(S), H1:=W12(S) is the Sobolev space, μ∈H0. We write iff for if and only if and use the known formulas for the limiting values of the potentials on S, see [3], pp. 148,153:
w±=0.5(A′∓I)μ;uN±=0.5(A±I)σ;w+N=w−N;Q(σ):=∫Sg(t,s)σ(s)ds, | (1.1) |
where A′μ=∫SgNt(t,s)μ(s)ds, Aσ=∫SgNs(t,s)σ(s)ds. In this paper it is proved that for every w in D there is a unique u, such that w=u in D, and vice versa.
Necessary and sufficient conditions are given for w=u in D′ and for u=w in D′.
In [4] the problem for the Laplace's equations was studied in Lipschitz domains. In this case the integral equations, based on potential of double layer, are uniquely solvable for any right-hand side. This is not so, in general, for the corresponding equations for the Helmholtz operator. Our method of proof and the results are new. We assume that the boundary S is smooth and connected. This is done for brevity and simplicity: we do not want to make the presentation more difficult for the reader than it is necessary. Our results and proofs are valid for Lipschitz boundaries. Theorem 1 can be used for looking for the solution of the Dirichlet problem in the form of the single-layer potential.
Let us state these results:
Theorem 1. For every w, defined in D, there is a unique u such that w=u in D, and vice versa.
For every w, defined in D′, there is a unique u such that w=u in D′ iff
∫Sw−pds=0∀p∈N(Q). | (1.2) |
For every u, defined in D′, there is a unique w such that w=u in D′ iff
∫Surds=0∀r∈N(A+I). | (1.3) |
This result is new, although the potential theory has more than 150 years of history.
In Section 2 proofs are given. In Section 3 it is proved that Q:H0→H1 is a Fredholm operator.
a) Assume that w=w(x,μ) is given in D. Let us prove that u=u(x,σ) exists such that u=w in D, and u is uniquely defined by w. First, let us prove the last claim. Suppose u1=w and u2=w in D. Let u1−u2:=u, u=∫Sg(x,s)σds in D, σ=σ1−σ2. Then u|S=0, (∇2+k2)u=0 in D′ and u satisfies the radiation condition, so u=0 in D′. Thus, u=0 in D∪D′, u1=u2, and the claim is proved.
Let us now prove the existence of u such that w=u in D. One has
w+=0.5(A′−I)μ=u|S=Q(σ) | (2.1) |
This is an equation for σ while w+ is given.
Note that Q=Q0+Q1, where Q0σ=∫Sg0(t,s)σ(s)ds, g0(t,s):=14π|t−s|. The operator Q0 is an isomorphism of H0 onto H1, see Lemma 1 in Section 3. Therefore, the operator Q−10 is well defined and maps H1 onto H0.
Consequently, equation (2.1) is equivalent to
w+=(I+Q1Q−10)Q0(σ)=(I+Q1Q−10)η,η:=Q0σ,σ=Q−10η. | (2.2) |
The operator Q1Q−10 is compact in H0, see Section 3. Therefore a necessary and sufficient condition for the solvability of equation (2.2), and the equivalent equation (2.1), is:
∫Sw+ˉηds=0∀η∈N((I+Q1Q−10)⋆), | (2.3) |
where N(B) is the null space of the operator B and B⋆ is the adjoint operator to B in H0, B=I+Q1Q−10, B is of Fredholm type in H0. The kernel g(t,s) of Q, the function g(t,s)=eik|t−s|4π|t−s|, is symmetric: g(t,s)=g(s,t). Therefore, the kernel of Q⋆ is ˉg(t,s). Clearly, (I+Q1Q−10)⋆η=0 iff (I+Q−10ˉQ1)η=0, or, taking the complex conjugate,
(I+Q−10Q1)ˉη=0, | (2.4) |
where we have used the real-valuedness of the kernel of Q0. Applying the operator Q0 to the last equation, one gets an equivalent equation
(Q0+Q1)ˉη=0, | (2.5) |
since Q0 is an isomorphism. Let u=u(x,ˉη). Then u|S=0 according to equation (2.5). Since (∇2+k2)u=0 in D′ and u satisfies the radiation condition, it follows that u=0 in D′ and ˉη=u+N−u−N=u+N. Therefore, using the Green's formula, one obtains:
∫Sw+ˉηds=∫Sw+u+Nds=∫Sw+Nuds=0, |
and, since u=0 on S, it follows that condition (2.3) is always satisfied.
Thus, the necessary and sufficient condition (2.3) for the solvability of equation (2.1) is always satisfied. Therefore, u(x,η)=w(x,μ) in D, Q−10η=σ.
b) Asume now that u is given in D and let us prove the existence of a unique w such that u=w in D. First, we prove that w is uniquely determined by u if u=w in D.
Indeed, assume that there are two wj, j=1,2, such that u=wj in D. Then w:=w1−w2=0 in D. Therefore wN+=0 on S. It is known (see [3], p. 154) that wN+=wN−, so wN−=0. Therefore, (∇2+k2)w=0 in D′, wN−=0 on S, and w satisfies the radiation condition at infinity. This implies w=0 in D′, so w=0 in D∪D′. Therefore μ=w–w+=0, so w1=w2 if u=wj, j=1,2, in D. We have proved that w is uniquely determined by u if u=w in D.
Let us now prove the existence of the solution μ to equation (2.1) and the relation u=w in D.
The operator A′−I is Fredholm in H0, so a necessary and sufficient condition for the equation (2.1) to be solvable is:
∫SQ(σ)ˉhds=0∀h∈N((A′−I)⋆). | (2.6) |
One has (A′−I)⋆h=(ˉA−I)h=0 iff (A−I)ˉh=0.
If (A−I)ˉh=0, then u−N(s,ˉh)=0, so u(s,ˉh)=0 in D′. Note that u(s,ˉh)=Q(ˉh). Therefore, Q(ˉh)=0 in D′. Since Q is a symmetric operator in H0, one has:
∫SQ(σ)ˉhds=∫SσQ(ˉh)ds=0. |
Consequently, condition (2.6) is always satisfied, the solution μ to equation (2.1) exists and u=w in D.
c) Assume that w is given in D′. Let us prove that u exists such that u=w in D′ iff
∫Sw−ˉpds=0∀p∈N(Q⋆). | (2.7) |
Consider the equation for σ:
w−=Q(σ). | (2.8) |
The operator Q:H0→H1 is Fredholm-type. Thus, a necessary and sufficient condition for the solvability of the above equation is equation (2.7). If σ solves (2.8), then u(x,σ)=w in D′ because the value of u on S determines uniquely u in D′.
d) Assume now that u is given in D′. Let us prove that w exists such that u=w in D′ iff
∫Suˉpds=0∀p∈N(ˉA+I). | (2.9) |
Note that p∈N(A+I) iff ˉp∈N(ˉA+I). The equation for μ, given u in D′, is:
0.5(A′+I)μ=u. | (2.10) |
Since the operator A′+I is Fredholm in H0, a necessary and sufficient condition for the solvability of (2.10) for μ is:
∫Suˉpds=0∀p∈N((A′+I)⋆). | (2.11) |
If p∈N((A′+I)⋆), then p∈N(ˉA+I), so condition (2.9) is the same as (2.11). As in section c), the relation u=w in D′ is a consequence of the fact that u=w− on S.
Theorem 1 is proved.
Remark 1. Our proofs remain valid if k=0, that is, for the potentials corresponding to the Laplace equation, rather than the Helmholtz equation.
Recall that H1 is the Sobolev space on S, H0=L2(S).
Lemma 1. The operator Q=Q0+Q1:H0→H1 is of Fredholm-type, where Q0 is the operator with the kernel 14π|t−s| and Q1 has the kernel eik|t−s|−14π|s−t|. The operator Q0 is an isomorhism of H0 onto H1, which has a continuous inverse. The operator Q1Q−10 is compact in H0.
Proof. Let us check that Q0:H0→H1 is an isomorphism. The Fourier transform of the kernel 14π|x−y| is positive: ∫R3eiξ⋅x4π|x|dx=1|ξ|2. So, Q0:H0→H1 is injective. The kernel of the operator Q1 is smooth enough for Q1:H0→H1 to be compact. Let us check that Q0:H0→H1 is surjective. Let f∈H1 and Q0σ=f. Then u:=u(x,σ)=∫Sg(x,s)σds solves the problem: ∇2u=0 in D, u|S=f. By the known elliptic estimates (see, e.g., [1]) one has ‖u‖H3/2(D)≤‖u‖H1(S). Therefore, ∇u∈H1/2(D) and, by the trace theorem, u|S∈H0(S). This proves surjectivity of Q0:H0→H1. Thus, Q0 is an isomorphism of H0 onto H1 which has a continuous inverse. The sum of an isomorphism Q0 and a compact operator Q1 is a Fredholm operator, see, e.g., [2]. The operator Q1Q−10 is compact in H0 because the kernel of Q1 is sufficiently smooth. Although the operator Q1Q−10 is defined on a dense subset H1 of H0, but since this operator is bounded in H0 its closure is a bounded operator in H0. Since the kernel of Q1 is O(|s−t|), the kernel of Q1Q−10 is a continuous function of |s−t| and the surface S is a compact set. Therefore, the operator Q1Q−10 is compact in H0.
Lemma 1 is proved.
It is proved that every double layer potential w in a bounded domain is equal to a single layer potential u in a bounded domain D with a smooth closed connected boundary. Necessary and sufficient conditions are given for w=u in the exterior domain D′.
The authors declare that there are no conflicts of interest.
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