Abstract
We deal with the system of equations of linear elastostatics, governing the equilibrium configurations of a linearly elastic body. We recall the basics of the theory of the elastic layer potentials and we extend the trace operators associated with the layer potentials to suitable sets of singular densities. We prove that the trace operators defined, for example, on (with and an open connected set of of class ), satisfy the Fredholm property.
MSC:
74B05; 35Q74; 45B05
1. Introduction
As is well-known [1], the equilibrium configurations of a homogeneous linearly elastic body (see Notation and Functional spaces in Section 2) with no body forces acting on it, satisfy the differential system
where is the elasticity tensor and is the unknown displacement field. Wide efforts have been directed, from a theoretical point of view, to the problem of existence and uniqueness of solutions of system (1) when the displacement, the traction, or a combination of them are prescribed on the boundary (see, e.g., [2,3,4,5]). In all the cited references, the regularity of the boundary values is required, since the problem is formulated within the approach of the variational theory. Nevertheless, in view of possible applications, it is clear that the investigation of the boundary value problems when the data are singular is a notable and engaging issue. Now, since the elasticity tensor is independent on the point, the analysis can be done by means of the elastic layer potentials defined through the fundamental solution (see Section 2). In particular, the proof of the existence and uniqueness of a solution of (1) passes through the possibility to apply the Fredholm alternative to the integral equation translating the boundary value problem which is examined. So, a preliminary step in the analysis of the existence and uniqueness problem is to show that the trace operators involved in the integral equations satisfy the so-called Fredholm property (see Notation and Functional spaces in Section 2). Obviously, this is well-understood when the densities are regular fields on the boundary (see, e.g., [6]). The aim of this paper is to show that the Fredholm property is also met for singular densities. For example, we prove that the trace operator associated with the single layer potential with density in is Fredholmian.
The paper is organized as follows. In Section 2 we recall some classical results about the system of homogeneous elastostatics and some notations on the involved functional spaces. In Section 3 and Section 4 we recall the most important facts about the layer potentials and we prove the Fredholm property for the associated trace operators.
2. Some Classical Results of Homogeneous Elastostatics
We essentially follow the notation in [1]. In particular, we denote by Lin the set of all tensors, i.e., linear applications from to and by Skw⊂Lin the set of all skew tensors. We use bold lower-case letters, like and , for vectors, and bold upper–case letters, like , and for tensors.
Recall that the elasticity tensor , representing the elastic properties of the body, is a linear map from such that
and
is positive definite if
where
and is strongly elliptic if
- •
- From now on we shall assume to be at least strongly elliptic.
A weak solution of (1) (variational solution for ) is a field such that
It is well–known that for strongly elliptic, every weak solution to (1) is analytical in .
Equation (1) admits a fundamental solution [7], i.e., a regular solution for all to
where denotes the Dirac distribution, expressed by
with homogeneous second–order tensor function of degree zero.
If is a bounded domain, then a standard computation assures that every solution of (1) is represented by the Somigliana formula [1]
for all , where
is the traction field on associated with (from now on we denote by the unit normal to exterior [resp. interior] with respect to for bounded [resp. exterior] domain). Starting from (9) and making use of Liouville’s theorem (see, e.g., [8,9]) one proves that if is a solution of (1) in an exterior domain such that , then (9) becomes
for suitable constants and . Hence the following representation follows
with
Clearly, for ,
Let denote by the set of all (infinitesimal) rigid displacements.
If is exterior and , with assigned, (13) implies
Hence, taking into account that by (11) , letting we obtain the work and energy theorem in exterior domains [1]
The following result is due to L. Van Hove [10] (see also [1] p. 105).
Lemma 1.
It holds
for all , where denotes the completion of with respect to .
Relations (13), (14) and Lemma 1 imply the following classical uniqueness results [1]: if is a variational solution of (1), with for exterior, then
and
- •
- From now on uniqueness for the traction problem in bounded domains will be understood in the class of normalized displacement, i.e., the set of fields such that (cf. [1] p. 110)
We will need the following result.
Lemma 2.
If is a variational solution of (1), then
for all bounded domains such that , with c independent of .
Proof.
Notation and Functional spaces—The body is identified with the domain it occupies in a reference configuration. We suppose to be a bounded or exterior domain of class . We denote by o the origin of the reference frame; we suppose [resp. ] for bounded [resp. exterior] domain. For every we set . Unless otherwise specified, in the formulas including integrals, the variable of integration is a point of the region indicated by the integral (, , etc.); we shall omit it when it will be clear from the context. If is exterior, we set , where and, as usual, if and are two functions on , by and we mean that and .
is the Sobolev space of all such that ; is the completion of with respect to and is its dual space. is the trace space of and is its dual space. We set
to denote (say) the value of the functional at . Of course, if is integrable, then . If is of class , since , for and , we have that . Then, in particular, , contains the space of all Borel measures on .
If is a functional space in , we denote by the set of all functions that belong to for every compact set .
Let , be two Banach spaces and denote by , their dual spaces. A linear and continuous map is said to be Fredholmian (or satisfies the Fredholm property) if its range is closed and , where is the adjoint of . A Fredholmian operator satisfies the classical Fredholm alternative and a well–known result of J. Peetre [12] assures that is Fredholmian if there is a compact operator from into a Banach space such that
and .
3. The Trace Operators Associated with the Simple Layer Potential
Every integral at right hand side of (9) is an analytic solution of (1) in . More in general, for every the field
defines an analytical solution of (1) in known as simple layer potential with density . Note that behaves at infinity as the fundamental solution . In particular,
and
It is well–known that for a density
with c independent of , the limit
exists for almost all (by the embedding theorem if , then (20) holds for all ) and axis in a ball tangent (on the side of ) to at and defines the trace of the simple layer potential with density [13]. As a consequence, is continuous in . Moreover, the map
is continuous; accordingly,
for some constant c depending only on and . Let and let be a regular sequence which converges to strongly in . By (22)
Therefore, by well-known results of functional analysis, can be extended to a linear and continuous operator
which is the adjoint of and defines the trace of the simple layer with density :
By (19) it is not difficult to see that
The traction field associated with the simple layer potential (16) with density is defined on both “faces” of by the limit
for almost all (by the embedding theorem if , then (25) holds for all ) and axis in a ball tangent (on the side of ) to at . Moreover,
for some constant c depending only on and , and the classical jump condition holds
We now show that the trace operator is Fredholmian. To this aim we make use of the following well–known results (cf. [11,14,15,16,17,18]).
Lemma 3.
Let Ω be a bounded domain of class . If , , and , then the displacement problem
has a unique solution and
Lemma 4.
Let Ω be a bounded domain of class . If , satisfies
and , then the traction problem
has a unique normalized solution and
The following theorem holds true.
Theorem 1.
Let Ω be a bounded or an exterior domain of class , . The operator is Fredholmian and
Proof.
Let be bounded. By the trace theorem, (20) and classical interior estimates (see Lemma 2) from (27) it follows
where is a ball of radius R centered at o and is a completely continuous map from in a Banach space. Hence by Peetre’s result (see Notation and Functional spaces in Section 2) it follows that has a closed range. If then by (17) an integration by parts gives
Hence by Lemma 1 it follows that in so that by (27) .
Let and let be a regular sequence which converges to strongly in . Of course, from (24) it follows that strongly in . Let be the solution of
Then, integrating by parts we have
Hence letting it follows that
for all so that in .
It is well–known that the system
has a unique solution . Let g be a regular function vanishing outside , equal to 1 in and such that for . Then integrating by parts we have
By Schwarz’s inequality and the properties of g
Likewise,
Hence letting yields
so that in and (27) and the above results imply that .
The proof of the Lemma for exterior follows the same steps so it is omitted. □
4. The Trace Operators Associated with the Double Layer Potential
For every the field
defines analytical solutions of (1) in and is known as double layer potential with density . Note that
The trace on of a double layer potential with density is defined on both “faces” of by the limit
for almost all (by the embedding theorem if , then (40) holds for all ) and axis in a ball tangent (on the side of ) to at . Moreover,
and for bounded
for some constant c depending only on and . The jump condition
holds and the classical Liapounov–Tauber theorem assures that the traction field associated with assumes the same value on both “faces” of
and defines a linear, continuous operator
i.e.,
for some constant c depending only on and . A standard argument shows that and are adjoint each other. Hence, for instance,
is the adjoint of
and defines the trace of a double layer potential with density in :
As we did for the trace operator of the single layer potential we can show that the adjoint operator of
is the trace of the traction field of the double layer potential with density .
As for the operator in the previous section, starting from Lemma 3, 4, we show that the operators , and are Fredholmian.
Theorem 2.
Let Ω be a bounded or an exterior domain of class . The operators , are Fredholmian, and
Proof.
Let be bounded. By Lemmas 3 and 4, the trace theorem and interior estimates
where , are completely continuous maps from in a Banach space and , completely continuous maps from in a Banach space. Therefore, by (42), (43) and (27)
for some completely continuous operators. Hence it follows that and have closed ranges.
If . By the uniqueness theorem in so that . Hence again by uniqueness in so that on . If , with , consider a regular sequence which converges to strongly in and the solution of
for . Integrating by parts and taking into account (17), we have
Hence, letting , it follows that in , so that . On the other hand, by uniqueness in so that . Hence by (27) . The proof of the other properties are quite analogous so it is omitted. □
Theorem 3.
Let Ω be a bounded domain or an exterior domain of class . The operator is Fredholmian and
Proof.
Let be bounded. The trace theorem and interior estimates yield
with completely continuous map from in a Banach space. Therefore, by Peetre’s result, has closed range.
Let . By the uniqueness theorem in and in . Therefore, by (43), it follows that . On the other hand, a direct inspection shows that belongs to .
Let now and consider the sequence strongly converging to in and the solution of
with such that
An integration by parts yields
Hence, letting , it follows that in so that, by (43), . The proof for exterior domains is analogous to the previous one, so it is omitted. □
5. Conclusions
In this article we dealt with some properties related to the trace operators associated with the elastic layer potentials. In particular, we proved that their extensions to some sets of singular densities satisfy the Fredholm property (Theorems 1–3). These results represent an important step in the analysis of the system of linear elastostatics, as they could lead to the existence and uniqueness of solutions to the main boundary value problems with singular data, to which we are going to dedicate our next researches.
Author Contributions
The authors contributed equally to this work. All authors read and approved the final manuscript.
Funding
This research was supported by Programma VALERE - Università degli Studi della Campania “Luigi Vanvitelli”.
Conflicts of Interest
The authors declare no conflict of interest.
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