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
be a variational solution of (
1). If
is bounded, then the work and energy theorem follows [
1]
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 holdsfor 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), thenfor all bounded domains such that , with c independent of . Proof. (
15) is a simple consequence of the classical Caccioppoli’s inequality (see, e.g., [
11])
for all
and
, with
c independent of
, taking into account that any derivative of
is a solution of (
1) and making use of Sobolev’s lemma. □
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 problemhas a unique solution and Lemma 4. Let Ω
be a bounded domain of class . If , satisfiesand , then the traction problemhas 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
gTherefore, taking into account Hardy’s inequality
for all
, we can let
in (
36) to have
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. □