Abstract
We use conformal mapping techniques together with analytic continuation to show that a non-parabolic open elastic inhomogeneity continues to admit a state of uniform internal stress when a hole with closed curvilinear traction-free boundary is placed in its vicinity and the surrounding matrix is subjected to uniform remote anti-plane stresses. The internal uniform stress field inside the inhomogeneity is found to be independent of the existence of the nearby hole and the specific non-parabolic shape of the inhomogeneity. In contrast, the non-parabolic shape of the inhomogeneity is influenced solely by the existence of the nearby hole.
1. Introduction
Eshelby’s uniformity property concerning stresses and strains inside elastic inhomogeneities continues to be an intriguing topic of discussion [1–15]. From a practical point of view, a uniform stress distribution inside an inhomogeneity is optimal in the sense that it eliminates stress peaks within the inhomogeneity, which are well known to be a primary cause of failure [9]. Recently, Wang and Schiavone [16] proved that a non-elliptical elastic inhomogeneity continues to admit an internal uniform stress state despite the presence of a nearby irregularly shaped hole when the matrix is subjected to uniform remote anti-plane shear stresses. In establishing this result the authors assumed that the boundaries of both the inhomogeneity and the hole are closed curvilinear contours. On the other hand, it is of interest to note that Wang and Schiavone [17] have also established (for both plane and anti-plane elasticity) that the internal stresses inside a parabolic elastic inhomogeneity with an open interface are unconditionally uniform when the matrix is subjected to uniform stresses at infinity. In the particular case of anti-plane elasticity, this uniformity property is in agreement with the observation that the flow velocity within a parabolic inclusion is constant under a uniform incident flow [18, 19]. The uniformity of anti-plane stresses inside a non-parabolic open elastic inhomogeneity interacting with a nearby screw dislocation or a circular Eshelby inclusion undergoing uniform anti-plane eigenstrains has also been observed [20, 21].
In this study, we examine the existence of an internal uniform stress field inside an elastic inhomogeneity with an open interface in the presence of a nearby hole with a closed curvilinear traction-free boundary when the surrounding matrix is subjected to uniform anti-plane stresses at infinity. Due to the influence of the adjacent hole, we will refer to the inhomogeneity as ‘non-parabolic’ to indicate a departure from a conventional parabolic inhomogeneity. Our results indicate that through a judicious design of the open shape of the inhomogeneity and the closed shape of the hole, the internal stress field inside the inhomogeneity can still remain uniform. Furthermore, the internal uniform stress field inside the inhomogeneity is independent of the specific open shape of the inhomogeneity and the existence of the nearby hole. The procedure used to design the shapes of the inhomogeneity and the hole is accomplished via the construction of a novel conformal mapping function for the matrix region containing first and second-order poles as well as a Laurent expansion. By satisfying the continuity conditions of traction and displacement across the inhomogeneity–matrix interface and the traction-free condition along the hole boundary, we obtain restrictions on the coefficients in the Laurent series. Satisfying these restrictions on the coefficients is sufficient to arrive at the desired configuration for the composite. In fact, we find that countless configurations for the composite can be generated in this way.
2. Complex variable formulation for anti-plane elasticity
First, we establish a Cartesian coordinate system
where µ is the shear modulus, and the two stress components can be expressed in terms of the stress function as in Ting [6]
Equation (2) is fundamental in describing the boundary value problem in terms of the analytic function
3. Internal uniform stress field
As shown in Figure 1, we consider a domain in

A hole with a closed curvilinear traction-free boundary in the vicinity of a non-parabolic open elastic inhomogeneity with internal uniform stresses when the matrix is subjected to uniform remote anti-plane stresses.
By employing equation (2), the boundary value problem in the z-plane takes the form:
where
To solve the boundary value problem developed above, we introduce the following conformal mapping function for the matrix region:
where R is a real scaling constant;

The problem in the ξ-plane.
To ensure that the stresses inside the non-parabolic open inhomogeneity are uniform, we assume that
where A is a complex constant to be determined.
By enforcing the conditions of continuity of traction and displacement across the perfect inhomogeneity–matrix interface
In writing the expression for
where the mismatch parameter K is defined by
For given values of the coefficients
By using equation (7) to satisfy the prescribed remote asymptotic behaviour of
from which the complex constant A can be uniquely determined quite simply as
Thus, the internal uniform stresses inside the non-parabolic inhomogeneity are explicitly given by
It is clear from the above that the internal uniform stress field inside the inhomogeneity is independent of the existence of the nearby hole and the specific non-parabolic shape of the inhomogeneity. In fact, the uniform stress field in equation (12) is identical to that inside a parabolic inhomogeneity in the absence of the nearby hole [17].
Furthermore, the stresses are non-uniformly distributed in the matrix as follows:
It is easily verified from the above that
4. Numerical results and discussions
In this section, detailed numerical results will be presented to demonstrate the feasibility of the theory proposed in the previous section.
We first illustrate in Figures 3 and 4 the non-parabolic open shape of the elastic inhomogeneity and the irregular closed shape of the hole for different values of

The non-parabolic open shape of the inhomogeneity and the irregular closed shape of the hole for different values of

The non-parabolic open shape of the inhomogeneity and the irregular closed shape of the hole for different values of

The non-parabolic open shape of the inhomogeneity and the irregular closed shape of the hole for different positive values of K with

The non-parabolic open shape of the inhomogeneity and the irregular closed shape of the hole for different negative values of K with

Condition for the mapping in equation (5) to be one-to-one for the matrix region when
We can also conveniently discuss the uniformity of anti-plane stresses inside a non-parabolic open elastic inhomogeneity interacting with a rigid inhomogeneity. In this case, instead of equation (4b) for a traction-free hole, the fixed condition on the boundary of the rigid inhomogeneity is given by
Consequently, to satisfy equation (14), it is sufficient to replace equation (8) by the following relationship:
and the mapping function in equation (5) is still valid. A comparison of equation (8) with equation (15) reveals the fact that the result for the case of a hole can be adapted to that for a rigid inhomogeneity by using the following substitution in equation (8):
An example is illustrated in Figure 8. In this case, the internal uniform stress field is determined from equation (12) as

The non-parabolic open shape of the elastic inhomogeneity and the irregular closed shape of the rigid inhomogeneity when choosing
5. Conclusions
Within the framework of anti-plane elasticity, we have achieved the uniformity of stresses inside a non-parabolic open inhomogeneity in the vicinity of a hole with a closed curvilinear traction-free boundary when the matrix is subjected to uniform stresses at infinity. The non-parabolic open interface
Footnotes
Funding
The authors disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: This work is supported by the National Natural Science Foundation of China (Grant No. 11272121) and through a Discovery Grant from the Natural Sciences and Engineering Research Council of Canada (Grant No: RGPIN – 2017 - 03716115112).
