Abstract
The analysis of plane stress problems has long been a topic of interest in linear elasticity. The corresponding problem for non-linearly elastic materials is considered here within the context of homogeneous incompressible isotropic elasticity. It is shown that when the problem is posed in terms of the Cauchy stress, a semi-inverse approach must be employed to obtain the displacement of a typical particle. If however the general plane stress problem is formulated in terms of the Piola-Kirchhoff stress, the deformation of a particle requires the solution of a non-linear partial differential equation for both simple tension and simple shear, the trivial solution of which yields a homogeneous deformation. It is also shown that the general plane stress problem can be solved for the special case of the neo-Hookean material.
Similar content being viewed by others
Explore related subjects
Find the latest articles, discoveries, and news in related topics.Avoid common mistakes on your manuscript.
1 Motivation
Classical non-linear incompressible homogeneous isotropic hyperelasticity as formulated by Rivlin (see, for example Rivlin [1]) assumes that the Cauchy stress \(\boldsymbol{T}\) can be determined as a function of the left Cauchy-Green deformation tensor \(\boldsymbol{B}\) so that
where, using the so-called semi-inverse approach, \(\boldsymbol{B}\) is determined from a given displacement field. This is precisely what is needed if accurate and reliable predictions of the stress in a deformed body are needed as displacement, but not stress, can be measured experimentally. There is the dual problem however, that has been largely ignored in the literature, of inverting (1.1) to determine \(\boldsymbol{B}\) from a known stress distribution, with the expectation that this might be most useful in experiments where the stress can be assumed to be homogeneous and is specified on the boundary of the deformed body. There are two significant impediments to a satisfactory solution to this dual problem: first, the stress-strain relation (1.1) is not in general invertible. Secondly, even if invertibility can be achieved, the existence and uniqueness of a regular deformation generating a pre-assigned left strain-tensor field \(\boldsymbol{B}\) is an open problem (Blume [2]). Blume [2] has shown, however, that if a regular deformation results in a constant \(\boldsymbol{B}\), then the deformation is homogeneous. This is obviously a very useful result when determining the existence of a deformation if a given Cauchy stress is assumed homogeneous.
Batra’s ostensibly simple theorem (Batra [3]) yields insight into this inverse problem for perhaps the simplest problem that can be posed in this context, i.e., what can be deduced about the nature of the deformation for simple tension if the Cauchy stress \(\boldsymbol{T}\) has the form
where \(T\) is a positive constant? Here the standard notation is used to denote unit vectors for a Cartesian co-ordinate system in the deformed configuration. Batra showed that, if the Empirical Inequalities hold, the left Cauchy-Green tensor \(\boldsymbol{B}\) must have the form
for the incompressible materials of interest here. The issue of determining a corresponding deformation was not considered by Batra. Trivially one such homogeneous deformation, and the deformation must be homogeneous (Blume [2]), has the form
denoting the Cartesian coordinates of a typical particle before and after deformation by \((X,Y,Z)\) and \((x,y,z)\) respectively, thus resolving the issue of existence. However the issue of uniqueness remains unresolved, even in this, the simplest of problems.
The corresponding problem for simple shear was first considered by Moon and Truesdell [4] who investigated the consequences of assuming a Cauchy stress of the form
This study and subsequent work by, amongst others, Mihai and Goriely [5], Destrade et al. [6] and Thiel et al. [7] shows that the left Cauchy-Green deformation tensor for incompressible materials must have the form
Again, as for simple tension, the deformation field cannot be derived from knowledge of \(\boldsymbol{B}\) but rather it can be simply shown that (1.6) is compatible with a simple shear superposed on a triaxial stretch so that, for example,
with the uniqueness issue again remaining unresolved.
It should be pointed out that the general issue of constitutive modeling for hyperelastic materials using the inverse approach of considering \(\boldsymbol{B}=\boldsymbol{g}(\boldsymbol{T})\) has been the subject of several studies in the literature (see, e.g., [8, 9] and references cited therein). The point of view proposed in these works is that such an approach is more realistic physically since one expects deformation to be the result of applied forces rather than the converse. The results to be presented below may be viewed as specific explicit illustrations of this new approach in the context of plane stress. In addition to this issue for the Cauchy stress, we also consider its counterpart for the first Piola-Kirchhoff stress. See also [10] for a recent treatment of simple shear resulting from applied Piola-Kirchhoff stress.
There is a rich tradition of exploring the consequences of assuming plane stress conditions in linear elasticity (see, for example, Timoshenko and Goodier [11]). However the corresponding problem for nonlinear elasticity is rarely considered, complicated as it is by the two difficulties mentioned previously for general dual problems. This is the main concern in this paper. If the plane stress problem is formulated in terms of the Cauchy stress, then
using an obvious notation for the Cartesian components of the stress tensor. It will also be assumed that the remaining in-plane stresses are homogeneous so that the equations of equilibrium are satisfied identically. Trivially then the dual problem for plane stress includes the dual problems of simple tension considered by Batra [3] and simple shear considered by Moon and Truesdell [4] and their approach based on the classical constitutive law of expressing the Cauchy stress in terms of the left Cauchy-Green tensor and its invariants will first be adopted, where the problems of invertibility and existence become immediately apparent. This is described in Sect. 2.
The problem of compatibility is significantly reduced however by assuming plane stress conditions in terms of the Piola-Kirchhoff stress \(\boldsymbol{P}\), so that
It is shown in Sects. 3 and 4 that the corresponding deformation field must be a plane deformation accompanied by a constant out-of-plane stretch for all incompressible isotropic hyperelastic materials for which the Empirical Inequalities hold. These results are made more explicit for the case of simple shear in Sect. 5. It is shown that the deformation for simple shear requires the solution of a non-linear partial differential equation, a particular solution of which yields a homogeneous deformation. In Sect. 6, it is shown that the general plane stress problem can be solved explicitly for the neo-Hookean material. The problem of simple tension is considered in Sect. 7. It is shown that in addition to the non-linear partial differential equation required for simple shear, the deformation also must satisfy Laplace’s equation. A particular solution involving a homogeneous deformation is obtained.
2 Plane Cauchy Stress Problems
The mechanical response of a homogeneous isotropic incompressible hyperelastic solid for which \(I_{3}=\text{det}\, \boldsymbol{B}=\text{det}\, \boldsymbol{C}\equiv 1\) is completely determined by specification of the strain energy per unit undeformed volume \(W=W(I_{1},I_{2})\) where
Here \(\boldsymbol{B}\equiv \boldsymbol{FF}^{T}\), \(\boldsymbol{C}\equiv \boldsymbol{F}^{T}\boldsymbol{F}\) are the left and right deformation tensors respectively and \(\boldsymbol{F}\) is the deformation gradient tensor. The constitutive law in terms of the Cauchy stress is given by
where \(p\) is an arbitrary scalar field. The Empirical Inequalities
will be assumed to hold throughout. The universal relation
follows immediately from (2.2). For the Cauchy plane stress conditions (1.8) this universal relation yields
and
The first of these has an immediate interpretation in terms of simple shear. For example, Rivlin’s formulation of plane stress simple shear (Rivlin [1]) specifies \(B_{xx}=1+K^{2}\), \(B_{yy}=1\), \(B_{xy}=K\), where \(K\) is the amount of shear. Equation (2.5) then yields the classical universal relation
Murphy et al. [12] observed that an inverted form of Rivlin’s universal relation (2.7) can be obtained by assuming a stress boundary problem for which \(T_{xy}\ne 0\) so that
This result also follows directly from (2.5).
Now consider the second set of universal relations (2.6). It follows that there are two categories of plane stress boundary value problems. The first is the set of problems for which
exemplified by simple shear for which \(T_{xx}=T_{yy}=0\), \(T_{xy}=T\ne 0\). The second category is the set which satisfy the singular condition
exemplified by simple tension for which \(T_{xx}=T\ne 0\), \(T_{yy}=T_{xy}=0\). Counterintuitively then, simple shear could therefore be considered to be a more regular stress boundary value than simple tension, at least within the context of plane Cauchy stress.
The singular simple tension problem was considered in [13] and attention will be focused here instead on the problem of simple shear. It follows immediately from (2.6) than
Solving for the pressure term using the remaining plane stress condition \(T_{zz}=0\) and substitution into the constitutive law (2.2) yields the following in-plane stresses:
This set of equations and the incompressibility constraint \(\text{det}\, \boldsymbol{B}=1\), which reduces to
constitute a system of four equations in the four unknowns \(B_{xx}\), \(B_{xy}\), \(B_{yy}\), \(B_{zz}\) for stress boundary value problems. However, inversion of (2.11) in order to obtain the components of \(\boldsymbol{B}\) in terms of the in-plane stresses is challenging, even for the simplest of materials. For example, for the neo-Hookean material
where \(\mu \) is the infinitesimal shear modulus, invertibility requires the solving of a cubic equation since substitution of (2.13) into (2.11) yields
where the hat notation denotes non-dimensionalisation with respect to \(\mu \).
The compatability problems follow immediately from (2.10). In terms of the components of the deformation gradient tensor \(\boldsymbol{F}\), these equations have the form
Noting that \(F_{iJ}\equiv \frac{\partial x_{i}}{\partial X_{J}}\), where \((X,Y,Z)\), \((x,y,z)\) are the Cartesian coordinates of a typical particle before and after deformation respectively, it is easily seen that (2.15) constitute an underdetermined system of non-linear coupled partial differential equations in \((x,y,z)\). A semi-inverse approach is typically adopted (Moon and Truesdell [4], Mihai and Goriely [5], Destrade et al. [6]) to solve this system in which it is assumed that
The incompressibility constraint then yields
Trivially then
and the equations (2.15) are identically satisfied.
Assume now that the constitutive law is invertible. For deformations of the form (2.16), the non-identically zero components of \(\boldsymbol{B}\) can be expressed in terms of the components of the deformation gradient tensor as follows:
Classically the ultimate goal in the analysis of plane stress boundary value problems is the determination of the displacement field of a typical particle. Therefore (2.19)1,2,3 constitute an over-determined system of non-linear partial differential equations for the in-plane coordinates \((x,y)\) of a typical particle in the deformed configuration. When the applied stress field is homogeneous, and therefore \(\boldsymbol{B}\) is homogeneous, another semi-inverse approach is usually adopted with deformation tensors of the form (2.19) being interpreted as describing a simple shear superposed on a triaxial stretch (Moon and Truesdell [4], Mihai and Goriely [5], Destrade et al. [6]) so that the deformation gradient tensor is assumed to be of the form
In contrast, it is shown later that for Piola-Kirchhoff plane stress problems a semi-inverse approach leading to (2.16) is not required and the non-uniqueness in the determination of the deformation gradient tensor can be more prescribed. This might suggest that the Piola-Kirchhoff formulation of plane stress is a more natural choice.
3 Piola-Kirchhoff Plane Stress Problems
Let \(\boldsymbol{P}\) denote the first Piola-Kirchhoff stress tensor so that in general
noting that for the incompressible materials of interest here \(J\equiv \text{det}\, \boldsymbol{F}\equiv 1\). The symmetry of the Cauchy stress tensor follows from conservation of angular momentum and therefore
If the Piola-Kirchhoff plane stress conditions (1.9) are assumed then (3.2) yields
and
which could be viewed as the Piola-Kirchhoff equivalents of the Cauchy stress universal relations (2.5), (2.6). Note however that the Piola-Kirchhoff relations hold for all deformable solids, whereas the Cauchy relations (2.4) are only valid for isotropic materials.
As for plane Cauchy stress problems, there are therefore two classes of plane stress problems for deformable solids when Piola-Kirchhoff stress is being considered. The first is that class for which
exemplified by the problem of simple shear for which
The second is the seemingly singular class for which
This class can be considered to describe simple tension since trivially classical simple tension
satisfies (3.7) as does the stress distribution
which describes the experiment in which equal and opposite forces are applied to opposing vertices of a cuboid specimen (Murphy [13]).
First consider the class of simple shear plane stress problems characterised by (3.5), with the simple tension class defined by (3.7) considered later. It follows from (3.4) that
and therefore
The deformation gradient tensor therefore has the form
and therefore for incompressible materials
It follows from (3.12) that
and
4 Hyperelastic Incompressible Isotropic Solids
To make further progress in the analysis of Piola-Kirchhoff plane stress problems, the constitutive law must be specified. The constitutive law for homogeneous isotropic incompressible materials in terms of the Piola-Kirchhoff stress can be written in the form
where \(p\) is the undetermined hydrostatic pressure. It follows from the results of the last section that
Since the determinant of the coefficients of the \(F_{xZ}\), \(F_{yZ}\) terms
by virtue of the Empirical Inequalities (2.3), it follows that the plane stress conditions \(P_{xZ}=P_{yZ}=0\) can be satisfied if and only if
It then follows from this and (3.11) that the incompressibility condition now yields
so that
Thus if the plane shear stress conditions
hold then the resulting deformation for all incompressible isotropic materials must be a plane deformation (4.3) restricted by (4.5) accompanied by a uniform out-of-plane contraction \((\lambda <1)\) or expansion \((\lambda >1)\).
The deformation tensors now have the following simplified forms:
The corresponding invariants are therefore given by
It remains to satisfy the normal plane stress condition
which is satisfied if and only if
The in-plane stress components for plane stress conditions therefore have the form
It is easy to check that the relation (3.3) is satisfied. Assume here and in what follows that
Two approaches will be adopted here to make further progress. The first is to consider those problems for which two of the stresses are specified to be identically zero. In that special case a universal relation valid for all materials can be obtained. The second, which is considered in Sect. 6, is to specify the strain energy and for ease of exposition only the neo-Hookean material will be considered.
5 Simple Shear
Now consider the problem of pure simple shear (3.6). It follows from the Empirical Inequalities (2.3) and (4.13)1,2 that (3.6)1,2 are satisfied if and only if
Consider first the solution for which \(F_{xX}=F_{yY}>0\) or alternatively that
Assuming that \(x=x(X,Y)\), \(y=y(X,Y)\) are sufficiently regular, this condition is equivalent to the existence of a deformation potential function \(\psi (X,Y)\) such that
Enforcing the incompressibility condition (4.5) yields the determining non-linear partial differential equation for \(\psi \),
Only the consequences of the particular solution to (5.3),
where \(c_{i}\) are constants satisfying \(c_{1}^{2}-c_{2}c_{3}>0\), are explored here. The consequences of more general solutions to the nonlinear hyperbolic Monge-Ampère partial differential equation (5.3) will be examined elsewhere. Solving (5.4) and ignoring constant and translational terms yields
The deformation of a typical particle then follows from (4.4) and (5.2) and is given by
where, to satisfy (5.3),
The in-plane normal stress conditions \(P_{xX}=P_{yY}=0\) and (4.13)1,2 then yield
on using the incompressibility condition. Since \(c_{1}\) has been assumed positive, it therefore follows that
where now
The universal relation (3.3) now yields
Adding (4.13)3,4 then yields
on using (5.9). To ensure a non-zero shear stress, it must be assumed that
The consequences of the second branch of the solution to (5.1) are now explored. Assume then that
The in-plane normal stresses are then given by
which, on using the Empirical Inequalities, yield
If \(\lambda \ne 1\), then \(F_{xX}=F_{yY}=0\), contradicting the assumption (4.14). Assume then that \(\lambda =1\) and therefore that \(F_{xX}=F_{yY}\), from (5.14). The governing equation (5.12) and the incompressibility constraint (4.5) then take the respective forms
which yield
Given that the shear stresses are now identically zero, the conclusion is that (5.12) is not a valid potential solution branch for (5.1) and therefore we have the unique solution that \(F_{xX}=F_{yY}>0\).
6 The Neo-Hookean Material
Let \(\hat{P}_{iA}\equiv \frac{P_{iA}}{\mu}\). Then the in-plane stress equations (4.13) can be inverted for the neo-Hookean material (2.13) to obtain
Substitution into the incompressibility relation (4.5) then yields
Since it has been assumed that \(\hat{P}_{xX}\hat{P}_{yY}-\hat{P}_{xY}\hat{P}_{yX}\ne 0\), first assume that
so that the normal stresses are dominant. Then there are two solutions to (6.2), one contractile with \(\lambda <1\) and one extensile with \(\lambda >1\). Now assume that the shear stresses are dominant with
Again there are two solutions to (6.2), one contractile and one extensile, with the exception of the unique solution \(\lambda =1\) when
In this case it now follows from the plane stress constitutive law that
There is therefore a non-uniqueness in both the normal and shear components of the deformation gradient tensor for this class of plane stress boundary value problems.
It follows from (6.1) therefore that when \(\lambda \ne 1\) the general plane stress deformation has the form
with \(\lambda \) determined from (6.2).
7 Simple Tension
Now consider the problem of determining the deformation for the class of plane stress simple tension problems defined by the condition that
The analysis of the general case is complicated by the fact the universal relations (3.3), (3.4) do not allow the simplification of the deformation gradient tensor that was possible for simple shear problems. Some progress can be made for some important special cases such as simple and biaxial tension and the case of uniform in-plane stress for which
For illustrative purposes only simple tension is considered. Assume then that
which corresponds to Piola-Kirchhoff simple tension in the \(X\)-direction. Then (7.1) is trivially satisfied and the universal relations (3.3), (3.4) yield
The deformation gradient tensor now has the form
and therefore for incompressible materials
Denoting partial differentiation using the comma notation, it follows from (7.6) that \(F_{xX,X}=0\) and therefore
This is therefore the unique form of the \(x\)-component of the deformation field for all deformable incompressible solids regardless of symmetry.
It follows from (7.5) that
The constitutive law (4.1) now yields
The Empirical Inequalities (2.3) then yield that \(P_{xY}=P_{xZ}=0\) if and only if
It follows from (7.7) that the \(x\)-component of the deformation field for incompressible, isotropic hyperelastic materials in simple tension must have the form
The simple tension conditions \(P_{yY}=P_{zZ}=0\) now take the respective forms
Multiplying the first of these by \(F_{yY}\), the second by \(F_{zZ}\) and subtracting yields
on using the Empirical Inequalities (2.3). Assume then that \(F_{yY}=F_{zZ}\ne 0\). Then mirroring the analysis for simple shear it follows that there exists a potential function \(\Psi \) such that
assuming sufficient regularity of the displacement field, with the potential function again satisfying the Monge-Ampére partial differential equation (5.3) with the appropriate changes in independent variables. The analysis following (5.3) for simple shear is therefore also valid for simple tension and will not be repeated here.
To reflect the more singular nature of simple tension, a further restriction other than that necessary for simple shear must also be imposed here. First note that it follows from (7.12) that
The remaining zero stress conditions \(P_{yZ}=P_{zY}=0\) then yield, on substitution from (7.14),
so that
on employing the Empirical Inequalities (2.3). The potential representation (7.13) then shows that \(\Psi \) must therefore also satisfy the two-dimensional Laplace’s equation
in addition to the Monge-Ampére equation. Again only the trivial solution (5.5)
to the Monge-Ampére equation will be considered. Substitution into Laplace’s Equation then yields
in contrast to the condition (5.11) for simple shear. The displacement field is thus given by
The incompressibility condition now simplifies to
Finally, the simple tension stress condition \(P_{xX}=P\) yields
where
8 Concluding Remarks
The objective of this work was to examine two different formulations of plane stress problems for incompressible isotropic hyperelastic materials. The first approach involves an initial prescription of a prescribed Cauchy stress field and an investigation of how much information can be deduced on the corresponding stretch tensor and deformation. Early work on this issue for special cases was carried out by Batra [3] for simple tension and by Moon and Truesdell [4] for simple shear. More recent work by other authors has been described in the Introduction. The second approach is concerned with prescription of a plane stress state in terms of the Piola-Kirchhoff stress and it is shown here that this formulation is more tractable analytically. All these developments have been carried out for a general incompressible isotropic hyperelastic material with strain-energy density expressed in terms of the two classical principal invariants. For the special case of a neo-Hookean material, an explicit representation for the general plane stress deformation in terms of the prescribed Piola-Kirchhoff stresses was obtained.
References
Rivlin, R.S.: Large elastic deformations of isotropic materials IV. Further developments of the general theory. Philos. Trans. R. Soc. Lond. A 241, 379–397 (1948)
Blume, J.A.: Compatibility conditions for a left Cauchy-Green strain field. J. Elast. 21, 271–308 (1989)
Batra, R.C.: Deformation produced by a simple tensile load in an isotropic elastic body. J. Elast. 6, 109–111 (1976)
Moon, H., Truesdell, C.: Interpretation of adscititious inequalities through the effects pure shear stress produces upon an isotropic elastic solid. Arch. Ration. Mech. Anal. 55, 1–17 (1974)
Mihai, L.A., Goriely, A.: Positive or negative Poynting effect? The role of adscititious inequalities in hyperelastic materials. Proc. R. Soc. A 467, 3633–3646 (2011)
Destrade, M., Murphy, J.G., Saccomandi, G.: Simple shear is not so simple. Int. J. Non-Linear Mech. 47, 210–214 (2012)
Thiel, C., Voss, J., Martin, R.J., Neff, P.: Shear, pure and simple. Int. J. Non-Linear Mech. 112, 57–72 (2019)
Rajagopal, K.R.: The elasticity of elasticity. Z. Angew. Math. Phys. 58, 309–317 (2007)
Rajagopal, K.R.: Conspectus of concepts of elasticity. Math. Mech. Solids 16, 536–562 (2011)
Horgan, C.O., Murphy, J.G.: Simple shear and applied Piola-Kirchhoff shear stress. J. Elast. 1-12 (2022). https://doi.org/10.1007/s10659-022-09924-1
Timoshenko, S., Goodier, J.N.: Theory of Elasticity. McGraw-Hill, New York (1951)
Murphy, J.G., Saccomandi, G., Vitral, E.: An inverted Rivlin-type universal relation for simple shear. Int. J. Non-Linear Mech. 140, 103911 (2022)
Murphy, J.G.: Simple tension three ways. Int. J. Solids Struct. 284, 112497 (2023)
Funding
Open Access funding provided by the IReL Consortium.
Author information
Authors and Affiliations
Contributions
C.O.H. and J.G.M. originated the original concept. The first draft was prepared by J.G.M. and extensively revised by C.O.H. Both authors reviewed the final version.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Additional information
Publisher’s Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Rights and permissions
Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
About this article
Cite this article
Horgan, C.O., Murphy, J.G. Plane Stress Problems for Isotropic Incompressible Hyperelastic Materials. J Elast (2024). https://doi.org/10.1007/s10659-024-10057-w
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s10659-024-10057-w
Keywords
- Plane stress
- Piola-Kirchhoff stress
- Incompressible isotropic hyperelastic materials
- Simple tension and shear
- Neo-Hookean material