A commented translation of Hans Richter's early work "The isotropic law of elasticity"
Kai Graban, Eva Schweickert, Robert J. Martin, Patrizio Neff

TL;DR
This paper offers an accurate English translation of Hans Richter's 1948 work on the isotropic law of elasticity, including an overview of Richter's contributions to the field.
Contribution
It provides the first faithful English translation of Richter's influential 1948 paper on isotropic elasticity laws, with a summarizing introduction.
Findings
Historical insight into Richter's work
Clarification of early elasticity laws
Enhanced accessibility for English-speaking researchers
Abstract
We provide a faithful translation of Hans Richter's important 1948 paper "Das isotrope Elastizit\"atsgesetz" from its original German version into English. Our introduction summarizes Richter's achievements.
| Our notation | Richter’s notation | meaning |
| , | , | arbitrary -matrices |
| transpose of | ||
| entry in the -th row and the -th column of | ||
| determinant of | ||
| trace of | ||
| identity tensor | ||
| inverse of | ||
| Jacobian matrix (state of strain) | ||
| pure Euclidean rotation | ||
| pure stretch | ||
| stress tensor (state of stress) | ||
| temperature | ||
| , , | , , | invariants of |
| logarithmic stretch: | ||
| , , | , , | invariants of : , , |
| , , | , , | coefficient functions |
| , , | , , | coefficient functions |
| internal energy | ||
| entropy | ||
| free energy | ||
| differential of the work | ||
| , , | , , | unit vectors in the principal stretch directions of |
| , , | , , | components of in the principal stretch directions of |
| , | , | stretch in shape, stretch in volume |
| stretch factor of the stretch in volume | ||
| , | , | , |
| arbitrary symmetric matrix | ||
| common deviator of | ||
| , | , | invariants of : , |
| , | , | volumetric energies |
| , | , | isochoric energies |
| resp. | resp. | reference temperatures |
| [index] | indicates the correspondence to the temperature | |
| logarithmic thermal expansion | ||
| deformation with respect to the initial state at | ||
| indicates the correspondence to the deformation | ||
| , | , | Lamé constants |
| Poisson modulus |
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Taxonomy
TopicsElasticity and Material Modeling · Composite Material Mechanics · Composite Structure Analysis and Optimization
A commented translation of Hans Richter’s early work
?The isotropic law of elasticity?
Kai Graban and Eva Schweickert and Robert J. Martin and Patrizio Neff Kai Graban, Fakultät für Mathematik, Universität Duisburg-Essen, Thea-Leymann Str. 9, 45127 EssenEva Schweickert, Lehrstuhl für Nichtlineare Analysis und Modellierung, Fakultät für Mathematik, Universität Duisburg-Essen, Thea-Leymann Str. 9, 45127 Essen, Germany; email: [email protected] J. Martin, Lehrstuhl für Nichtlineare Analysis und Modellierung, Fakultät für Mathematik, Universität Duisburg-Essen, Thea-Leymann Str. 9, 45127 Essen, Germany; email: [email protected] Neff, Head of Lehrstuhl für Nichtlineare Analysis und Modellierung, Fakultät für Mathematik, Universität Duisburg-Essen, Thea-Leymann Str. 9, 45127 Essen, Germany, email: [email protected]
(March 9, 2024)
Abstract
We provide a faithful translation of Hans Richter’s important 1948 paper ?Das isotrope Elastizitätsgesetz? from its original German version into English. Our introduction summarizes Richter’s achievements.
Abstract
From the demand of the isotropy and of the existence of the thermodynamic potentials a general form of the three-dimensional law of elasticity is stated. In doing so, the logarithmic matrix of relative elongations is used, which permits the separation of the variation of the volume and that of the shape by simply forming the deviator. The resilience energy is exactly the sum of the energy of the variation of the volume and that of the shape, if the average tension depends only on the variation of the volume. For finite deformations, the law of Hooke is permissible only in the case .
Aus der Forderung der Isotropie und der Existenz der thermodynamischen Potentiale wird für das räumliche Elastizitätsgesetz eine allgemeine Form angegeben, wobei die logarithmische Dehnungsmatrix verwendet wird, bei der die Trennung in Volum- und Gestaltänderung durch gewöhnliche Deviatorbildung möglich ist. Die elastische Energie ist genau dann die Summe aus Volum- und Gestaltänderungsenergie, wenn die mittlere Spannung nur von der Volumänderung abhängt. Das Hookesche Gesetz ist für endliche Verzerrungen nur bei zulässig.
En supposant l’isotropie et l’existence des potentiels thermodynamiques, on donne une forme générale de la loi de l’élasticité en se servant d’une matrix logarithmique d’allongement. Ce procédé permet une séparation des changements de volume et de forme par une simple formation de déviateur. Si la tension moyenne ne dépend que du changement de volume, l’énergie d’élasticité est la somme des énergies de changement du volume et de la forme. La loi de Hooke n’est admissible que pour .
Key words: nonlinear elasticity, isotropic tensor functions, hyperelasticity, logarithmic stretch, volumetric-isochoric split, Hooke’s law, finite deformations, isotropy
**AMS 2010 subject classification: 74B20, 01A75
**
Introduction
Shortly after the second world war, in a series of papers [23, 24, 25, 26] from , Hans Richter () laid down his general format of isotropic nonlinear elasticity based on a rather modern approach with direct tensor notation. By translating his work ?Das isotrope Elastizitätsgesetz? [23], we aim at making his development, which precedes later work in the field by several decades, accessible to the international audience.
Let us briefly summarize Richter’s achievement in this paper. He uses, for the time, rather advanced methods of matrix analysis (including the theory of primary matrix functions [12]) and employs the left polar decomposition [11, 22, 20] of the deformation gradient into a stretch and a rotation . For Richter, the ?physical stress tensor? is the Cauchy stress tensor . From the coaxiality between and for an isotropic response, he deduces the representation formula for isotropic tensor functions (the Richter representation, see (2.6))
[TABLE]
(predating the Rivlin-Ericksen representation theorem [27] by years) where , are scalar valued functions of the invariants , , with
[TABLE]
Alongside, Richter introduces the logarithmic stretch tensor without citing the previous work of Hencky [7, 9, 8, 10, 16, 18, 19, 17, 21]. He then turns to the question of what happens if the relation (0.1) is derived from a stored energy , i.e. when (0.1) is consistent with hyperelasticity. He obtains the correct representation (see (3.11) in his text)
[TABLE]
In the next section, Richter introduces the multiplicative split of the elastic stretch into volume preserving (isochoric) parts and volume change (see (4.1))
[TABLE]
and he observes that the logarithmic stretch tensor additively separates both contributions by using the classical deviator operation (see (4.2)) such that
[TABLE]
He also observes that the invariants based on the logarithmic stretch tensor satisfy certain algebraic relations, cf. [3]. In Richter’s fifth section, he introduces the volumetric-isochoric split
[TABLE]
of the stored energy (often erroneously attributed to [6]) and he immediately obtains the important result:
An isotropic energy is additively split into volumetric and isochoric parts if and only if the mean Cauchy stress is only a function of the relative volume change . In that case,
[TABLE]
This result has been rediscovered and re-derived multiple times, e.g. in [2, 13, 28, 4, 5, 14]. In addition, Richter shows that this property of the volumetric-isochoric split is invariant under a change of the reference temperature. Finally, he poses the question whether a linear relation between and in the form (the Hooke’s law as he perceives it)
[TABLE]
where is the shear modulus and is the second Lamé parameter, can be consistent with hyperelasticity. A short calculus reveals that (0.6) is hyperelastic if and only if , i.e. for Poisson ratio (which is approximately satisfied for many metals, e.g. aluminium). For all other values of , Hooke’s law is incompatible with the hyperelastic approach and Richter proposes to use instead (the quadratic Hencky energy [7, 15])
[TABLE]
with the induced stress-strain law
[TABLE]
where is the Kirchhoff stress tensor.
We will briefly discuss the constitutive relation (0.6). In order to check hyperlasticity of the Cauchy stress-stretch relation in this case, we use the representation, consistent with (0.2),
[TABLE]
and consider the energy . Then .
Since and , the Cauchy stress tensor given by (0.6) with is injective (but not bijective, since for there does not exist a stretch such that ). Furthermore, note that
[TABLE]
where are the singular values of the deformation gradient . Then
[TABLE]
For this energy, the weak empirical inequalities [30] and are satisfied. The principal Cauchy stresses are given by , which shows that the tension-extension (TE) inequalities and the Baker-Ericksen (BE) inequalities [1], given by
[TABLE]
respectively, are satisfied as well. We also note that is the Shield-transformation [29] of , where
[TABLE]
has the Valanis-Landel form111This calculus shows that the Valanis-Landel form is not invariant under the Shield transformation. In addition, the mapping of the stretch to the Biot stress tensor is strictly monotone. [31] and is convex in ; the TE-inequalities are satisfied as well.
Richter’s paper is not only written in German, but his notation strongly relies on German fraktur letters, which makes reading his original work rather challenging. In our faithful translation of his paper, we have therefore updated the notation to more current conventions; a complete list of notational changes is provided in Appendix A. Richter’s original equation numbering has been maintained throughout.
1 Definitions
In generalization of Hooke’s law, a material is called purely elastic if the Cauchy stresses depend in a uniquely reversible way on the stretches. Strictly speaking, however, it is necessary to discuss the heat transfer which occurs in the tensile test; in particular, it is necessary to distinguish between an adiabatic and isothermal law of elasticity. This choice also clarifies what is meant by strains, since strains on the adiabat resp. isotherm can be referred e.g. to the initial state, for which the stresses disappear completely. The strains can also be referred to a stress-free initial state at an arbitrarily chosen initial temperature instead. Then the stress-free state at another temperature corresponds, in the case of an isotropic material, to uniform stretches in all directions, i.e. the thermal expansion. In this manner the law of thermal expansion is included in the elastic law. Of course, the affected material must be assumed not to change permanently by changes in temperature within the considered temperature range.
Thus, we assume a stress-free state at a temperature . Let the deformation of the material into another state be characterized by the matrix and the related stresses by the stress tensor .222 is the Jacobian matrix: . is the physical stress tensor at the point . We call the material ideally elastic if depends uniquely on and . The material is said to be isotropic if this dependence is invariant under Euclidean rotations.
When solving the problem of finding the most general form of this dependence, one appropriately operates with matrices, where the following abbreviations are used:
is the matrix obtained by reflecting over its main diagonal. is the entry in the -th row and the -th column of . is the determinant of . is the sum of the elements on the main diagonal of : called the trace of . is the identity tensor. If , then, assuming convergence, .
Recall the following simple statements:
[TABLE]
if commutes with , but not necessarily with .
[TABLE]
if is well defined.
[TABLE]
Every can be represented in the form:
[TABLE]
where the multiplication is to be read in its functional notation from right to left.
2 Consequence of isotropy
According to (1.5), can be interpreted as a rotation followed by a stretch , where the principal stretch directions of the latter are rotated against those of the coordinate axes. For the case of isotropic materials, the application of must not have any influence on . Therefore, is a function of and . For given , we can find by using (1.4) and (1.5) by
[TABLE]
The most general coaxial relation between and which fulfills the invariance under rotations is now, obviously,
[TABLE]
where the are the invariants333It is easy to see that here, one of the invariants can be omitted, in contrast to the subsequent formula (2.7). of .
Instead of , one can also use a uniquely invertible function of . As we will see later on, it is appropriate to use the “logarithmic stretch”
[TABLE]
which is always defined because of the positive eigenvalues of . We denote the invariants of by
[TABLE]
Further, from (1.3) and (2.1) we obtain: .
Instead of (2.2), we can now write
[TABLE]
Here, , and are functions of , , and due to (2.5). If we now define the invariants , and as the solutions to the system of equations
[TABLE]
with, in general, non-vanishing determinant, then we have for
[TABLE]
Since is coaxial to , it is completely determined by , and . Therefore, holds; i.e.
[TABLE]
Hence, we have found the most general isotropic relation. Using instead of , we would correspondingly obtain:
[TABLE]
3 Consequence of the potential
The internal energy of the material per unit volume in the initial state is denoted by
[TABLE]
Then the free energy takes the form
[TABLE]
If is now the differential of the work done by the element of volume, then
[TABLE]
Thus for isothermal elastic changes, we have
[TABLE]
where has to be eliminated in (3.1) and (3.2), so that appears as a function of , , and .
In order to calculate , we transition from a deformation to the neighboring deformation . Since a pure rotation has no influence on , we can assume that is a pure stretch. Let , and be the unit vectors in the principal stretch directions of , which can be interpreted as coordinate vectors. Let , and be the components of in these directions. We can use the rectangular parallelepiped spanned by , and as the volume element, which is generated by the stretch applied to the unit cube. Let us now consider the side which starts from and which is spanned by and . Besides an infinitesimal tilting and change of the surface, this side undergoes a displacement in the -direction with the magnitude in the transition from to . The work done on the considered side is therefore
[TABLE]
Thus the entire work done by the volume element is
[TABLE]
The deformation now corresponds to a stretch , where due to (2.1),
[TABLE]
Multiplying the left side of the equation by , taking the trace and using (1.1), we find
[TABLE]
since is symmetric and coaxial to . From (3.7) we therefore obtain
[TABLE]
Hence, due to (1.2), (1.3) and (2.4):
[TABLE]
If we substitute this expression into the isothermal relation (3.5) and use (2.6), then it follows:
[TABLE]
Since, by (2.4),
[TABLE]
we finally conclude that
[TABLE]
and therefore, with (2.6),
[TABLE]
Accordingly, from (3.6) we obtain for the adiabatic law:
[TABLE]
If we want to omit the introduction of and use directly when formulating the law of elasticity, then we appropriately use the following as the invariants of :
[TABLE]
Furthermore, according to (2.7), (3.5) and (3.8), an analogous computation leads to the law of elasticity in the form
[TABLE]
and a corresponding formulation with instead of .
4 Transition to the deviators
The introduction of the logarithmic stretch now proves to be not only appropriate to formulate the law of elasticity as simple as possible, but using also allows for the decomposition of a deformation into a shape change and volume change by simply taking the deviatoric part, i.e. the same approach as for infinitesimal strains, whereas a corresponding decomposition in terms of is highly inconvenient. To see this, we decompose the general stretch into a shape-changing stretch and a volume-changing stretch , i.e. we demand:
[TABLE]
Obviously, (4.1) uniquely determines such a decomposition for each with ; namely, for given ,
[TABLE]
Since commutes with , we can take the logarithm of (4.1):
[TABLE]
Then, by (1.3), we obtain:
[TABLE]
If, in general, we denote by the deviator corresponding to the symmetric matrix , i.e.
[TABLE]
we can finally write:
[TABLE]
Thus the change of shape is indeed characterized by the deviator of . For infinitesimal strains we have , so that turns into the usual deformation deviator.
If we now introduce the invariants of :
[TABLE]
We can use , and instead of , and as variables. Then characterizes the change of volume, whereas and characterize the change of shape. As one can easily calculate, (3.9) leads to the formula
[TABLE]
where, in contrast to (3.9), now holds.
A corresponding formula results from (3.10).
Without proof, let us remark that and cannot take on all possible values independently of each other, but are restricted by the condition
[TABLE]
5 Decomposable elasticity laws
In the elasticity theory of infinitesimal strains the elastic energy can be interpreted as the sum of the energy of the volume and shape change. Since the change of volume is represented by and the change of shape is represented by and , this decomposition is possible for the case of finite strains if and only if
[TABLE]
holds. Then with (4.6):
[TABLE]
Thus the average stress depends only on , i.e. on the change of volume. If, vice versa, depends only on , then by (4.6) we obtain
[TABLE]
which also leads to the form of in (5.1). Consequently, we can state: The elastic energy can be decomposed into the energy of change of volume and of change of shape if and only if the mean stress depends only on the change of volume.
6 Transition to a new reference temperature
We referred the deformations to the stress-free state at a certain temperature . Now we assume another temperature to be used as initial temperature instead of . For , the temperature corresponds to a certain deformation with . is a scalar multiple of the identity tensor; thus , . Then with (4.6):
[TABLE]
which leads to the law of thermal expansion:
[TABLE]
Since is the matrix corresponding to the deformation with respect to the new initial state, we thus have , and hence
[TABLE]
In formula (4.6), we can now replace by if we simultaneously substitute with
[TABLE]
In particular, it follows that the decomposition of the elastic energy, which was discussed in Section 5, is independent of the choice of the reference temperature.
7 Validity of Hooke’s law
Due to the formulae found previously, one can impose a wide variety of requirements on the law of elasticity, in particular with respect to the dependence on temperature, and verify if these requirements can be satisfied. Let us now consider the question whether the common law by Hooke remains valid for finite strains.
Using the Lamé constants, Hooke’s law takes the form
[TABLE]
It is obvious that (7.1) is actually derived from the general formula (3.9) for small .
In order for the isothermal law of elasticity (7.2) to remain valid for finite strains, the following equations must be fulfilled according to (3.11):
[TABLE]
This is only possible if , which corresponds to the Poisson ratio . For all other values of , Hooke’s law cannot be used for finite strains. Instead, one can use the corresponding logarithmic law
[TABLE]
which, in the isothermal case, corresponds to the decomposable energy
[TABLE]
††Received 2. February 1948
Appendix A List of Symbols
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] M. Baker and J. L. Ericksen “Inequalities restricting the form of the stress-deformation relation for isotropic elastic solids and Reiner-Rivlin fluids” In J. Washington Acad. Sci. 44 , 1954, pp. 33–35
- 2[2] P Charrier, Bernard Dacorogna, B Hanouzet and P Laborde “An existence theorem for slightly compressible materials in nonlinear elasticity” In SIAM Journal on Mathematical Analysis 19.1 SIAM, 1988, pp. 70–85
- 3[3] J. C. Criscione, J. D. Humphrey, A. S. Douglas and W. C. Hunter “An invariant basis for natural strain which yields orthogonal stress response terms in isotropic hyperelasticity” In Journal of the Mechanics and Physics of Solids 48.12 Elsevier, 2000, pp. 2445–2465
- 4[4] Nicolas Favrie, S Gavrilyuk and S Ndanou “A thermodynamically compatible splitting procedure in hyperelasticity” In Journal of Computational Physics 270 Elsevier, 2014, pp. 300–324
- 5[5] Salvatore Federico “Volumetric-distortional decomposition of deformation and elasticity tensor” In Mathematics and Mechanics of Solids 15.6 Sage Publications Sage UK: London, England, 2010, pp. 672–690
- 6[6] P. J. Flory “Thermodynamic relations for high elastic materials” In Transactions of the Faraday Society 57 The Royal Society of Chemistry, 1961, pp. 829–838
- 7[7] H. Hencky “Über die Form des Elastizitätsgesetzes bei ideal elastischen Stoffen” available at www.uni-due.de/imperia/md/content/mathematik/ag_neff/hencky 1928.pdf In Zeitschrift für technische Physik 9 , 1928, pp. 215–220
- 8[8] H. Hencky “Das Superpositionsgesetz eines endlich deformierten relaxationsfähigen elastischen Kontinuums und seine Bedeutung für eine exakte Ableitung der Gleichungen für die zähe Flüssigkeit in der Eulerschen Form” available at https://www.uni-due.de/imperia/md/content/mathematik/ag_neff/hencky_superposition 1929.pdf In Annalen der Physik 394.6 , 1929, pp. 617–630
