Continuum Mechanics and Elasticity
Between the finitely many degrees of freedom of Rigid Bodies and Rotating Frames and the fluids of Fluid Dynamics stands the deformable solid. This chapter replaces the rigid body's six coordinates by continuous fields: the displacement field and its strain tensor, the stress tensor that transmits force through matter, and the linear law — Hooke's — that couples them. From these follow the equations of elastodynamics, the elastic waves that carry earthquakes across the planet, the engineering theories of rods, beams and plates, and the measured elastic constants that anchor every parameter of the theory to experiment. The continuum limit constructed here is also the pattern for every later field theory in the book, from the fluids of the next chapter to the lattice dynamics of Phonons and Lattice Dynamics and the Lagrangian fields of Generalized Classical Field Theory. The canonical monograph is Landau and Lifshitz's Theory of Elasticity [Landau:1986].
The tensor machinery this chapter uses — the transformation law under orthogonal changes of frame, the algebra of Cartesian tensors, the quotient law — is that of Differentiable Manifolds, Tensors, and Curvature, and is not rebuilt here. What is built here is physics: which tensors the solid carries, what the observed relation between them is, and what follows from it.
Following [Landau:1986], \(u_{i}\) with one index denotes a component of the displacement field and \(u_{ik}\) with two denotes a component of the strain tensor; they are different objects, related by Equation (30.4). Stress is \(\sigma_{ik}\), mass density \(\rho\), and repeated Latin indices are summed over the three spatial directions. All indices are Cartesian, so index position carries no meaning (Definition 13.5); the metric is \(\delta_{ik}\). Rests on Definition 13.5.
The continuum hypothesis
A cubic centimetre of copper holds of order \(10^{23}\) nuclei and as many electrons, and no theory of matter that tracks them individually will ever predict the sag of a bridge. The whole of this chapter rests on replacing that population by a handful of smooth fields. The replacement is not a mathematical convenience but a physical claim with a domain of validity, and the claim can be stated sharply enough to be tested.
Let \(a\) be the mean spacing between the constituent particles of a body and \(L\) the scale over which the applied loads and the geometry vary. A representative volume element at the point \(\vect{x}\) is a region of linear size \(\ell\) centred there with
A continuum field is a quantity assigned to \(\vect{x}\) by averaging the corresponding microscopic quantity over the representative volume element: the mass density \(\rho(\vect{x})=\Delta m/\Delta V\), the velocity \(\vect{v}(\vect{x})=\Delta\vect{p}/\Delta m\), and so on. The continuum hypothesis is the assertion that Equation (30.1) can be satisfied, so that the averages are insensitive to \(\ell\) over a wide range and the resulting fields are smooth on the scale \(L\). Rests on Definition 7.65.
The hypothesis is quantitative because the insensitivity is quantitative. Density fluctuations in a volume holding \(N\) particles are of relative size \(N^{-1/2}\) (Kinetic Theory of Gases), so the width of the plateau in \(\ell\) is set by how fast \(N\) grows.
Copper has mass density \(8960\,\mathrm{kg}/\mathrm{m}^{3}\) and molar mass \(63.55\,\mathrm{g}/\mathrm{mol}\), giving a number density \(n=8.49\times 10^{28}\,/\mathrm{m}^{3}\) and a mean spacing \(a=n^{-1/3}=0.227\,\mathrm{nm}\). A cube of side \(100\,\mathrm{nm}\) then contains \(N=8.5\times 10^{7}\) atoms and its density is defined to a relative precision \(N^{-1/2}=1.1\times 10^{-4}\). That cube is already \(440\) atoms across, so it is large in the sense of Equation (30.1); and it is \(10^{4}\) times smaller than a millimetre-scale specimen, so it is also small in that sense. Both inequalities in Equation (30.1) hold with four orders of magnitude to spare, which is why elasticity works so well for ordinary solids and why nothing in this chapter needs to know that copper is made of atoms. Rests on Definition 30.2.
Label each material particle by its position \(\vect{X}\) in a chosen reference configuration. The motion is the map \(\vect{x}=\vect{\chi}(\vect{X},t)\), and the displacement is
A field written as a function of \((\vect{X},t)\) is in the material (Lagrangian) description; written as a function of \((\vect{x},t)\), in the spatial (Eulerian) description. The two are related by the chain rule, so that for any field \(f\)
the second form being the material derivative. Rests on Proposition 7.72 and Definition 30.2.
A solid has a preferred reference configuration — the unloaded one, to which it returns — so solid mechanics is naturally Lagrangian. A fluid has none, which is why Fluid Dynamics is written in the spatial description throughout; Equation (30.3) is the bridge between the two chapters, and the nonlinear term it carries is the origin of the difficulties of that one.
Equation (30.1) is an inequality between measurable lengths, so its failure is measurable too.
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Rarefied gases. The relevant microscopic length is the mean free path \(\ell_{\text{mfp}}\), not the particle spacing. Air at room conditions has \(\ell_{\text{mfp}}\approx68\,\mathrm{nm}\), negligible against any laboratory apparatus; but in a high vacuum, or in the upper atmosphere, \(\ell_{\text{mfp}}\) grows to metres and the Knudsen number \(\ell_{\text{mfp}}/L\) approaches unity. Beyond \(\ell_{\text{mfp}}/L\sim0.1\) the continuum equations of Fluid Dynamics fail and the kinetic description of Kinetic Theory of Gases must be used instead.
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Nanoscale structures. A wire ten atoms across has no interior: most of its atoms are surface atoms, with a different coordination and a different local stiffness, so no plateau in \(\ell\) exists and the elastic moduli measured on such a specimen depend on its size.
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Singular regions inside a continuum. A shock front is a few mean free paths thick and a crack tip has a radius of a few lattice spacings. In both cases Equation (30.1) fails locally while holding everywhere else, which is why the continuum theory can keep them as idealised surfaces and points — and also why it predicts infinite stress there (Section 30.7).
What underwrites the hypothesis where it holds is the kinetic theory of Kinetic Theory of Gases: it is the law of large numbers applied to a mechanical system, and the smallness of \(N^{-1/2}\) is the whole of the argument. Rests on Definition 30.2 and Equation (30.1).
Deformation: the strain tensor
Displacement and linear strain
A displacement field that is the same everywhere translates the body without deforming it, and one that is linear and antisymmetric rotates it. Deformation is therefore carried by the symmetric part of the displacement gradient, and this is what the strain tensor isolates. Cauchy introduced both it and the stress tensor of Section 30.3 in the memoir that founded the subject [Cauchy:1823].
For a displacement field \(\vect{u}\) with small gradients, the strain tensor and the rotation tensor are the symmetric and antisymmetric parts of \(\pp_{i}u_{k}\):
Both are dimensionless. The dilatation is the trace \(u_{ll}=\vect{\nabla}\cdot\vect{u}\), and the traceless remainder
is the deviatoric or shear part. Rests on Equation (30.2) and Definition 13.91.
Under a change of orthonormal frame \(x'_{i}=a_{ik}x_{k}\) the nine quantities \(u_{ik}\) transform as \(u'_{ik}=a_{il}a_{km}u_{lm}\), that is, as the components of a rank-two tensor in the sense of Definition 13.5. The same holds for \(\omega_{ik}\), \(d_{ik}\), and the trace \(u_{ll}\) is a scalar. Rests on Definitions 13.5 and 30.6.
Derives Proposition 30.7. The displacement is a vector, \(u'_{k}=a_{km}u_{m}\), and for an orthogonal transformation with constant coefficients the differential operator carries a vector index as well, \(\pp'_{i}=a_{il}\pp_{l}\). The product \(\pp_{i}u_{k}\) is therefore a rank-two tensor by the product rule of Section 13.2.2, its symmetric and antisymmetric parts are tensors by the addition and index-permutation rules there, and the trace is a rank-zero tensor by the contraction rule. That the trace is a scalar is the statement that \(\vect{\nabla}\cdot\vect{u}\) does not depend on the frame in which it is computed, which is what makes Proposition 30.8 a statement about the body rather than about the observer.
∎This is the reason the subject is written in tensors at all. A material law must relate the deformation to the force without reference to the orientation of the laboratory; a relation between objects with the transformation law of Equation (13.22) has that property automatically, and one between arbitrary arrays of nine numbers does not.
To first order in the displacement gradients, a material element of volume \(\dd V\) becomes
so that \(u_{ll}\) is the fractional change of volume and the deviatoric part \(d_{ik}\) deforms at constant volume. Rests on Definition 30.6 and Equation (30.2).
Derives Proposition 30.8. The map \(\vect{X}\mapsto\vect{X}+\vect{u}(\vect{X})\) has Jacobian matrix \(F_{ik}=\delta_{ik}+\pp_{k}u_{i}\), and a volume element is multiplied by \(\det F\). For any matrix \(A\), \(\det\left(\identity+A\right)=1+\operatorname{tr}A+O(A^{2})\), since the terms of the determinant that are not the product of diagonal entries contain at least two off-diagonal factors. Hence \(\det F=1+\pp_{i}u_{i}+O\left((\pp u)^{2}\right)\), and \(\pp_{i}u_{i}=u_{ii}=u_{ll}\) because the antisymmetric part of \(\pp_{i}u_{k}\) has zero trace. The deviatoric part is traceless by construction, so it changes no volumes to this order.
∎At each point there is an orthonormal frame in which \(u_{ik}\) is diagonal. Its three diagonal entries \(u^{(1)},u^{(2)},u^{(3)}\) — the principal strains — are the fractional extensions along the three corresponding principal directions, and \(u_{ll}=u^{(1)}+u^{(2)}+u^{(3)}\). Rests on Definition 30.6 and Theorem 5.75.
Derives Proposition 30.9. \(u_{ik}\) is a real symmetric array, hence the matrix of a self-adjoint operator on \(\R^{3}\) with the Euclidean inner product; by Theorem 5.75 it has an orthonormal eigenbasis and real eigenvalues. In that basis a material line element along the \(j\)-th eigenvector of length \(\dd l\) becomes, to first order, one of length \(\left(1+u^{(j)}\right)\dd l\), since the antisymmetric part contributes a rotation and not a length change. The trace is basis independent by Proposition 30.7.
∎Let \(\vect{u}=(\gamma y,0,0)\) with \(\gamma=10^{-3}\): the displacement gradient has the single entry \(\pp_{y}u_{x}=\gamma\), so
The principal strains are \(\pm\gamma/2\) along the two directions at \(45^\circ\) to the axes, and \(0\) along \(z\); the trace vanishes, so no volume changes. What distinguishes “simple” shear from “pure” shear is only the accompanying rigid rotation \(\omega_{ik}\) of magnitude \(\gamma/2=5\times 10^{-4}\), and by Proposition 30.7 that rotation cannot enter any material law. A steel bar strained in shear by \(\gamma=10^{-3}\) is therefore stressed exactly as one stretched by \(5\times 10^{-4}\) along one diagonal and compressed by the same amount along the other. Rests on Proposition 30.9 and Definition 30.6.
Finite strain and compatibility
Definition 30.6 was announced as valid “for small gradients”. The exact statement is available and shows precisely what the truncation costs.
The Green (Lagrangian) strain tensor of the motion Equation (30.2) is
in which the indices are the material coordinates \(\vect{X}\). Rests on Equation (30.2) and Definition 30.6.
For every material line element \(\dd\vect{X}\),
with no approximation. Consequently \(E_{ik}\) vanishes identically if and only if the motion is a rigid displacement. Rests on Definitions 13.118 and 30.11.
Derives Proposition 30.12. With \(F_{ik}=\pp_{k}\chi_{i}=\delta_{ik}+\pp_{k}u_{i}\) one has \(\dd x_{i}=F_{ik}\dd X_{k}\), so
and subtracting \(\dd l^{2}=\delta_{lk}\dd X_{l}\dd X_{k}\) gives Equation (30.8). If \(E_{ik}\equiv0\) then every material length is preserved, so the motion is an isometry of \(\R^{3}\) and hence (Proposition 13.121) a rotation followed by a translation; the converse is immediate because a rigid motion has \(F\transpose F=\identity\).
∎Rotate a body rigidly about \(z\) through \(\theta\). Then \(\vect{u}=(R-\identity)\vect{X}\) with \(R\) the rotation matrix, and the linear strain of Equation (30.4) evaluates to
while \(E_{ik}=0\) exactly by Proposition 30.12. The linear measure reports a spurious contraction of \(\theta^{2}\) in volume where nothing has been deformed at all. For \(\theta=0.1\,\mathrm{rad}\) — under \(6^\circ\) — that is \(-5\times 10^{-3}\), four times the elastic strain \(\sigma_{\mathrm{y}}/E\approx1.2\times 10^{-3}\) at which structural steel yields (Phenomenon 30.73). The linear theory is therefore restricted not by the smallness of the strains but by the smallness of the rotations: a thin strip may bend far past \(\theta=0.1\) while every fibre in it stays elastic, and such a problem must be treated with Equation (30.7), or with the special geometrically nonlinear theories of Section 30.6.1. Rests on Proposition 30.12 and Definition 30.6.
The second question about a strain field is the reverse one. Six functions \(u_{ik}\) are prescribed; do they come from any displacement at all? The system Equation (30.4) is six equations for three unknowns, so the answer is no in general, and the obstruction has a name.
If \(u_{ik}\) is the linear strain of a \(C^{3}\) displacement field, then
identically. In three dimensions Equation (30.9) has six independent components. Rests on Definition 30.6 and Proposition 7.73.
Derives Proposition 30.14. Substitute \(u_{ij}=\tfrac{1}{2}(\pp_{i}u_{j}+\pp_{j}u_{i})\) into the left-hand side. The first term contributes \(\tfrac{1}{2}(\pp_{l}\pp_{k}\pp_{i}u_{j}+\pp_{l}\pp_{k}\pp_{j}u_{i})\) and the other three the analogous expressions; every one of the eight resulting third derivatives appears twice with opposite signs once the partial derivatives are freely commuted, which Proposition 7.73 licenses for a \(C^{3}\) field. The sum therefore vanishes term by term. The left-hand side is antisymmetric under \(i\leftrightarrow l\) and under \(j\leftrightarrow k\) and symmetric under the exchange of the pairs, which in three dimensions leaves \(3\times3\) components of which the six symmetric ones are the independent conditions — exactly the index symmetries of a curvature tensor (Proposition 13.154).
∎Let \(\Omega\subset\R^{3}\) be open, connected and simply connected, and let \(u_{ik}\) be a symmetric \(C^{2}\) field on \(\Omega\) satisfying Equation (30.9). Then there is a displacement field \(\vect{u}\) on \(\Omega\) whose linear strain is \(u_{ik}\), unique up to the addition of a rigid displacement \(\vect{a}+\vect{b}\times\vect{x}\). Rests on Propositions 7.104 and 30.14.
Derives Theorem 30.15. The construction is Cesàro's: recover first the rotation that the strain does not record, then the displacement. It uses no mathematics beyond Proposition 7.104(3), that a curl-free \(C^{1}\) field on a simply connected open set is a gradient.
Step 1: the rotation field. Set
which is \(C^{1}\) and antisymmetric in \(ij\). Were \(u_{ik}\) already the strain of a displacement, \(\Phi_{ijk}\) would be \(\pp_{k}\omega_{ij}\) with \(\omega_{ij}=\tfrac{1}{2}(\pp_{i}u_{j}-\pp_{j}u_{i})\) the infinitesimal rotation: substituting \(u_{jk}=\tfrac{1}{2}(\pp_{j}u_{k}+\pp_{k}u_{j})\) into Equation (30.10) gives \(\tfrac{1}{2}(\pp_{i}\pp_{k}u_{j}-\pp_{j}\pp_{k}u_{i})\), which is that derivative. Take this as the equation to be solved. For each fixed pair \(ij\) the field \(k\longmapsto\Phi_{ijk}\) is curl-free exactly when
vanishes, and the right-hand side is the compatibility expression Equation (30.9) with its four indices taken in the order \((i,k,l,j)\) and the sign reversed. It vanishes by hypothesis. By Proposition 7.104(3) on the simply connected \(\Omega\) there are therefore functions \(\omega_{ij}\) with \(\pp_{k}\omega_{ij}=\Phi_{ijk}\), each fixed up to a constant. Since \(\Phi_{ijk}=-\Phi_{jik}\), the constants may be chosen so that \(\omega_{ij}=-\omega_{ji}\), and \(\omega_{ii}=0\).
Step 2: the displacement. For each fixed \(i\) consider \(k\longmapsto u_{ik}-\omega_{ik}\), which is \(C^{1}\). Its curl is
every term cancelling in pairs, the last two because \(u_{kl}=u_{lk}\). Proposition 7.104(3) again supplies functions \(u_{i}\) with \(\pp_{k}u_{i}=u_{ik}-\omega_{ik}\). Symmetrising and using the symmetry of \(u_{ik}\) with the antisymmetry of \(\omega_{ik}\),
so \(\vect{u}\) has the prescribed strain.
Step 3: uniqueness. Let \(\vect{v}\) have zero strain, \(\pp_{i}v_{k}+\pp_{k}v_{i}=0\). The identity of step 1, applied with \(u_{ik}=0\), gives \(\pp_{k}w_{ij}=\Phi_{ijk}=0\) for \(w_{ij}=\tfrac{1}{2}(\pp_{i}v_{j}-\pp_{j}v_{i})\), so \(w\) is a constant antisymmetric array on the connected \(\Omega\). The symmetric part of \(\pp_{j}v_{k}\) vanishes by hypothesis, so \(\pp_{j}v_{k}=w_{jk}\) is constant and \(v_{k}=a_{k}+w_{jk}x_{j}\) with \(a_{k}\) constant; writing the antisymmetric \(w_{jk}\) as \(\varepsilon_{jkm}b_{m}\) and using the cyclic symmetry of \(\varepsilon\) puts this in the form \(\vect{v}=\vect{a}+\vect{b}\times\vect{x}\). Conversely every such field has zero strain. Two displacements with the same strain differ by one of them, which is the stated uniqueness.
∎The index symmetries found in the proof of Proposition 30.14 are not a coincidence. The deformed body carries the metric \(g_{ik}=\delta_{ik}+2E_{ik}\) by Equation (30.8), and to first order in \(E\) the left-hand side of Equation (30.9) is \(-2\) times the linearised Riemann tensor of that metric (Theorem 13.152). Compatibility says that the deformed body is still a piece of flat Euclidean space — that it can be laid down in \(\R^{3}\) without tearing or overlapping. An incompatible strain field is one that cannot: it describes a body with built-in stresses that no external load produces and no unloading removes. Crystal dislocations are the physical realisation, and their density is precisely the incompatibility Equation (30.9); the microscopic account belongs to Phonons and Lattice Dynamics. Rests on Equation (30.9) and Theorem 13.152.
Stress: the Cauchy tensor
Traction and the existence of the stress tensor
Cut the body along a surface through the point \(\vect{x}\) with unit normal \(\vect{n}\). The material on the side into which \(\vect{n}\) points exerts on the material on the other side a force \(\Delta\vect{F}\) across an element of area \(\Delta A\) of the cut. The traction is
an SI force per unit area, measured in \(\mathrm{N}/\mathrm{m}^{2}=\mathrm{Pa}\). It depends on the orientation of the cut as well as on the point. Rests on Definitions 7.94 and 30.2.
That the traction depends on \(\vect{n}\) at all is what distinguishes a solid from an ideal fluid, in which the traction is \(-p\vect{n}\) for every \(\vect{n}\). The content of Cauchy's theorem is that the dependence is as simple as it could possibly be.
There is a field \(\sigma_{ik}(\vect{x})\), a Cartesian tensor of rank two, such that for every unit vector \(\vect{n}\)
Its column \(\sigma_{ik}\) at fixed \(k\) is the traction across the coordinate plane with normal \(\hat{\vect{e}}_{k}\). Rests on Definitions 13.5 and 30.17.
Derives Theorem 30.18. First, \(\vect{t}(\vect{x},-\vect{n})=-\vect{t}(\vect{x},\vect{n})\). Apply Newton's second law to a flat pillbox of face area \(A\) and thickness \(h\) straddling the cut: the mass and hence the inertia and the body force are \(O(hA)\), while the two faces contribute \(\left[\vect{t}(\vect{n})+\vect{t}(-\vect{n})\right]A\) and the rim \(O\left(hA^{1/2}\right)\). Dividing by \(A\) and letting \(h\to0\) leaves the stated relation.
Now take a tetrahedron with three faces in the coordinate planes, meeting at \(\vect{x}\), and a fourth face of area \(A\) with outward unit normal \(\vect{n}\) at perpendicular distance \(h\) from \(\vect{x}\). The coordinate faces have areas \(An_{k}\) and outward normals \(-\hat{\vect{e}}_{k}\), and the volume is \(hA/3\). Newton's second law for the tetrahedron reads
where \(\vect{b}\) is the body force per unit mass and the mean values of the continuous fields over the faces have been used. Divide by \(A\) and let \(h\to0\): the left side vanishes, and
This is Equation (30.15). The nine numbers \(\sigma_{ik}\) so defined are a tensor by the quotient law of Section 13.2.2: \(t_{i}\) and \(n_{k}\) are vectors and \(\vect{n}\) is arbitrary, so the array contracting one into the other must transform as a rank-two tensor. Note that no constitutive assumption of any kind has been made — the argument is pure balance of momentum, and Equation (30.15) therefore holds for fluids, plastic solids and viscoelastic media as well.
∎In the absence of distributed body couples, \(\sigma_{ik}=\sigma_{ki}\). Rests on Theorem 30.18 and Definition 30.17.
Derives Proposition 30.19. Apply the balance of angular momentum about its own centre to a cube of side \(\ell\) centred at \(\vect{x}\). The torque about the \(z\) axis from the tractions on the four vertical faces is, to leading order, \(\left(\sigma_{yx}-\sigma_{xy}\right)\ell^{3}\); the torque from the body force is \(O(\ell^{4})\), because \(\int(\vect{r}\times\vect{f})\dd V\) over a region of size \(\ell\) centred on the reference point carries one factor of \(\ell\) from \(\vect{r}\) and three from \(\dd V\); and the moment of inertia is \(\rho\ell^{5}/6\). Hence the angular acceleration is
which diverges as \(\ell\to0\) unless \(\sigma_{yx}=\sigma_{xy}\). The same argument on the other two axes completes the proof. The hypothesis is essential and is not vacuous: a medium carrying an intrinsic torque per unit volume — a magnetised body in a field (Magnetism in Matter), a liquid crystal — adds a term of order \(\ell^{3}\) to the numerator and does support an antisymmetric part.
∎The pressure and the deviatoric stress are
so that \(\sigma_{ik}=-p\,\delta_{ik}+s_{ik}\) with \(s_{ll}=0\). By Proposition 30.19 and Theorem 5.75 there is an orthonormal frame in which \(\sigma_{ik}\) is diagonal; its entries \(\sigma_{1}\geq\sigma_{2}\geq\sigma_{3}\) are the principal stresses, and \(p=-\left(\sigma_{1}+\sigma_{2}+\sigma_{3}\right)/3\). Rests on Proposition 30.19 and Theorem 5.75.
The split is not cosmetic. Phenomenon 30.28 will show that \(p\) and \(s_{ik}\) are controlled by two independent material constants; Proposition 30.74 will show that plastic failure is governed by \(s_{ik}\) alone. A steel specimen at the bottom of the ocean, with \(p=110\,\mathrm{MPa}\) and \(s_{ik}=0\), is compressed by about \(6.6\times 10^{-4}\) in volume and is in no danger whatever; the same material at \(\sigma_{1}-\sigma_{3}=500\,\mathrm{MPa}\) has already yielded.
Momentum balance
For a continuum of density \(\rho\) carrying a body force \(f_{i}\) per unit volume,
in the material description and for small displacements. Statics is the case \(\pp_{t}^{2}u_{i}=0\), giving the equilibrium equations \(\pp_{k}\sigma_{ik}+f_{i}=0\). Rests on Theorems 7.101 and 30.18.
Derives Theorem 30.21. Let \(V\) be any fixed material region with boundary \(S\). Newton's second law for the material in \(V\) balances the rate of change of its momentum against the surface tractions and the body force:
using Equation (30.15). By the divergence theorem (Theorem 7.101) applied to each of the three vector fields \(k\mapsto\sigma_{ik}\),
The region \(V\) was arbitrary and the integrand is continuous, so it vanishes pointwise — the argument of the fundamental lemma Lemma 16.18, applied here with arbitrary subregions rather than arbitrary test functions.
∎The boundary \(\pp\Omega\) is partitioned into a part \(\pp\Omega_{\mathrm{u}}\) where the displacement is prescribed, \(u_{i}=\bar{u}_{i}\), and a part \(\pp\Omega_{\mathrm{t}}\) where the traction is prescribed, \(\sigma_{ik}n_{k}=\bar{t}_{i}\). A free surface is the case \(\bar{t}_{i}=0\). A kinematically admissible field is any \(C^{1}\) field agreeing with \(\bar{u}_{i}\) on \(\pp\Omega_{\mathrm{u}}\). Rests on Theorem 30.21 and Definition 10.24.
Let \(\sigma_{ik}\) satisfy equilibrium and the traction condition of Definition 30.22. Then for every field \(w_{i}\) vanishing on \(\pp\Omega_{\mathrm{u}}\),
with \(w_{ik}=\tfrac{1}{2}(\pp_{i}w_{k}+\pp_{k}w_{i})\); and conversely, a stress field satisfying Equation (30.18) for all such \(w_{i}\) is in equilibrium. Rests on Theorem 30.21 and Definition 30.22.
Derives Proposition 30.23. Because \(\sigma_{ik}\) is symmetric, \(\sigma_{ik}\pp_{k}w_{i} =\sigma_{ik}w_{ik}\). Integrate the identity \(\pp_{k}\left(\sigma_{ik}w_{i}\right) =\left(\pp_{k}\sigma_{ik}\right)w_{i}+\sigma_{ik}\pp_{k}w_{i}\) over \(\Omega\) and apply Theorem 7.101:
On \(\pp\Omega_{\mathrm{u}}\) the field \(w_{i}\) vanishes and on \(\pp\Omega_{\mathrm{t}}\) the traction is \(\bar{t}_{i}\); substituting \(\pp_{k}\sigma_{ik}=-f_{i}\) rearranges the display into Equation (30.18). For the converse, run the computation backwards: Equation (30.18) becomes \(\int_{\Omega}\left(\pp_{k}\sigma_{ik}+f_{i}\right)w_{i}\dd V =\int_{\pp\Omega_{\mathrm{t}}}\left(\bar{t}_{i} -\sigma_{ik}n_{k}\right)w_{i}\dd S\) for all admissible \(w_{i}\), and choosing \(w_{i}\) supported in the interior and then near the traction boundary kills the two brackets in turn by Lemma 16.18.
∎Equation (30.18) is the principle of virtual work of Central Forces and Statics written for a continuum, and it is the form in which elasticity is actually solved: it asks only one derivative of the displacement instead of two, which is what makes the finite-element method and the Sobolev theory of Definition 10.85 and Theorem 10.88 applicable.
Linear elasticity: Hooke's law and the moduli
Hooke's law
Hooke published the law in 1676 as the anagram ceiiinosssttuv and unscrambled it two years later as ut tensio, sic vis — as the extension, so the force [Hooke:1678]. What he had was a statement about springs and wires; the tensorial statement below is what it becomes when the body is described by Definition 30.6 and Theorem 30.18.
The elastic energy density \(F(u_{ik})\) is the reversible work done per unit volume in bringing the body from its unstrained state to the strain \(u_{ik}\), and the stress is
The elasticity tensor is \(C_{iklm}=\pp^{2}F/\pp u_{ik}\pp u_{lm}\) evaluated at \(u_{ik}=0\), a rank-four Cartesian tensor with the SI dimension of pressure, \(\mathrm{Pa}\). Rests on Definition 30.6 and Theorem 30.18.
\(C_{iklm}\) obeys the minor symmetries \(C_{iklm}=C_{kilm}=C_{ikml}\), which follow from the symmetry of \(u_{ik}\) and of \(\sigma_{ik}\), and the major symmetry \(C_{iklm}=C_{lmik}\), which follows from the existence of the energy \(F\). A general anisotropic solid therefore has \(21\) independent elastic constants. Rests on Definition 30.24 and Proposition 7.73.
Derives Proposition 30.25. Only the part of \(C_{iklm}\) symmetric in \((ik)\) and in \((lm)\) can contribute to \(C_{iklm}u_{ik}u_{lm}\), since \(u_{ik}\) is symmetric; this is the minor symmetry, and it reduces each index pair to the \(6\) values \(\{11,22,33,23,13,12\}\). The major symmetry is \(\pp^{2}F/\pp u_{ik}\pp u_{lm}=\pp^{2}F/\pp u_{lm}\pp u_{ik}\), which is Proposition 7.73 for the smooth function \(F\); without an energy function there would be no reason for it. The array is therefore a symmetric \(6\times6\) matrix, with \(6\times7/2=21\) independent entries.
∎Every rank-four Cartesian tensor invariant under all of \(\SO(3)\) is a linear combination
of the three products of Kronecker deltas, with \(a,b,c\) scalars. Rests on Theorem 5.128 and Definition 13.5.
Full derivation in Appendix A.
Derives Lemma 30.26.
The classification of the isotropic Cartesian tensors of ranks two, three and four is invariant theory for the rotation group — general mathematics rather than elasticity — and it is proved in Part II, for ranks one to four together, as Theorem 5.128; the ranks are settled in one theorem because they share the same machinery, not because the higher needs the lower. The rank-four case is restated here in the notation of this chapter because it is the one step that turns Proposition 30.25's twenty-one constants into two; the appendix section additionally carries the cubic case, which Part II does not treat.
Two pieces of general mathematics are used below and proved nowhere in this chapter, so they are named here rather than passed over. Both were written into Part II in August 2026 after this chapter reported them missing, and the entries stand as a record of what this chapter rests on. First, the classification just stated: the isotropic Cartesian tensors of rank two, three and four are spanned by \(\delta_{ik}\), by \(\varepsilon_{ikl}\) and by the three products Equation (30.20) respectively. It is invariant theory for \(\SO(3)\), and it is Theorem 5.128, with Section 13.2.2 recording what it does for the tensor algebra. Second, the Helmholtz decomposition — that a vector field on a suitable domain splits into a gradient and a curl — which is Theorem 7.105. This chapter does not use it: the potential representation of Proposition 30.48 is introduced as an ansatz and verified, which proves that the Rayleigh wave exists and is all that proposition claims. The decomposition would be needed only to prove that every plane-strain motion is of that form, a completeness statement made nowhere in this chapter. Rests on Theorems 5.128 and 7.105.
For sufficiently small deformations the response of a solid is linear and reversible: the elongation of a loaded spring or bar is proportional to the load and is recovered in full when the load is removed — “ut tensio, sic vis” [Hooke:1678]. In continuum terms the stress is a linear function of the strain, and for an isotropic body it depends on the strain through two material constants alone,
[Lame:1852] [Landau:1986]. In structural metals the linear regime extends to strains of order \(10^{-3}\) and ends at the yield point of Phenomenon 30.73. Rests on Definition 30.24 and Lemma 30.26.
Derivation. Derives Phenomenon 30.28. The undeformed state is an equilibrium and carries no stress, so the expansion of the energy density about \(u_{ik}=0\) has neither a constant nor a linear term:
with the constant coefficients of Definition 30.24. By Equation (30.19) the stress is then linear in the strain up to the cubic remainder, \(\sigma_{ik}=C_{iklm}u_{lm}\). That is Hooke's law, and its observed domain of validity is precisely the range of strains over which the remainder is negligible — which is why the law is a small-strain statement and not a property of any particular material.
If the body is isotropic, \(C_{iklm}\) is invariant under every rotation of the frame, so by Lemma 30.26 it has the form Equation (30.20). The minor symmetries of Proposition 30.25 force \(b=c\), since exchanging \(i\) and \(k\) in Equation (30.20) exchanges the coefficients of \(\delta_{il}\delta_{km}\) and \(\delta_{im}\delta_{kl}\). Writing \(a=\lambda\) and \(b=c=\mu\) and contracting with \(u_{lm}\) gives \(\sigma_{ik}=\lambda u_{ll}\delta_{ik}+2\mu u_{ik}\), which is Equation (30.21). That two constants suffice for an isotropic solid is a consequence of symmetry, not a further approximation [Landau:1986].
∎\(\lambda\) and \(\mu\) are the Lamé constants [Lame:1852], both measured in \(\mathrm{Pa}\). Substituting Equation (30.21) into Equation (30.19) and integrating gives the energy density, which in terms of the split Equation (30.5) reads
The second form is the useful one: it separates the energy of a pure volume change from that of a pure shape change, and shows that the two are stored independently. \(\mu\) is the shear modulus and \(K\) the bulk modulus. Rests on Equations (30.5) and (30.21).
The unstrained state is a strict minimum of the elastic energy if and only if
Rests on Equation (30.23) and Theorem 5.112.
Derives Proposition 30.30. The second form of Equation (30.23) is a sum of two squares in variables that are independent — the trace \(u_{ll}\) and the five components of the traceless \(d_{ik}\) — so the quadratic form is positive definite exactly when both coefficients are positive, which is Theorem 5.112 read on a form already in normal shape. Each condition is realised by an admissible strain: a pure dilatation \(u_{ik}=\epsilon\delta_{ik}\) has \(F=\tfrac{9}{2}K\epsilon^{2}\) and no shear, and a pure shear as in Example 30.10 has \(F=\mu\gamma^{2}/2\) and no dilatation. A body violating either bound would gain energy by deforming and would not be found in the unstrained state at all.
∎The elastic moduli and their measurement
The two constants of Equation (30.21) may be traded for any other independent pair, and the laboratory has good reasons to prefer other pairs: \(\lambda\) corresponds to no experiment anyone performs, whereas the modulus that a tensile machine measures does.
For an isotropic solid define
-
the bulk modulus \(K\) by \(p=-K\,u_{ll}\) under hydrostatic loading;
-
the shear modulus \(\mu\) by \(s_{ik}=2\mu\,d_{ik}\);
-
Young's modulus \(E\) [Young:1807] by \(\sigma=E\,u_{\parallel}\) under uniaxial stress;
-
Poisson's ratio \(\nu\) [Poisson:1829] by \(\nu=-u_{\perp}/u_{\parallel}\) under uniaxial stress;
-
the P-wave modulus \(M=\lambda+2\mu\), the stiffness under uniaxial strain.
All but \(\nu\) are pressures, measured in \(\mathrm{Pa}\); \(\nu\) is dimensionless. Rests on Equation (30.21) and Definition 30.20.
A bar stretched along its axis contracts in the two transverse directions. Under uniaxial stress the ratio of transverse contraction to longitudinal extension is a material constant, Poisson's ratio \(\nu\) [Poisson:1829], and the axial strain is itself proportional to the applied stress, the constant of proportionality being Young's modulus \(E\) [Young:1807]. The measured value of \(\nu\) for every ordinary solid lies inside the stability window
clustering near \(\nu\approx0.3\) for structural metals and approaching the upper, incompressible end for materials whose shear modulus is small against their bulk modulus [Simmons:1971]. Rests on Phenomenon 30.28 and Proposition 30.30.
Derivation. Derives Phenomenon 30.32. Take the bar along \(z\) and impose the uniaxial stress \(\sigma_{zz}=\sigma\) with all other stress components zero. By isotropy the strain is diagonal, with \(u_{xx}=u_{yy}\equiv u_{\perp}\) and \(u_{zz}\equiv u_{\parallel}\). The transverse components of Equation (30.21) read \(0=\lambda(2u_{\perp}+u_{\parallel})+2\mu u_{\perp}\), so
which is positive whenever \(\lambda>0\): the transverse strain has the sign opposite to the axial one, as observed. Substituting back into the axial component gives \(\sigma=\mu(3\lambda+2\mu)u_{\parallel}/(\lambda+\mu)\), so that \(E=\mu(3\lambda+2\mu)/(\lambda+\mu)\) — the modulus is not an independent constant but a combination of the two in Equation (30.21). For the bounds, use Proposition 30.30: \(\mu>0\) and \(K=\lambda+\tfrac{2}{3}\mu>0\). Writing \(x=\mu/K\), so that \(x\) ranges over \((0,\infty)\), Equation (30.26) becomes
a strictly decreasing function of \(x\) with limits \(\tfrac{1}{2}\) as \(x\to0\) and \(-1\) as \(x\to\infty\). Its range is therefore the open interval of Equation (30.25). A solid far harder to compress than to shear sits at the top of that interval: it is effectively incompressible and contracts transversely by half of what it extends.
∎Any two of \(\left(\lambda,\mu,K,E,\nu,M\right)\) determine the rest. In particular
Rests on Phenomenon 30.32 and Definition 30.31.
Derives Proposition 30.33. The derivation of Phenomenon 30.32 gave \(\nu=\lambda/\left[2(\lambda+\mu)\right]\) and \(E=\mu(3\lambda+2\mu)/(\lambda+\mu)\). Solving the first for \(\lambda\) gives \(\lambda(1-2\nu)=2\mu\nu\), the third relation of Equation (30.28); substituting it into the second gives \(E=\mu\left[3\cdot2\mu\nu/(1-2\nu)+2\mu\right] \big/\left[2\mu\nu/(1-2\nu)+\mu\right]=2\mu(1+\nu)\), the first. Then \(K=\lambda+\tfrac{2}{3}\mu =2\mu\nu/(1-2\nu)+\tfrac{2}{3}\mu =\tfrac{2}{3}\mu(1+\nu)/(1-2\nu)=E/\left[3(1-2\nu)\right]\), the second. Eliminating \(\nu\) between the first two of Equation (30.28) gives \(3K(1-2\nu)=2\mu(1+\nu)\), hence \(\nu=(3K-2\mu)/\left[2(3K+\mu)\right]\) and, back-substituting, \(E=2\mu(1+\nu)=9K\mu/(3K+\mu)\). Finally \(M=\lambda+2\mu=\left(K-\tfrac{2}{3}\mu\right)+2\mu =K+\tfrac{4}{3}\mu\).
∎One further consequence of the quadratic energy is needed before the measured values, because it is what turns an assumed deformation into a rigorous bound on a modulus.
Among all kinematically admissible displacement fields, the equilibrium field — and only it, up to a rigid displacement compatible with the constraints — minimises
Derives Proposition 30.34. Let \(\vect{u}\) be the equilibrium field and \(\vect{v}=\vect{u}+ \vect{w}\) any admissible competitor, so that \(\vect{w}\) vanishes on \(\pp\Omega_{\mathrm{u}}\). Because \(F\) is the quadratic form Equation (30.22), \(F(u_{ik}+w_{ik})=F(u_{ik})+\sigma_{ik}w_{ik}+F(w_{ik})\) exactly, the cross term being \(C_{iklm}u_{lm}w_{ik}=\sigma_{ik}w_{ik}\) by the major symmetry of Proposition 30.25. Hence
The first three terms cancel by Proposition 30.23, and the last is non-negative by Proposition 30.30, vanishing only if \(w_{ik}\equiv0\), i.e. only if \(\vect{w}\) is a rigid displacement (Proposition 30.12). This is the Dirichlet principle of Proposition 10.91 for the elastic operator, and the same convexity underwrites the direct method Theorem 16.70.
∎| Crystal | $C_{11}$ | $C_{12}$ | $C_{44}$ | $A$ | $C_{12}/C_{44}$ |
|---|---|---|---|---|---|
| (GPa) | (GPa) | (GPa) | |||
| Aluminium | 106.8 | 60.4 | 28.3 | 1.22 | 2.13 |
| Copper | 168.4 | 121.4 | 75.4 | 3.21 | 1.61 |
| Iron | 231.4 | 134.7 | 116.4 | 2.41 | 1.16 |
| Sodium chloride | 49.1 | 12.8 | 12.8 | 0.71 | 1.00 |
| Diamond | 1076 | 125 | 577 | 1.21 | 0.22 |
| Material | $K$ (GPa) | $\mu$ (GPa) | $E$ (GPa) | $\nu$ |
|---|---|---|---|---|
| Aluminium | 75.9 | 26.1 | 70.4 | 0.345 |
| Copper | 137.1 | 47.3 | 127.3 | 0.345 |
| Iron | 166.9 | 81.8 | 210.9 | 0.289 |
| Sodium chloride | 24.9 | 14.7 | 36.8 | 0.253 |
| Diamond | 442 | 534 | 1142 | 0.069 |
A polycrystal is a mass of randomly oriented anisotropic grains and is isotropic on the average, so it must be described by two constants built from the three of Table 30.1. For a cubic crystal the bulk modulus is exact and orientation independent, \(K=(C_{11}+2C_{12})/3\). The shear modulus is not, and is bracketed by two estimates: assuming a uniform strain throughout the aggregate gives the Voigt value \(\mu_{\mathrm{V}}=(C_{11}-C_{12}+3C_{44})/5\), and assuming a uniform stress gives the Reuss value \(\mu_{\mathrm{R}}=5(C_{11}-C_{12})C_{44} \big/\left[4C_{44}+3(C_{11}-C_{12})\right]\). A uniform strain is a kinematically admissible field but not the equilibrium one, so by Proposition 30.34 it stores more energy than the true field does at the same overall deformation: the aggregate looks stiffer than it is, and \(\mu_{\mathrm{V}}\) is a rigorous upper bound. \(\mu_{\mathrm{R}}\) is the corresponding uniform-stress estimate; it falls below \(\mu_{\mathrm{V}}\) for every entry of Table 30.1, and the dual variational principle — minimum complementary energy at fixed stress, which this chapter states without proving — is what makes that ordering general. Their arithmetic mean is a convention, not a theorem, and it is what Table 30.2 reports.
For iron the arithmetic is \(K=(231.4+269.4)/3=166.9\,\mathrm{GPa}\), \(\mu_{\mathrm{V}}=(96.7+349.2)/5=89.2\,\mathrm{GPa}\), \(\mu_{\mathrm{R}}=5(96.7)(116.4)/(465.6+290.1) =74.5\,\mathrm{GPa}\), mean \(81.8\,\mathrm{GPa}\); then Equation (30.29) gives \(E=211\,\mathrm{GPa}\) and \(\nu=0.289\). Those are the values quoted for structural steel in every engineering handbook, obtained here from three ultrasonic measurements on a single crystal of pure iron and one averaging assumption. The width of the Voigt–Reuss bracket, \(18\,\mathrm{\%}\) of the mean, is a direct measure of the anisotropy \(A=2.41\); for aluminium, with \(A=1.22\), the same bracket is under \(1\,\mathrm{\%}\) wide, and the Hill convention costs nothing there. Rests on Propositions 30.33 and 30.34.
Three routes, of increasing precision, all traceable to the SI metre, second and kilogram (Measurement, SI Units, and the Theory of Errors).
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Static loading. Hang a known force on a bar of known cross-section and measure the extension. A steel bar at \(\sigma=200\,\mathrm{MPa}\) — a working stress — stretches by \(u_{\parallel}=\sigma/E=9.5\times 10^{-4}\), about one part in a thousand, so a metre of bar lengthens by \(0.95\,\mathrm{mm}\). That is easy to see and hard to measure to better than \(1\,\mathrm{\%}\), and the method is further limited by grip effects and by creep.
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Resonance. Excite a bar or plate and count its natural frequencies; the moduli follow from the eigenvalue relations of Propositions 30.57 and 30.66. Counting is the one laboratory operation done without error, so this is immediately two orders of magnitude better.
-
Ultrasonic pulse-echo. Time a pulse across a specimen of measured thickness and obtain \(v_{\mathrm{P}}\) and \(v_{\mathrm{S}}\) directly; then by Equation (30.35)
\begin{equation}\tag{30.31} \mu=\rho\,v_{\mathrm{S}}^{2}\ec\qquad \lambda=\rho\left(v_{\mathrm{P}}^{2} -2v_{\mathrm{S}}^{2}\right)\ep \end{equation}This needs one length, two times and a density, is insensitive to the specimen's shape, and works on a crystal small enough that no static test could grip it — which is why the tabulated single-crystal constants of Table 30.1 are almost all ultrasonic.
Rests on Equation (30.35) and Proposition 30.33.
Anisotropic elasticity
Map each symmetric index pair to a single index by \(11\mapsto1\), \(22\mapsto2\), \(33\mapsto3\), \(23\mapsto4\), \(13\mapsto5\), \(12\mapsto6\), and write \(C_{\alpha\beta}\) for the resulting symmetric \(6\times6\) matrix of Proposition 30.25 [Voigt:1910]. The stress components map directly, \(\sigma_{\alpha}\); the strain components carry a factor two on the shear entries, \(u_{4}=2u_{23}\), \(u_{5}=2u_{13}\), \(u_{6}=2u_{12}\), so that \(\sigma_{\alpha}=C_{\alpha\beta}u_{\beta}\) and \(F=\tfrac{1}{2}C_{\alpha\beta}u_{\alpha}u_{\beta}\) both hold with no stray factors. Rests on Proposition 30.25 and Definition 30.24.
Crystal symmetry cuts the \(21\) constants down. Each symmetry operation of the crystal class must leave \(C_{\alpha\beta}\) invariant, and the resulting linear conditions leave \(13\) constants for the monoclinic classes, \(9\) for the orthorhombic, \(6\) or \(7\) for the tetragonal and trigonal, \(5\) for the hexagonal, \(3\) for the cubic — \(C_{11}\), \(C_{12}\) and \(C_{44}\), the constants tabulated in Table 30.1 — and \(2\) for the isotropic limit, where in addition \(C_{11}=\lambda+2\mu\), \(C_{12}=\lambda\) and \(C_{44}=\mu\), so that \(A=2C_{44}/(C_{11}-C_{12})=1\) [Voigt:1910]. The measured \(A\) is thus a direct readout of how far a crystal is from isotropy, and Table 30.1 shows it ranging from \(0.71\) for sodium chloride to \(3.21\) for copper: a copper single crystal is more than three times stiffer in shear on one set of planes than on another, which is why a textured copper sheet is not an isotropic body.
Suppose the atoms of a crystal sit at centres of symmetry of the lattice and interact through central pair potentials \(\varphi(r)\), and that the crystal is under no external stress. Then \(C_{iklm}\) is symmetric under every permutation of its four indices, so that six further relations hold and only \(15\) constants remain. For a cubic crystal the single relation is
Rests on Definition 30.24 and Proposition 30.25.
Derives Proposition 30.38. Write \(\eta_{b}=u_{ik}n_{i}n_{k}\) for the bond of length \(r_{b}\) and direction \(\hat{\vect{n}}\). By Equation (30.8) the strained length is \(r_{b}'=r_{b}\left(1+2\eta_{b}\right)^{1/2} =r_{b}\left(1+\eta_{b}-\tfrac{1}{2}\eta_{b}^{2}+\cdots\right)\). Because every atom sits at a centre of symmetry the bonds come in antiparallel pairs, so no internal relaxation of the sublattices is induced by a homogeneous strain and the energy per unit volume is simply \(\sum_{b}\varphi(r_{b}')\) over the bonds of one cell divided by its volume. Expanding,
The coefficient of the term linear in \(u_{ik}\) is the residual stress, which vanishes by the zero-stress hypothesis. The quadratic term gives
since \(\eta_{b}^{2}=u_{ik}u_{lm}n_{i}n_{k}n_{l}n_{m}\); the weights \(w_{b}\) depend on the bond length alone, and their exact normalisation — how the bond sum is counted — does not matter for what follows. Every summand is a product of four components of one and the same unit vector, hence invariant under any permutation of \(iklm\); so is \(C_{iklm}\). In particular \(C_{1122}=C_{1212}\), which in the notation of Definition 30.37 reads \(C_{12}=C_{66}\), and \(C_{66}=C_{44}\) for a cubic crystal: that is Equation (30.32). The other five relations are the remaining independent identifications among the \(21\) constants.
∎Proposition 30.38 was the ground of a nineteenth-century dispute. Navier and Poisson built elasticity on central forces between molecules and so predicted \(15\) constants, and \(1\) for an isotropic body — with \(\lambda=\mu\) and therefore \(\nu=\tfrac{1}{4}\) exactly [Navier:1827] [Poisson:1829]. Green and Lamé built it on the energy alone and predicted \(21\) and \(2\) [Lame:1852]. The question is empirical, and Table 30.1 settles it: the last column should be \(1.00\) for every crystal if the Cauchy relations held, and it is \(1.00\) only for sodium chloride, running to \(2.13\) for aluminium and \(0.22\) for diamond. Voigt's systematic measurements across the crystal classes are what closed the matter in favour of the multi-constant theory [Voigt:1910]. The physical reading is now clear: an ionic crystal is held together by very nearly central forces between closed shells, so it nearly obeys the relations; a metal is held together by a delocalised electron gas and diamond by directional covalent bonds, and neither is a sum of central pair potentials. That is a statement about the electronic structure, and it is settled in Electrons in Solids: Band Theory; the elastic constants of Table 30.1 are among the sharpest classical constraints on it, and they reappear as the long-wavelength limit of the lattice dynamics of Phonons and Lattice Dynamics. Rests on Proposition 30.38 and Definition 30.37.
Elastodynamics and elastic waves
The Navier–Cauchy equations
Derives Theorem 30.40. Substitute Equation (30.21), with \(u_{ik}=\tfrac{1}{2}(\pp_{i}u_{k}+\pp_{k}u_{i})\), into Cauchy's equation Equation (30.17). Since \(\lambda\) and \(\mu\) are constants,
where \(\pp_{k}\pp_{i}u_{k}=\pp_{i}\pp_{k}u_{k} =\pp_{i}(\vect{\nabla}\cdot\vect{u})\) by Proposition 7.73. This is Equation (30.33). Navier reached the same equation from a molecular model in which the constants were not independent [Navier:1827]; Cauchy reached it from the stress tensor, in which they are [Cauchy:1823], and Remark 30.39 says which of the two the measurements support.
∎Define the energy density and the energy flux
Then \(\pp_{t}e+\pp_{k}q_{k}=f_{i}\dot{u}_{i}\): elastic energy is locally conserved, and it is transported at the rate at which the internal tractions do work. Rests on Theorem 30.40 and Equation (30.23).
Derives Proposition 30.41. Differentiate: \(\pp_{t}e=\rho\dot{u}_{i}\ddot{u}_{i} +\sigma_{ik}\dot{u}_{ik}\), using Equation (30.19) for the second term. Because \(\sigma_{ik}\) is symmetric, \(\sigma_{ik}\dot{u}_{ik} =\sigma_{ik}\pp_{k}\dot{u}_{i}\). Substituting \(\rho\ddot{u}_{i}=\pp_{k}\sigma_{ik}+f_{i}\) from Equation (30.17),
which is the stated balance with \(q_{k}\) as defined.
∎The initial-boundary-value problem for Equation (30.33) — with \(\vect{u}\) and \(\dot{\vect{u}}\) given at \(t=0\), and with either the displacement or the traction prescribed at every point of \(\pp\Omega\) at every time — has at most one solution, up to a time-independent rigid displacement when no displacement is prescribed anywhere. Rests on Propositions 30.30 and 30.41.
Derives Theorem 30.42. Let \(\vect{w}\) be the difference of two solutions. It solves Equation (30.33) with \(\vect{f}=0\), with zero initial data, and with \(\vect{w}=0\) or \(\sigma_{ik}[\vect{w}]n_{k}=0\) at each boundary point. By Proposition 30.41 its total energy \(\mathcal{E}(t)=\int_{\Omega}e\,\dd V\) satisfies
by Theorem 7.101, since on each part of the boundary one factor of the integrand vanishes — the traction where the traction is prescribed, the velocity where the displacement is. Hence \(\mathcal{E}(t)=\mathcal{E}(0)=0\) for all \(t\). But \(\mathcal{E}\) is an integral of a sum of two non-negative terms, the second positive definite by Proposition 30.30, so \(\dot{\vect{w}}\equiv0\) and \(w_{ik}\equiv0\); by Proposition 30.12 \(\vect{w}\) is a rigid displacement, constant in time, and it vanishes if the displacement is prescribed anywhere. This is what makes the problem well posed in the sense of Definition 10.24, and the same energy identity gives the continuous dependence on the data.
∎P and S waves
An isotropic elastic solid transmits exactly two kinds of bulk wave: a longitudinal, compressional wave (the P phase of seismology) and a transverse, shear wave (the S phase), travelling at the distinct speeds
with \(v_{\mathrm{P}}>v_{\mathrm{S}}\) in every material [Poisson:1829]. The P arrival therefore always precedes the S arrival on a seismogram, and their separation measures the distance to the source [Oldham:1900]. A fluid, which cannot support a static shear, has \(\mu=0\) and carries no transverse branch at all. Rests on Theorem 30.40 and Proposition 30.30.
Derivation. Derives Phenomenon 30.43. Look for plane-wave solutions of the source-free Equation (30.33), \(\vect{u}=\vect{A}\exp\left[\ii\left(\vect{k}\cdot\vect{x} -\omega t\right)\right]\), with \(\vect{A}\) a constant polarization vector. Each spatial derivative brings down \(\ii k_{j}\) and each time derivative \(-\ii\omega\), so \(\vect{\nabla}(\vect{\nabla}\cdot\vect{u})\mapsto -\left(\vect{k}\cdot\vect{A}\right)\vect{k}\) and \(\nabla^{2}\vect{u}\mapsto-k^{2}\vect{A}\), giving
A plane wave exists exactly when \(\vect{A}\) is an eigenvector of the acoustic tensor \(\Gamma_{il}\), with \(\rho\omega^{2}\) the eigenvalue. \(\Gamma\) is real and symmetric, so Theorem 5.75 supplies an orthonormal eigenbasis, and it can be read off: \(\hat{\vect{k}}\) is an eigenvector with eigenvalue \((\lambda+\mu)k^{2}+\mu k^{2}=(\lambda+2\mu)k^{2}\), and every vector orthogonal to \(\vect{k}\) is an eigenvector with eigenvalue \(\mu k^{2}\). Those three exhaust \(\R^{3}\), so there are no other polarizations. Hence
which are the two speeds Equation (30.35). Both branches are non-dispersive: \(\omega\) is proportional to \(k\), so a pulse travels undistorted, which is what makes an arrival time a meaningful observable at all.
The physical labels follow from the polarizations. The longitudinal branch has \(\vect{\nabla}\times\vect{u}=0\) and carries the dilatation \(\vect{\nabla}\cdot\vect{u}\); the transverse branch has \(\vect{\nabla}\cdot\vect{u}=0\) and carries the rotation, deforming without changing any volume. Finally
by Proposition 30.30: the ordering of the two speeds is not an accident of the materials that happen to exist but follows from the existence of a stable unstrained state. Setting \(\mu=0\) annihilates the transverse branch and leaves \(v_{\mathrm{P}}=\sqrt{K/\rho}\), the sound speed of Fluid Dynamics.
∎a strictly increasing function of \(\nu\) on Equation (30.25) with range \(\left(2/\sqrt{3},\infty\right)\). No elastic solid whatever has \(v_{\mathrm{P}}/v_{\mathrm{S}}\leq2/\sqrt{3}=1.1547\), and a measurement of the ratio determines \(\nu\) without any knowledge of the density. Rests on Equation (30.35) and Proposition 30.33.
Derives Proposition 30.44. From Equation (30.35), \(v_{\mathrm{P}}^{2}/v_{\mathrm{S}}^{2}=(\lambda+2\mu)/\mu =\lambda/\mu+2\), and \(\lambda/\mu=2\nu/(1-2\nu)\) by Equation (30.28); adding gives \(\left(2\nu+2-4\nu\right)/(1-2\nu)=2(1-\nu)/(1-2\nu)\), which is Equation (30.37). Differentiating the square, \(\dd\left[2(1-\nu)/(1-2\nu)\right]/\dd\nu =2/(1-2\nu)^{2}>0\), so it increases; its values at the endpoints \(\nu=-1\) and \(\nu\to\tfrac{1}{2}\) are \(4/3\) and \(+\infty\). The density cancels between the two speeds, which is the practical point: an ultrasonic apparatus that measures only times and one length returns \(\nu\) directly.
∎Take the aggregate iron of Table 30.2, \(E=211\,\mathrm{GPa}\), \(\nu=0.289\), with \(\rho=7850\,\mathrm{kg}/\mathrm{m}^{3}\). Then \(\mu=E/\left[2(1+\nu)\right]=81.8\,\mathrm{GPa}\) and \(M=\lambda+2\mu=K+\tfrac{4}{3}\mu=276\,\mathrm{GPa}\), so
in a ratio \(1.84\), which Equation (30.37) returns from \(\nu=0.289\) alone. These are the handbook speeds for steel, and the agreement is a closed loop: three ultrasonic constants of a single crystal in Table 30.1, averaged in Example 30.35, reproduce the ultrasonic speeds of the polycrystal.
The separation of the two arrivals then gives the distance. A source at range \(d\) sends its P and S phases along the same path, so
and for the steel above \(\Delta t/d=1.41\times 10^{-4}\,\mathrm{s}/\mathrm{m}\): a delay of one millisecond places the source \(7.1\,\mathrm{m}\) away. The same arithmetic on a planetary scale, with the phases identified on a seismogram written thousands of kilometres from the epicentre, is Oldham's method and the foundation of seismology [Oldham:1900]. Rests on Proposition 30.44 and Equation (30.35).
The derivation of Phenomenon 30.43 was carried out on plane waves, where the completeness of the two polarizations is the spectral theorem for the \(3\times3\) matrix \(\Gamma_{il}\) and nothing more. The usual textbook route instead splits an arbitrary displacement field as \(\vect{u}=\vect{\nabla}\phi+\vect{\nabla}\times\vect{\psi}\) with \(\vect{\nabla}\cdot\vect{\psi}=0\) and shows that \(\phi\) and \(\vect{\psi}\) separately obey wave equations with the speeds Equation (30.35). That route needs the Helmholtz decomposition theorem — existence and uniqueness of the split, with the conditions at infinity that make it unique — which is general vector analysis and is Theorem 7.105, proved in The Helmholtz Decomposition. Either route is therefore available. The plane-wave argument is kept because it is self-contained and because it is what the seismological data are read against; the same theorem is what the potentials of Proposition 30.48 would need if that proposition claimed completeness, which it does not — see Remark 30.27. Rests on Phenomenon 30.43, Theorem 30.40 and Theorem 7.105.
Surface waves and the seismological evidence
A seismogram written far from an earthquake shows three groups of arrivals in a fixed order: a first, small compressional motion, a second and larger shear motion, and last of all a long, slowly decaying train of large-amplitude waves whose period varies through the train [Oldham:1900]. The third group is confined to the neighbourhood of the free surface, travels more slowly than either bulk wave of Phenomenon 30.43, and decays with depth over a distance of the order of a wavelength; its two polarizations are the vertically polarized Rayleigh wave, which exists on a homogeneous half-space [Rayleigh:1885], and the horizontally polarized Love wave, which requires a surface layer of lower shear speed over a faster substrate [Love:1911]. Rests on Phenomenon 30.43 and Proposition 30.49.
Derivation. Derives Phenomenon 30.47. The order of the first two groups is Equation (30.38) with \(v_{\mathrm{P}}>v_{\mathrm{S}}\), established in Phenomenon 30.43. That the third group comes last is Proposition 30.49 and Proposition 30.50: both surface branches travel below \(v_{\mathrm{S}}\), the Rayleigh wave at \(0.919\,v_{\mathrm{S}}\) for a Poisson solid and the Love wave between the two shear speeds of the layered structure. That the third group is the largest at great range, though the source radiates mostly body waves, is geometric. A body wave from a point source spreads over a hemisphere of area \(2\pi r^{2}\), so its energy flux falls as \(r^{-2}\) and its amplitude as \(r^{-1}\); a surface wave is confined to a skin of fixed thickness of order one wavelength and spreads over a cylinder of area \(2\pi r\times\text{const}\), so its flux falls as \(r^{-1}\) and its amplitude only as \(r^{-1/2}\). At \(r=1000\,\mathrm{km}\) from a source of characteristic size \(10\,\mathrm{km}\) the surface wave is therefore favoured by a factor \(\left(r/r_{0}\right)^{1/2}=10\) in amplitude over the body waves, which is why it dominates a distant record.
That the train is long and its period varies through it — the observed dispersion — is Proposition 30.50: the Love speed depends on \(\omega H/\beta\), so different periods arrive at different times and a single impulsive source is drawn out into a train ordered in period. A homogeneous half-space would give a Rayleigh wave with no dispersion at all (Proposition 30.48 contains no length), so the observed dispersion is itself the evidence that the Earth is layered. Finally, the confinement to the surface: both branches are built from solutions decaying as \(\ee^{-qz}\) with \(q\) of order \(k\), so the motion is negligible below a depth of about one wavelength — \(35\,\mathrm{km}\) for a \(10\,\mathrm{s}\) Love wave travelling at \(3.5\,\mathrm{km}/\mathrm{s}\).
∎On the traction-free surface of a homogeneous isotropic half-space there is a wave whose displacement is confined to a plane containing the propagation direction and the normal, decays exponentially with depth, and travels at a speed \(c=\xi v_{\mathrm{S}}\) where \(\xi\) solves
with \(0<\xi<1\) [Rayleigh:1885]. The equation contains no length, so the wave is non-dispersive. Rests on Theorem 30.40 and Definition 30.22.
Derives Proposition 30.48. Let \(z\) measure depth from the free surface, so that the solid occupies \(z>0\), let the propagation be along \(x\), and seek a motion with \(u_{y}=0\) and no dependence on \(y\). Build it from two potentials,
This is an ansatz, not a decomposition theorem, and it is all the proposition needs: it asserts that such a wave exists, so it is enough to exhibit one. Since \(\vect{\nabla}\cdot\vect{u}=\nabla^{2}\phi\), substituting Equation (30.40) into the source-free Equation (30.33) and collecting gives
for the \(x\) component and the same two brackets differentiated by \(\pp_{z}\) and \(-\pp_{x}\) for the \(z\) component, so it suffices that each bracket vanish: \(\phi\) obeys the wave equation at \(v_{\mathrm{P}}\) and \(\psi\) at \(v_{\mathrm{S}}\), the two speeds Equation (30.35).
Take the surface wave
with \(k>0\). The two wave equations fix \(p^{2}=k^{2}-\omega^{2}/v_{\mathrm{P}}^{2}\) and \(q^{2}=k^{2}-\omega^{2}/v_{\mathrm{S}}^{2}\), so writing \(c=\omega/k=\xi v_{\mathrm{S}}\),
both real and positive — so that the motion decays with depth over a distance of order \(1/k\) — precisely when \(0<\xi<1\), since \(\gamma<1\) by \(v_{\mathrm{S}}<v_{\mathrm{P}}\) (Phenomenon 30.43).
The free surface \(z=0\) carries no traction (Definition 30.22), which for this motion is the two conditions \(\sigma_{zz}=\sigma_{xz}=0\). From Equation (30.21),
Insert Equation (30.41). In the first, the coefficient of \(A\) is \(\lambda\left(p^{2}-k^{2}\right)+2\mu p^{2} =(\lambda+2\mu)p^{2}-\lambda k^{2}=2\mu k^{2}-\rho\omega^{2} =\mu k^{2}\left(2-\xi^{2}\right)\), using \(\rho\omega^{2}=\mu k^{2}\xi^{2}\); in the second, the coefficient of \(B\) is \(\mu\left(q^{2}+k^{2}\right)=\mu k^{2}\left(2-\xi^{2}\right)\), the same combination. The cross terms are \(2\ii\mu kq\) in the first and \(-2\ii\mu kp\) in the second. Dividing throughout by \(\mu\), the two conditions at \(z=0\) are therefore
a homogeneous pair with a non-trivial solution only if its determinant \(k^{4}\left(2-\xi^{2}\right)^{2}-4k^{2}pq\) vanishes. Dividing by \(k^{4}\) and substituting Equation (30.42) gives Equation (30.39).
It remains to know that an admissible root exists. Put \(t=\xi^{2}\) and \(f(t)=\left(2-t\right)^{2} -4\sqrt{\left(1-t\right)\left(1-\gamma t\right)}\). Then \(f(0)=0\) and \(f'(0)=-4+2\left(1+\gamma\right)=2\left(\gamma-1\right)<0\), so \(f\) is negative just to the right of the origin, while \(f(1)=1>0\); by the intermediate value theorem (Theorem 7.23) \(f\) has a root in \((0,1)\), and \(\xi=\sqrt{t}\) is the Rayleigh ratio. Finally, no length enters Equation (30.39): \(\xi\) depends on \(\gamma\) alone, so \(c=\xi v_{\mathrm{S}}\) is independent of \(k\) and the wave does not disperse. The depth of penetration, by contrast, is \(1/p\) and \(1/q\), both of order the wavelength.
∎For \(\nu=\tfrac{1}{4}\) — the case \(\lambda=\mu\), \(\gamma=1/3\) — Equation (30.39) has exactly one admissible root, and
Rests on Proposition 30.48.
Derives Proposition 30.49. Put \(t=\xi^{2}\) and \(\gamma=1/3\) and square Equation (30.39):
Expanding, \((2-t)^{4}=t^{4}-8t^{3}+24t^{2}-32t+16\) and the right side is \(16-\tfrac{64}{3}t+\tfrac{16}{3}t^{2}\), so the difference is \(t^{4}-8t^{3}+\tfrac{56}{3}t^{2}-\tfrac{32}{3}t =\tfrac{t}{3}\left(3t^{3}-24t^{2}+56t-32\right)\). The root \(t=0\) is the trivial static solution. The cubic has \(t=4\) as a root by inspection, and dividing out leaves \(3t^{2}-12t+8=0\) with roots \(t=2\pm2/\sqrt{3}\). Admissibility requires \(0<t<1\), since both radicals in Equation (30.39) must be real for the depth dependence to decay: this excludes \(t=4\) and \(t=2+2/\sqrt{3}=3.1547\) and leaves \(t=2-2/\sqrt{3}=0.845299\). Squaring can create roots, so verify in the unsquared equation: \((2-t)^{2}=1.33333\) and \(4\sqrt{1-t}\sqrt{1-t/3} =4(0.393320)(0.847487)=1.33333\), so it is genuine. Hence \(\xi=\sqrt{0.845299}=0.91940\). The Rayleigh wave is thus slower than the S wave by \(8\,\mathrm{\%}\), which is what puts it last on the seismogram of Phenomenon 30.47, and its speed is a fixed multiple of \(v_{\mathrm{S}}\) with no free length — so on a homogeneous half-space it does not disperse.
∎Let a layer of thickness \(H\), density \(\rho_{1}\) and shear modulus \(\mu_{1}\) rest on a half-space with \(\rho_{2}\), \(\mu_{2}\), and write \(\beta_{j}=\sqrt{\mu_{j}/\rho_{j}}\). Horizontally polarized surface waves of angular frequency \(\omega\) and speed \(c=\omega/k\) exist if and only if \(\beta_{1}<c<\beta_{2}\) and
In particular no such wave exists unless \(\beta_{1}<\beta_{2}\), and the speed depends on \(\omega\): the Love wave is dispersive [Love:1911]. Rests on Theorem 30.40 and Definition 30.22.
Derives Proposition 30.50. Let \(z\) measure depth from the free surface, and look for a motion purely along \(y\), \(\vect{u}=\left(0,v,0\right)\) with \(v=f(z)\exp\left[\ii(kx-\omega t)\right]\). Such a field has \(\vect{\nabla}\cdot\vect{u}=0\), so Equation (30.33) reduces in each homogeneous medium to \(\rho\,\pp_{t}^{2}v=\mu\nabla^{2}v\), and hence to
In the layer take \(c>\beta_{1}\), so \(s^{2}=\omega^{2}/\beta_{1}^{2}-k^{2}>0\) and \(f=A\cos sz+B\sin sz\). The free surface carries the traction \(\sigma_{yz}=\mu_{1}\pp_{z}v\), which must vanish at \(z=0\): hence \(B=0\) and \(f=A\cos sz\). In the half-space take \(c<\beta_{2}\), so \(q^{2}=k^{2}-\omega^{2}/\beta_{2}^{2}>0\) and the only solution bounded at depth is \(f=C\ee^{-q(z-H)}\). Continuity of the displacement and of the traction \(\mu\pp_{z}v\) across \(z=H\) gives
and dividing the second by the first, \(\mu_{1}s\tan sH=\mu_{2}q\), which is Equation (30.47) once \(s\) and \(q\) are written out. If \(\beta_{1}\geq\beta_{2}\) the two requirements \(c>\beta_{1}\) and \(c<\beta_{2}\) are incompatible and no solution exists — a homogeneous half-space, in particular, carries no Love wave, which is why Love had to introduce the layer [Love:1911]. Finally \(k\) and \(\omega\) enter Equation (30.47) separately and not only through \(c\), so \(c\) depends on frequency; as \(\omega\to\infty\) the wave concentrates in the layer and \(c\to\beta_{1}\), while near the cut-off of each higher branch \(c\to\beta_{2}\).
∎Rods, beams and plates
A rod, a beam, a plate and a shell are not new physics: they are Equation (30.33) on a domain with one or two small dimensions, reduced by exploiting that smallness. The reduction replaces a three-dimensional problem by a one- or two-dimensional one and turns the elastic energy into a functional of a single function, after which the machinery of Calculus of Variations does the rest.
The elastica and Euler buckling
Let a slender rod of cross-section \(S\) lie along \(x\) and bend in the \(xz\) plane with small deflection \(w(x)\). If plane cross-sections remain plane and normal to the deformed axis, and if the only non-negligible stress is the axial one, then the fibre at height \(z\) carries the strain and stress
and the internal bending moment about the neutral axis is
with \(I\) the second moment of area, of SI dimension \(\mathrm{m}^{4}\). Rests on Equation (30.21) and Definition 30.31.
Derives Proposition 30.51. Under the kinematic hypothesis, a cross-section at \(x\) rotates through the angle \(w'(x)\), so the axial displacement of the fibre at height \(z\) is \(u_{x}=-z\,w'(x)\) and its axial strain is \(u_{xx}=\pp_{x}u_{x}=-z\,w''\). The lateral faces of the rod are free, so \(\sigma_{yy}=\sigma_{zz}=0\) and the state is uniaxial stress — whence \(\sigma_{xx}=E\,u_{xx}\) by Definition 30.31, with \(E\) and not \(M\) appearing. The moment of these stresses about the axis \(z=0\) is \(-\int_{S}\sigma_{xx}z\,\dd S=Ew''\int_{S}z^{2}\dd S=EIw''\). The axis \(z=0\) is fixed by requiring zero net axial force, \(\int_{S}\sigma_{xx}\dd S=0\), i.e. \(\int_{S}z\,\dd S=0\): the neutral axis passes through the centroid.
∎A slender straight column under a slowly increased axial compression remains straight, shortening elastically, until at a definite critical load it bows sideways; the deflection appears suddenly and the column carries no more load. The critical load does not depend on the strength of the material but on its stiffness, and falls as the inverse square of the length: for a column of length \(L\), Young's modulus \(E\) and area moment of inertia \(I\), pinned at both ends,
Doubling the length of a column therefore quarters the load it can bear [Euler:1744]. Rests on Proposition 30.51 and Theorem 16.22.
Derivation. Derives Phenomenon 30.52. Let the column occupy \(0\leq x\leq L\) under the axial compression \(P\) and let \(y(x)\) be a small lateral deflection, with the ends pinned so that \(y(0)=y(L)=0\) and no moment is transmitted there. By Proposition 30.51 the bending moment at \(x\) is \(EI\,y''(x)\), and the moment of the applied load about the same section is \(-P\,y(x)\); equilibrium of the deflected shape therefore requires
This is an eigenvalue problem. Writing \(k^{2}=P/(EI)\), the general solution is \(y=A\sin kx+B\cos kx\); the condition at \(x=0\) forces \(B=0\), and the condition at \(x=L\) then requires either \(A=0\) — the straight column, available at every load — or \(\sin kL=0\), i.e.\ \(kL=n\pi\) with \(n\) a positive integer. A deflected equilibrium therefore exists only at the discrete loads \(P_{n}=n^{2}\pi^{2}EI/L^{2}\), and the smallest of them, \(n=1\), is Equation (30.50). Below it the straight column is the only equilibrium; at it a one-parameter family of bent shapes appears, which is what is seen as the sudden onset of buckling. Note that the material enters only through \(E\) and the cross-section only through \(I\): the yield stress of Phenomenon 30.73 plays no part, so a slender column fails long before its material does.
∎Take a circular steel rod of diameter \(10\,\mathrm{mm}\) and length \(1\,\mathrm{m}\), pinned at both ends, with \(E=210\,\mathrm{GPa}\). Its area moment is \(I=\pi d^{4}/64=4.91\times 10^{-10}\,\mathrm{m}^{4}\) and its area \(S=7.85\times 10^{-5}\,\mathrm{m}^{2}\), so Equation (30.50) gives
an axial stress of only \(13.0\,\mathrm{MPa}\). Crushing the same rod would need \(\sigma_{\mathrm{y}}S=19.6\,\mathrm{kN}\) at a yield stress of \(250\,\mathrm{MPa}\): buckling arrives at a nineteenth of that. The dimensionless control parameter is the slenderness \(L/r\) with \(r=\sqrt{I/S}=d/4=2.5\,\mathrm{mm}\) the radius of gyration, here \(L/r=400\), and Equation (30.50) in those terms is \(\sigma_{\mathrm{crit}}=\pi^{2}E/(L/r)^{2}\). Yield and buckling change places at \(L/r=\pi\sqrt{E/\sigma_{\mathrm{y}}}=91\): a rod stubbier than that is crushed, a slenderer one buckles. This is the single most consequential formula in structural engineering, and it was the first instability ever computed. Rests on Phenomenon 30.52 and Equation (30.50).
Clamping the ends changes only the length of the half-wave that must fit: Equation (30.50) holds with \(L\) replaced by an effective length \(L_{\mathrm{eff}}=\kappa L\), with \(\kappa=1\) pinned at both ends, \(\kappa=2\) for a cantilever fixed at one end and free at the other, \(\kappa=\tfrac{1}{2}\) clamped at both, and \(\kappa=0.699\) clamped at one and pinned at the other. The load capacity therefore varies by a factor \(16\) between the extremes at fixed \(L\).
Read variationally, buckling is the loss of positive-definiteness of a second variation. The energy of the compressed column is
the second term being the work done by \(P\) as the bent column shortens. This is exactly the accessory functional of Proposition 16.50, and Equation (30.51) is its Jacobi equation (Definition 16.53); \(P=P_{\mathrm{crit}}\) is the load at which \(x=L\) first becomes conjugate to \(x=0\), and Theorem 16.55 is the statement that the straight column ceases to be a minimum there. The two subjects — the sufficiency theory of the calculus of variations and the stability of structures — are the same theory. Rests on Phenomenon 30.52 and Theorem 16.55.
Equation (30.51) is the small-deflection limit. Euler solved the exact problem in the appendix on elastic curves of the Methodus inveniendi [Euler:1744]: parametrising the rod by arc length \(s\) and letting \(\theta(s)\) be the angle of the tangent, the exact statement that the curvature is proportional to the moment is
which is the pendulum equation of Oscillations and Mechanical Waves with \(s\) in place of time. Its solutions are elliptic functions, and the amplitude of the buckled shape grows as \(\theta_{\max}\propto\left(P/P_{\mathrm{crit}}-1\right)^{1/2}\) just above threshold — a supercritical pitchfork bifurcation (Nonlinear Dynamics and Chaos). The linear theory predicts the threshold exactly and the amplitude not at all, which is the generic situation for a bifurcation and is why Equation (30.50) is safe to design with and useless for predicting how far a buckled column bends. Rests on Phenomenon 30.52 and Equation (30.7).
Euler–Bernoulli beam theory
A slender rod of bending stiffness \(EI\), mass per unit length \(\rho S\), carrying a transverse load \(q(x)\) per unit length, has transverse deflection \(w(x,t)\) obeying
At a free end the natural boundary conditions \(EIw''=0\) and \(\left(EIw''\right)'=0\) hold — vanishing moment and vanishing shear force. Rests on Proposition 30.51 and Theorem 16.38.
Derives Theorem 30.56. By Equation (30.48) the elastic energy density is \(\tfrac{1}{2}E\left(zw''\right)^{2}\); integrating over the cross-section gives \(\tfrac{1}{2}EI\left(w''\right)^{2}\) per unit length, so the action of the rod is \(\int\!\!\int\Lag\,\dd x\,\dd t\) with Lagrangian density
The density depends on a second derivative, so the stationarity condition is the Euler–Poisson equation Theorem 16.38,
which evaluates to \(q-\pp_{x}^{2}\left(EIw''\right) -\rho S\pp_{t}^{2}w=0\), i.e.\ Equation (30.53). The boundary terms produced by the integration by parts are \(\left[EIw''\,\delta w'\right]_{0}^{L}\) and \(-\left[\left(EIw''\right)'\delta w\right]_{0}^{L}\); where the end is free, \(\delta w\) and \(\delta w'\) are unconstrained and each bracket must vanish separately, which is Theorem 16.31. Where the end is clamped, \(\delta w\) and \(\delta w'\) vanish and the conditions are \(w=w'=0\) instead — two conditions at each end in every case, as a fourth-order equation requires.
∎Free waves on a uniform beam obey
so the phase velocity \(\omega/k\) grows without bound with \(k\) and the group velocity is twice the phase velocity. The natural frequencies of a beam of length \(L\) are \(\omega_{n}=\left(\beta_{n}L\right)^{2}\sqrt{EI/(\rho SL^{4})}\) with \(\beta_{n}L\) fixed by the end conditions; for a cantilever the roots of \(\cos\beta L\cosh\beta L+1=0\) give \(\beta_{1}L=1.8751\). Rests on Theorem 30.56 and Definition 9.2.
Derives Proposition 30.57. Substitute \(w=\exp\left[\ii\left(kx-\omega t\right)\right]\) into the source-free Equation (30.53) with \(EI\) constant: \(-\rho S\omega^{2}+EIk^{4}=0\), which is Equation (30.54). Then \(v_{\mathrm{ph}}=\omega/k=k\sqrt{EI/\rho S}\) and \(v_{\mathrm{g}}=\dd\omega/\dd k=2k\sqrt{EI/\rho S}=2v_{\mathrm{ph}}\). For a finite beam, separating \(w=W(x)\ee^{-\ii\omega t}\) gives \(W''''=\beta^{4}W\) with \(\beta^{4}=\rho S\omega^{2}/(EI)\), whose general solution is a combination of \(\sin\beta x,\cos\beta x,\sinh\beta x,\cosh\beta x\); imposing \(W=W'=0\) at the clamped end and \(W''=W'''=0\) at the free one gives a \(4\times4\) homogeneous system whose determinant reduces to \(\cos\beta L\cosh\beta L+1=0\), and its smallest positive root is \(\beta_{1}L=1.8751\).
∎Clamp a steel strip \(20\,\mathrm{mm}\) wide and \(2\,\mathrm{mm}\) thick with \(300\,\mathrm{mm}\) projecting. Then \(I=bh^{3}/12=1.33\times 10^{-11}\,\mathrm{m}^{4}\), \(EI=2.80\,\mathrm{N}\,\mathrm{m}^{2}\) and \(\rho S=0.314\,\mathrm{kg}/\mathrm{m}\), so
which is what a twanged ruler does. Note the scaling that Proposition 30.57 encodes: \(f_{1}\propto h/L^{2}\) at fixed material, since \(\sqrt{EI/\rho S}\propto h\) for a rectangle. Halving the overhang quadruples the pitch — two octaves — and this is the measurement route to \(E\) of Remark 30.36, since \(f_{1}\) can be counted to \(10^{-4}\) while an extension of a millimetre cannot. Rests on Proposition 30.57 and Theorem 30.56.
Equation (30.54) is unphysical at large \(k\): the phase velocity grows without limit and eventually exceeds \(v_{\mathrm{P}}\), which no disturbance in an elastic solid can do. The reason is that the theory neglects the shear deformation of the cross-section and its rotary inertia, and both matter once the wavelength approaches the depth \(h\). Comparing Equation (30.54) with the shear speed for a rectangular section, \(\sqrt{EI/\rho S}=h\sqrt{E/\rho}/\sqrt{12}\), the two agree when \(kh=\sqrt{12\mu/E}=\sqrt{6/(1+\nu)}\approx2.2\): the theory degrades once the wavelength falls below about three times the beam depth. Timoshenko's correction restores both neglected effects and gives a dispersion relation with two branches, both with bounded phase velocity [Timoshenko:1921]. This is the general pattern of a reduced theory: the reduction assumes a separation of scales, and it fails exactly where the separation does — as in Equation (30.1), one level up. Rests on Proposition 30.57 and Equation (30.35).
Torsion
A thin metal wire clamped at one end and twisted at the other exerts a restoring torque proportional to the angle of twist, and independent of the angle's history provided the twist is small. Coulomb measured the constant of proportionality and found it proportional to the fourth power of the diameter and inversely proportional to the length,
with \(\kappa\) measured in \(\mathrm{N}\,\mathrm{m}/\mathrm{rad}\) [Coulomb:1784]. A body of moment of inertia \(I_{0}\) suspended on such a fibre oscillates with period \(T=2\pi\sqrt{I_{0}/\kappa}\), which is how \(\kappa\) is measured and how the fibre becomes an instrument. Rests on Equation (30.21) and Definition 30.31.
Derivation. Derives Phenomenon 30.60. Take a circular cylinder of radius \(a=d/2\) along \(z\) and twist it uniformly, so that the section at height \(z\) rotates through \(\theta'z\) with \(\theta'=\Phi/L\) the twist per unit length. In cylindrical coordinates the displacement is \(u_{\phi}=\theta'zr\), \(u_{r}=u_{z}=0\), whose only non-vanishing strain component is \(u_{\phi z}=\tfrac{1}{2}\theta'r\); the deformation is a pure shear, so no volume changes and only \(\mu\) can enter. By Equation (30.21) the stress is \(\sigma_{\phi z}=2\mu u_{\phi z}=\mu\theta'r\), and the torque transmitted across a section is
Setting \(\theta'=\Phi/L\) gives Equation (30.55). The \(d^{4}\) is the content of Coulomb's measurement: a factor \(d^{2}\) because the sheared area grows so, and a second factor \(d^{2}\) because the lever arm and the strain each grow with \(r\). The restoring torque is linear in \(\Phi\) because Hooke's law is linear in the strain, so the torsional pendulum is harmonic and its period is amplitude independent, giving \(T=2\pi\sqrt{I_{0}/\kappa}\) from Oscillations and Mechanical Waves.
∎A fused-silica fibre of diameter \(50\,\mu\mathrm{m}\) and length \(1\,\mathrm{m}\), with shear modulus \(\mu=31\,\mathrm{GPa}\), has
A bar carrying \(I_{0}=10^{-4}\,\mathrm{kg}\,\mathrm{m}^{2}\) then swings with period \(T=2\pi\sqrt{I_{0}/\kappa}=456\,\mathrm{s}\), about \(7.6\,\mathrm{min}\). Because \(\kappa\) is read from that period and from a moment of inertia — a mass and a length — the instrument measures torque on an absolute scale, and a deflection of \(1\,\mathrm{mrad}\), easily resolved optically, corresponds to \(1.9\times 10^{-11}\,\mathrm{N}\,\mathrm{m}\). That sensitivity, and nothing more exotic, is what makes the Cavendish measurement of Experiment: The Cavendish Torsion Balance possible, and the same fibre reappears in every torsion-balance test of the equivalence principle. Rests on Phenomenon 30.60 and Equation (30.55).
Equation (30.56) used the circular symmetry twice: to assert that plane sections stay plane and to evaluate \(\int r^{2}\dd S\). Neither survives for a general cross-section. Saint-Venant's solution adds an axial displacement \(u_{z}=\theta'\psi(x,y)\) — the warping function — and equilibrium then requires \(\nabla^{2}\psi=0\) inside the section with a Neumann condition on its boundary, an ordinary potential problem of Section 10.4.3 [SaintVenant:1855]. The torsional rigidity that results is always less than \(\mu J\): the circle is the only section that does not warp, and it is the stiffest section of given area in torsion. For an ellipse of semi-axes \(a\) and \(b\) the exact rigidity is \(\mu\pi a^{3}b^{3}/(a^{2}+b^{2})\), which is \(4a^{2}b^{2}/(a^{2}+b^{2})^{2}\) times \(\mu J\) — \(64\,\mathrm{\%}\) for a \(2:1\) ellipse, and falling to zero for a slit. Using \(\mu J\) for a non-circular shaft therefore overestimates its stiffness, sometimes grossly, which is why open thin-walled sections are avoided wherever torsion is carried. Rests on Phenomenon 30.60 and Equation (30.55).
Plates and shells
For a plate of thickness \(h\) made of an isotropic material, the flexural rigidity is
with SI dimension \(\mathrm{N}\,\mathrm{m}\). The factor \(\left(1-\nu^{2}\right)^{-1}\) distinguishes a plate from a beam: a plate bent in one direction is prevented by its own width from contracting transversely, so the relevant stiffness is the plane-strain modulus \(E/(1-\nu^{2})\) and not \(E\). Rests on Propositions 30.33 and 30.51.
Under the hypotheses that the plate is thin, that normals to the mid-surface remain normal, and that the transverse normal stress is negligible, the transverse deflection \(w(x,y,t)\) of a plate of uniform thickness obeys
with \(\nabla^{4}=\nabla^{2}\nabla^{2}\) the biharmonic operator and \(q\) the transverse load per unit area. At a free edge the two boundary conditions are Kirchhoff's: the bending moment vanishes, and the transverse shear combined with the gradient of the twisting moment vanishes [Kirchhoff:1850]. Rests on Definition 30.63 and Theorem 16.38.
Full derivation in Appendix A.
Derives Theorem 30.64.
The reduction has three stages, all carried out there. The Kirchhoff kinematics — \(u_{x}=-z\,\pp_{x}w\), \(u_{z}=w\), and the plane-stress condition \(\sigma_{zz}=0\) in place of plane strain — turns the isotropic energy density into a quadratic in the curvatures of the mid-surface, and integrating it across the thickness produces the flexural rigidity Equation (30.57) together with a term proportional to the Gaussian curvature of the deflected surface, which is a pure boundary term whenever the edge is clamped. Varying the resulting functional gives Equation (30.58) by the Euler–Poisson equation Theorem 16.38. The third stage is Kirchhoff's: the variation leaves three boundary quantities at a free edge, one more than a fourth-order equation can carry, and the twisting moment is integrated by parts along the edge so that its gradient joins the transverse shear, leaving two conditions and a concentrated corner force.
Sand strewn on a flat plate driven at one of its resonances is swept off the moving regions and collects along sharp curves — the nodal lines of the excited mode. The pattern is not continuous in the driving frequency: it is unchanged through a resonance and jumps to a wholly different figure at the next, so that a given plate and clamping reproduce the same discrete set of frequencies and the same set of figures every time [Chladni:1787]. The mode frequencies of geometrically similar plates of the same material scale in proportion to the thickness and inversely as the square of the lateral dimension [Germain:1821] [Kirchhoff:1850]. Rests on Theorem 30.64 and Proposition 30.66.
Derivation. Derives Phenomenon 30.65. Free harmonic motion of the plate is \(w=W(x,y)\ee^{-\ii\omega t}\) in Equation (30.58) with \(q=0\), so \(W\) satisfies \(D\nabla^{4}W=\rho h\omega^{2}W\) with the plate's own boundary conditions. That is a self-adjoint eigenvalue problem of the kind of Definition 9.54: its spectrum is a discrete increasing sequence \(\omega_{1}<\omega_{2}<\cdots\), so a resonance can only occur at one of countably many frequencies and the mode shape is locked to the frequency. That is the observed discontinuity: sweeping the driving frequency, nothing changes until the next \(\omega_{n}\) is reached, and then the whole figure is replaced by the next eigenfunction.
The sand marks the nodal set \(\{W=0\}\) because a grain leaves the surface whenever the plate's peak downward acceleration exceeds \(g\): with local amplitude \(A\) the condition is \(\omega^{2}A>g\), so at \(f=500\,\mathrm{Hz}\) any region moving by more than \(A=g/\omega^{2}=1.0\,\mu\mathrm{m}\) throws its grains clear. They land elsewhere, are thrown again, and random-walk until they reach a region where \(A\) falls below the threshold — the neighbourhood of a node. The figure is therefore a picture of \(\{W=0\}\) broadened by the threshold, which is why the curves are sharp: near a nodal line \(W\) grows linearly, so the width of the deposit is the threshold amplitude divided by the slope of \(W\), and both are small.
The scaling is Proposition 30.66. Nothing in this argument is peculiar to a plate; the same three statements — discrete spectrum, nodal set, threshold — describe every visualisation of a standing wave in Experiment: Waves and Acoustics.
∎For geometrically similar plates of the same material, thickness \(h\), lateral dimension \(a\) and fixed boundary conditions, the natural frequencies are
with \(\Lambda_{n}\) a pure number depending on the shape and the boundary conditions but on nothing else. Rests on Theorem 30.64 and Definition 30.63.
Derives Proposition 30.66. Write \(\vect{x}=a\vect{\zeta}\) with \(\vect{\zeta}\) ranging over the fixed reference shape. Then \(\nabla^{4}=a^{-4}\nabla_{\zeta}^{4}\), and the eigenvalue problem \(D\nabla^{4}W=\rho h\omega^{2}W\) becomes \(\nabla_{\zeta}^{4}W=\Lambda W\) with \(\Lambda=\rho h\omega^{2}a^{4}/D\). The reduced problem involves only the reference shape and the boundary conditions, so its eigenvalues \(\Lambda_{n}\) are pure numbers. Solving for \(\omega\),
using Equation (30.57), and taking the square root gives Equation (30.59): proportional to \(h\), inversely proportional to \(a^{2}\), exactly as observed in Phenomenon 30.65. The same relation read backwards is a measurement of \(E/\left[\rho(1-\nu^{2})\right]\) from a frequency, a thickness and a diameter.
∎Chladni's figures were an open challenge for a generation. Germain won the Academy prize with an essay containing the fourth-order equation Equation (30.58) [Germain:1821]; her edge conditions were not correct, and neither were Poisson's, who imposed three conditions on a free edge where a fourth-order equation admits only two. Kirchhoff resolved the conflict by deriving the conditions from the variation of the energy rather than from a force balance — the natural boundary conditions of Theorem 16.31 — which combine the transverse shear and the twisting moment into a single effective shear [Kirchhoff:1850]. The episode is a clean instance of the general point: for a variational problem, the boundary conditions are not free to be chosen, they are part of the answer. Rests on Theorems 16.31 and 30.64.
Give the mid-surface curvature \(1/R\) and the reduction changes character. A transverse load on a flat plate can only be resisted by bending, with stiffness proportional to \(h^{3}\) through Equation (30.57); on a curved shell it is resisted also by stretching of the mid-surface, with stiffness proportional to \(h\). The ratio of the two is of order \(\left(R/h\right)^{2}\), which for an eggshell — \(R\approx20\,\mathrm{mm}\), \(h\approx0.35\,\mathrm{mm}\) — is about \(3000\). That is why an egg is hard to crush end-on and trivial to break on a rim, and why every efficient structure that spans a distance is curved. The price is that a shell resists load by membrane stress and can therefore lose it catastrophically by buckling, at a load far below the Euler estimate of Equation (30.50) and notoriously sensitive to imperfections. Rests on Definition 30.63 and Phenomenon 30.52.
Static problems and contact
Every reduced theory of Section 30.6 replaced a real end loading — a clamp, a pin, a hydraulic ram — by a resultant force and moment, and the replacement is licensed by what is called Saint-Venant's principle: two loadings of the same small region with the same resultant force and moment produce stress fields differing appreciably only within a distance of the order of the diameter of that region [SaintVenant:1855]. The physical content is that a self-equilibrated load — zero resultant, zero moment — produces a field that decays exponentially, and the decay length is set by the only length in the problem, the size of the loaded region.
It is called a principle and not a theorem for good reason. It is provable for a cylinder of compact cross-section, where the decay rates are the eigenvalues of an explicit auxiliary problem, and it fails for thin-walled and for strongly anisotropic structures, where a self-equilibrated end load can propagate for many diameters. The honest statement is that it is a very good rule for stocky isotropic bodies, that it is what makes the whole engineering theory of structures possible, and that a designer using it on a thin-walled box section is relying on something known to be false there. Rests on Proposition 30.23 and Theorem 30.21.
Two elastic bodies pressed together touch over a finite area, not at a point, and the force required grows faster than linearly with the approach of their centres. For two spheres of radii \(R_{1},R_{2}\) the measured relation between the normal force \(F\) and the mutual approach \(\delta\) is
with contact radius \(a=\sqrt{R\delta}\) and peak pressure \(p_{0}=3F/\left(2\pi a^{2}\right)\) [Hertz:1882]. The contact is therefore stiffening: doubling the approach requires nearly three times the force. Rests on Proposition 30.23 and Definition 30.31.
Derivation. Derives Phenomenon 30.70. The exponent follows from three geometric and dimensional statements and needs no solution of the elastic problem. Let \(a\) be the radius of the contact circle. First, the geometry of two nearly touching spheres gives \(\delta=a^{2}/R\) to leading order in \(a/R\), since the gap between the undeformed surfaces at distance \(a\) from the axis is \(a^{2}/2R_{1}+a^{2}/2R_{2}=a^{2}/2R\) and the two surfaces must meet there. Second, the only strain scale in the contact region is the indentation divided by its own size, \(\delta/a=a/R\), because \(a\) is the only length over which the displacement varies. Third, the stress is then \(E^{*}\) times that strain and acts over an area \(\pi a^{2}\), so
which is Equation (30.60) up to the pure number \(4/3\). The exponent \(3/2\) is exact and is purely geometric: it says that a Hertzian contact stiffens because the contact area grows with the load, not because any material stiffens. The combination \(E^{*}\) is the plane-strain modulus \(E/(1-\nu^{2})\) of Definition 30.63, appearing because the material just under a broad contact patch is laterally confined, and the two bodies act as compliances in series — hence the sum of reciprocals. The coefficient \(4/3\) and the pressure distribution \(p(r)=p_{0}\sqrt{1-r^{2}/a^{2}}\) require the full elastic solution for a half-space [Hertz:1882].
∎Full derivation in Appendix A.
Derives Phenomenon 30.70.
What is left to the appendix is the part the scaling argument cannot reach: the numerical coefficient \(4/3\) and the pressure profile \(p(r)=p_{0}\sqrt{1-r^{2}/a^{2}}\). It is obtained from Boussinesq's solution for a half-space loaded by a prescribed normal pressure over a circle — the surface displacement is a potential-theory integral of the pressure, of the kind of Section 10.4.3 — together with the two contact conditions: inside the circle the two deformed surfaces coincide, which for spheres means the surface displacement must vary as \(\delta-r^{2}/2R\); outside it they separate and the pressure vanishes. The elliptic profile is the unique pressure whose Boussinesq displacement is quadratic in \(r\) inside the circle, and integrating it over the contact area gives \(F=\tfrac{2}{3}p_{0}\pi a^{2}\), which with \(a=\sqrt{R\delta}\) is Equation (30.60).
Press two steel balls of radius \(10\,\mathrm{mm}\) together with \(1\,\mathrm{N}\). With \(E=210\,\mathrm{GPa}\) and \(\nu=0.29\), \(E^{*}=115\,\mathrm{GPa}\) and \(R=5\,\mathrm{mm}\), so Equation (30.60) gives a contact radius \(a=\left[3FR/(4E^{*})\right]^{1/3}=32\,\mu\mathrm{m}\), an approach \(\delta=a^{2}/R=0.20\,\mu\mathrm{m}\) and a peak pressure
One newton — the weight of an apple — generates half a gigapascal, nearly twice the yield stress of mild steel. The mean contact strain \(a/R=6.4\times 10^{-3}\) is nevertheless small, so linear elasticity is self-consistent as a description of the strain; what is not small is the stress, because \(E\) is large. This is why ball bearings are made of hardened steel with \(\sigma_{\mathrm{y}}\approx2\,\mathrm{GPa}\) rather than of the structural steel of Example 30.53, and why every rolling contact eventually fails by subsurface fatigue rather than by wear. Rests on Phenomenon 30.70 and Equation (30.60).
A uniform tension \(\sigma\) in a large plate is tripled at the edge of a small circular hole: the peak stress is \(3\sigma\), independent of the hole's size [Landau:1986]. For an elliptical hole of semi-axes \(a\) across the tension and \(b\) along it, with tip radius of curvature \(\varrho=b^{2}/a\), the peak is
which diverges as the ellipse degenerates into a crack, \(\varrho\to0\). Two consequences run through the rest of engineering. First, holes and notches must be given generous radii; a sharp re-entrant corner is a mathematical singularity and a practical crack starter. Second, and more seriously, Equation (30.61) says that linear elasticity predicts infinite stress at a crack tip for any applied load whatever, so it cannot by itself say when a cracked body breaks. Resolving that is the content of Proposition 30.76, and the resolution is to abandon the stress criterion for an energy one. Rests on Equation (30.21) and Theorem 30.18.
The limits of elasticity
Everything above rests on Equation (30.22): that the energy is quadratic and the stress therefore linear. Four distinct things end that regime, and it is worth being explicit that they are different failures with different signatures.
Elasticity has a boundary, and it is reached in two different ways. A ductile metal loaded beyond a critical stress ceases to recover its shape and flows: the flow sets in when the maximum shear stress in the body reaches a material constant, and superposing a hydrostatic pressure — however large — does not by itself produce it [Tresca:1864]. A brittle solid does not flow but breaks, and its measured strength is one to two orders of magnitude below the stress at which the interatomic bonds would part; the strength is set by the largest pre-existing flaw and falls as the inverse square root of its length, so that fine fibres of the same glass are far stronger than bulk specimens [Griffith:1921]. Rests on Propositions 30.74 and 30.76.
Derivation. Derives Phenomenon 30.73. The two halves are Proposition 30.74 and Proposition 30.76 respectively. What the pair says together is that “strength” is not one material property but two, governed by different parts of the stress tensor: ductile flow by the deviatoric part \(s_{ik}\) of Equation (30.16), which is why it is insensitive to pressure, and brittle fracture by the elastic energy available to be released, which is why it is sensitive to the flaw population and hence to the specimen's history rather than to its composition alone. That is also why the same material can do both: a steel that flows at room temperature cleaves below its transition temperature, where the shear stress needed for flow rises above the stress needed to run a crack.
∎The largest shear traction over all planes through a point is
attained on the two planes bisecting the extreme principal directions, and it is unchanged by the addition of any hydrostatic stress \(\sigma_{ik}\mapsto\sigma_{ik}-p_{0}\delta_{ik}\). A yield criterion of the form \(\tau_{\max}=k\) is therefore independent of pressure [Tresca:1864]. Rests on Definition 30.20 and Theorem 30.18.
Derives Proposition 30.74. Work in the principal frame of Definition 30.20, so \(\sigma=\diag\left(\sigma_{1},\sigma_{2},\sigma_{3}\right)\) with \(\sigma_{1}\geq\sigma_{2}\geq\sigma_{3}\). For a unit normal \(\vect{n}\) the traction is \(t_{i}=\sigma_{i}n_{i}\) (no sum), its normal component is \(\bar{\sigma}=\sum_{i}\sigma_{i}m_{i}\) with \(m_{i}=n_{i}^{2}\), and the shear component has magnitude
Since \(\sigma_{3}\leq\sigma_{i}\leq\sigma_{1}\) we have \(\left(\sigma_{i}-\sigma_{3}\right) \left(\sigma_{1}-\sigma_{i}\right)\geq0\) for each \(i\); averaging with the weights \(m_{i}\) gives \(\sum_{i}\sigma_{i}^{2}m_{i}\leq \left(\sigma_{1}+\sigma_{3}\right)\bar{\sigma}-\sigma_{1}\sigma_{3}\). Hence
the last step being the inequality between the geometric and arithmetic means of two non-negative numbers whose sum is \(\sigma_{1}-\sigma_{3}\). Both inequalities are equalities when \(m=\left(\tfrac{1}{2},0,\tfrac{1}{2}\right)\), i.e. for \(\vect{n}\) at \(45^\circ\) between the first and third principal directions, giving Equation (30.62). Adding \(-p_{0}\delta_{ik}\) shifts every principal stress by the same \(-p_{0}\) and leaves every difference, hence \(\tau_{\max}\), unchanged.
∎Equation (30.62) is not the only pressure-independent function of the deviator. The alternative in general engineering use replaces it by the second invariant \(\sqrt{\tfrac{3}{2}s_{ik}s_{ik}}\), which is smooth where Equation (30.62) has corners and fits ductile metals somewhat better; the two differ by at most \(15\,\mathrm{\%}\) for any stress state. This treatise cites no primary source for that criterion, because none was located in the accessible literature during the preparation of this chapter, and the claim is recorded here as uncited rather than attached to a reference that does not support it. Tresca's criterion, by contrast, rests on his own extrusion measurements [Tresca:1864]. Rests on Proposition 30.74 and Definition 30.20.
A plate under remote tension \(\sigma\) containing a through-crack of length \(2c\) releases elastic energy \(\pi\sigma^{2}c^{2}/E\) per unit thickness and creates surface energy \(4\gamma c\), with \(\gamma\) the surface energy per unit area. The total energy has a maximum at
so a crack shorter than \(2E\gamma/(\pi\sigma^{2})\) is stable and a longer one runs away. Strength therefore falls as \(c^{-1/2}\) and is a property of the flaw population, not of the bonds [Griffith:1921]. Rests on Remark 30.72 and Equation (30.23).
Derives Proposition 30.76. Let \(U(c)\) be the total energy of the plate at fixed remote displacement, measured from the uncracked state. Introducing the crack relaxes the material near it and releases stored elastic energy; the elastic solution for an elliptical hole degenerating to a crack, which Griffith took over for this purpose, gives that release as \(\pi\sigma^{2}c^{2}/E\) per unit thickness [Griffith:1921]. Creating the two new faces costs \(\gamma\) per unit area, and the two faces of a crack of length \(2c\) have total area \(4c\) per unit thickness. Hence
The derivative vanishes at \(c^{*}=2E\gamma/\left(\pi\sigma^{2}\right)\) and \(\dd^{2}U/\dd c^{2}=-2\pi\sigma^{2}/E<0\), so \(c^{*}\) is a maximum of the energy — an unstable equilibrium. A crack shorter than \(c^{*}\) can only grow by climbing the energy barrier and does not; one longer than \(c^{*}\) releases more energy than it costs at every subsequent length and accelerates without limit. Solving \(c=c^{*}\) for \(\sigma\) gives Equation (30.63). The criterion is an energy balance and not a stress criterion, which is exactly what was needed: Remark 30.72 showed that the stress at a crack tip is infinite for any load, so no stress criterion could ever have distinguished a safe crack from a dangerous one.
∎Take a silicate glass with \(E=70\,\mathrm{GPa}\) and a surface energy \(\gamma=0.5\,\mathrm{J}/\mathrm{m}^{2}\), and a surface flaw of half-length \(c=2\,\mu\mathrm{m}\) — a scratch invisible to the eye. Then Equation (30.63) gives
which is squarely inside the range that bulk glass actually shows. The stress the bonds themselves could support is of order \(\sqrt{E\gamma/a_{0}}\) with \(a_{0}=0.3\,\mathrm{nm}\) an interatomic spacing, about \(11\,\mathrm{GPa}\) — a hundredfold higher, and that hundredfold is the whole of the discrepancy the phenomenon reports. Reduce the flaw to \(c=20\,\mathrm{nm}\), which is what drawing and fire-polishing a fine fibre does, and Equation (30.63) predicts \(1.1\,\mathrm{GPa}\); this is why Griffith found the strength of his glass fibres rising steeply as their diameter fell, and it is why an optical fibre with a pristine surface outperforms structural steel in tension [Griffith:1921]. Nothing about the glass changed between the two numbers — only the largest scratch on it. Rests on Proposition 30.76 and Equation (30.63).
The cubic remainder discarded in Equation (30.22) is not only a correction to Hooke's law; it is the entire origin of two effects that a perfectly harmonic solid does not have. A harmonic solid does not expand when heated — the mean position of every atom sits at the minimum of a symmetric well regardless of the amplitude — and it has infinite thermal conductivity, because its normal modes never scatter off one another. Real solids do both, with a coefficient of linear expansion of order \(10^{-5}\,/\mathrm{K}\) for metals, and the microscopic account is the anharmonic lattice dynamics of Phonons and Lattice Dynamics. The macroscopic bookkeeping is that the elastic moduli measured adiabatically and isothermally differ, by a term proportional to the square of the expansion coefficient; for metals at room temperature that is a fraction of a percent, which is at the level of the uncertainties in Table 30.1. Rests on Phenomenon 30.28 and Definition 30.24.
A Maxwell material in shear responds to a deviatoric stress \(s_{ik}\) with a deviatoric strain rate
the two terms being an elastic and a viscous contribution in series, with \(\eta\) the shear viscosity in \(\mathrm{Pa}\,\mathrm{s}\). Its relaxation time is
Rests on Equation (30.21) and Definition 30.20.
Under a step of stress applied at \(t=0\) and held, Equation (30.64) gives \(d_{ik}(t)=\left(s_{ik}/2\mu\right) \left(1+t/t_{\mathrm{r}}\right)\): the response is elastic for \(t\ll t_{\mathrm{r}}\) and viscous for \(t\gg t_{\mathrm{r}}\). Under a step of strain held fixed, the stress decays as \(s_{ik}(t)=s_{ik}(0)\ee^{-t/t_{\mathrm{r}}}\). Rests on Definition 30.79.
Derives Proposition 30.80. For a constant \(s_{ik}\) the first term of Equation (30.64) vanishes after the step and integration gives \(d_{ik}(t)=d_{ik}(0)+s_{ik}t/(2\eta)\) with the instantaneous elastic response \(d_{ik}(0)=s_{ik}/(2\mu)\); factoring out \(s_{ik}/2\mu\) and using Equation (30.65) gives the stated form. For constant \(d_{ik}\) the left side vanishes and Equation (30.64) becomes \(\dot{s}_{ik}=-\left(\mu/\eta\right)s_{ik}\), whose solution is the stated exponential.
∎The ratio \(t_{\mathrm{r}}\) to the time of observation decides which chapter a material belongs in. Window glass at room temperature has \(t_{\mathrm{r}}\) of order \(10^{20}\) years and is a solid by any test that will ever be applied to it; the Earth's mantle has \(\eta\approx10^{21}\,\mathrm{Pa}\,\mathrm{s}\) and \(\mu\approx10^{11}\,\mathrm{Pa}\), so \(t_{\mathrm{r}}\approx10^{10}\) seconds — a few hundred years. It therefore transmits the seismic waves of Phenomenon 30.43 as an elastic solid on a timescale of minutes and convects as a fluid on a timescale of millions of years, and both descriptions are correct at their own frequency. That is the sense in which Fluid Dynamics is not a different subject but the same one at a different value of \(\omega t_{\mathrm{r}}\); the Cauchy momentum equation Equation (30.17) is common to both, and only the constitutive law relating \(\sigma_{ik}\) to the motion changes — from Equation (30.21), linear in the strain, to a law linear in the strain rate.